下扬子地区早古生代前陆盆地与油气前景分析
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摘要
下扬子地区晚奥陶世开始发生了剧烈的岩相古地理的变化,并沉积了巨厚的上奥陶统-志留系碎屑岩,覆盖于下伏碳酸盐岩台地之上。该套地层的沉积时代与华南早古生代造山时间相当,进一步确定该期盆地的性质和沉积演化过程对研究华南早古生代盆山关系和构造背景具有重要的意义。研究区在中、新生代经历了多期的叠加和改造,详细的分析每一期构造的性质、影响范围不仅对认识该区的构造格局有重要作用,而且对该区的油气勘探具有指导意义。
本文以盆地为主线,首先通过锆石定年探讨华南早古生代造山带的时代,确定下扬子地区早古生代盆地沉积的区域构造背景；其次根据沉积厚度的变化、盆地沉降过程和碎屑锆石物源分析等探讨前陆盆地的发育和演化过程；然后以构造解析为手段研究下扬子地区早古生代前陆盆地在中、新生代的构造改造；最后以石油地质理论为指导,综合分析该区的油气成藏条件和页岩气勘探前景。
利用锆石La-ICPMS定年测定了八都群和陈蔡群基底变质岩的变质年龄为453-442Ma,同构造花岗岩慈竹、金溪岩体年龄为分别为450Ma和430Ma左右。综合华南变质岩和同构造花岗岩已有数据和盆地研究资料得出华南早古生代造山作用主要发生在455-425Ma,与世界上典型加里东造山带形成的时间相当；基于上述认识和华南缺少泛非运动这一事实,提出华南在志留纪可能与加里东造山带相邻,并以古地磁资料为约束,将华南置于格林兰北部或挪威北部。
基于地层对比、地层厚度、沉积相变化、沉积过程和碎屑锆石物源分析,确定了下扬子晚奥陶世-志留纪盆地是受华南早古生代造山控制形成的前陆盆地,其前渊拗陷位于浙北皖南,前缘隆起位于沿江一带,苏北地区为隆后拗陷；碎屑锆石定年数据表明前陆盆地的物源主要有五个年龄峰,即2500Ma,1800-2100Ma,900-1200Ma,740-860Ma和425-460Ma,其中前三个年龄峰的物源主要来自武夷山元古界-奥陶纪系的再旋回沉积,后两个年龄峰对应于武夷山新元古代的岩浆事件和早古生代的造山事件,并且最年轻的锆石为志留纪茅山组的沉积时代提供了一个约束；根据厚度分布、沉积相特征和物源变化可以将前陆盆地的演化分为晚奥陶世欠充填阶段、早志留世鲁丹期-特里奇早期充填阶段和特里奇晚期过充填阶段。
根据不整合面分布、地层接触关系和断陷盆地的发育,得出下扬子地区早古生代前陆盆地在中新生代主要经历了晚三叠世、中晚侏罗世两期挤压和晚白垩世-古近纪的一期伸展断陷,早期的挤压由北西向南东,主要分布在长江沿岸以北地区,晚期的挤压由南东向北西,主要分布在长江以南地区,二者在长江沿岸地区形成对冲带；结合区域构造演化将下扬子盆地分为七个构造层,从下至上分别是震旦系-中奥陶统、上奥陶统-志留系、上古生界-中三叠统、上三叠统-中下侏罗统、上侏罗统-下白垩统构造层、上白垩统-古近系构造层和新近系-第四系构造层；依据变形的基本特征和变形期次的差异,将研究区分为10个构造单元,分别是江南褶皱带、江阴-无锡滑脱褶皱带、常州-宣城断陷盆地带、茅山褶皱冲断带、南陵-句容断陷盆地带、宁镇褶皱冲断带、铜陵-繁昌褶皱带、沿江盆地带、滁州-宿松褶皱带和苏北盆地。
该区早古生代发育下寒武统和上奥陶统-下志留统两套黑色页岩,二者具有厚度大、分布广、有机碳含量较高、有机质成熟度高、处于生气阶段等特点,具有非常好的页岩气勘探前景,特别是江阴-无锡滑脱褶皱带构造相对稳定,下古生界成藏条件优越,是油气勘探特别是页岩气勘探的有利区带。
Great changes of lithofacies and paleogeography occurred in the Lower Yangtze region during late Ordovician and Silurian, and thick siliciclastic was deposited and covered on the previous carbonate platform. The deposition was coeval with the orogenic event in South china, so study the type of the basin and its evolution has great importance to understand the relationship between the orogenic and basin, as well as the whole tectonic setting. Complex structures were formed in the study area due to multiple phases of compression and extension during Mesozoic and Cenozoic. To analyze the feature and extent of each tectonic event is the key to understand the structure features and also beneficial for the hydrocarbon exploration.
The thesis is focused on the basin formation and evolution. First of all, the method of zircon dating was used to analyze the timing of the orogenic event, in order to study the tectonic setting of the basin; second, comprehensive analyses of sediment thickness, subsidence process and detrital zircon provenance were carried out to study the development and evolution of the foreland basin; and then influence of Mesozoic and Cenozoic tectonic events on the foreland basin was studied in detail; finally, the elements of hydrocarbon and shale gas were evaluated from the aspects of source rocks, reservoir, seal and plays.
Zircon U-Pb dating indicates that the Badu and Chencai group were metamorphosed at about453-442Ma, and the syntectonic granites of Jinxi and Cizu were emplaced at about450Ma and430Ma respectively. Combined with available data of other metamorphic rocks and syntectonic granites as well as information about basin evolution, it is suggested that orogenic ativity mainly took place during455-425Ma, which was nearly coeval with the Caledonian orogeny. Based on above information and absent Pan-Africa orogeny in South China,1tentatively proposed that South China was near the Caledonian orogeny in Silurian, and place it to the north of the Greenland or the north of Scandinavian.
According to the analyses of strata correlation, thickness, sedimentary facies, subsidence and detrital zircon provenance, it is confirmed that the basin in the lower Yangtze region was a foreland basin during late Ordovician to Silurian, which was controlled by the early Paleozoic orogeny in South China. The foredeep was located in North Zhejiang and South Anhui, the forebulge along the Yangtze River, and the backbulge in the north of Jiangsu Provenance. Detrital zircon dating indicates the provenance of the foreland basin has five age populations,2500Ma,1800-2100Ma,900-1200Ma,40-860Ma and425-460Ma. The former three populations were derived from the recycling of the Proterozoic and early Paleozoic rocks in the orogenic belt, and the later two correlated well with the Neoproterozoic and early Paleozoic tectonic events, respectively. The youngest age of425Ma provided an age constrain for the timing of the foreland basin development. Combined with sedimentary features and provenance changes, it is proposed that the foreland basin was in underfilled stage during late Ordovician, filled stage in Llandovery, and overfilled stage in Wenlock.
It is revealed that the foreland basin has experienced two phases of compression during late Triassic and middle to late Jurassic and one phase of extension in late Cretaceous and Paleogene since it formed, according to the distribution of unconformity, the contact relationship of strata and rift basin development. The first compression was from NW toward SE and mainly influenced the area of north Yangtze River, while the late compression was from SE toward NW and mainly influenced the area in the south of Yangtze river. The formation of the basin can be divided into seven tectonic sequences, and from bottom to top they are Sinian-middle Ordovician, upper Ordovician-Silurian, upper Paleozoic-middle Triassic, upper Triassic-middle Jurassic, upper Jurassic-lower Cretaceous, upper Cretaceous-Paleogene and Neogene-Quaternary; according to deformation style and timing, ten tectonic units are divided, including Jiangnan belt, Jiangyin-Wuxi detachment folds, Changzhou-Xuancheng rift, Maoshan thrust belts, Nanling-Jurong rift, Niangzhen thrust belts, Tongling-Fanchang thrust belt, Chuzhou-Susong thrust belts and Subei rift basin.
Studies of source rocks, reservoir, seals and accumulation conditions of hydrocarbon reveal that the black shales of lower Cambrian and upper Ordovician-lower Silurian are thick, wide distribution, high in total organic carbon, and matured enough, which are favourable for shale gas exploration, and the Jiangyin-Wuxi area is the prospect play for the relatively simple structures.
本文以盆地为主线,首先通过锆石定年探讨华南早古生代造山带的时代,确定下扬子地区早古生代盆地沉积的区域构造背景；其次根据沉积厚度的变化、盆地沉降过程和碎屑锆石物源分析等探讨前陆盆地的发育和演化过程；然后以构造解析为手段研究下扬子地区早古生代前陆盆地在中、新生代的构造改造；最后以石油地质理论为指导,综合分析该区的油气成藏条件和页岩气勘探前景。
利用锆石La-ICPMS定年测定了八都群和陈蔡群基底变质岩的变质年龄为453-442Ma,同构造花岗岩慈竹、金溪岩体年龄为分别为450Ma和430Ma左右。综合华南变质岩和同构造花岗岩已有数据和盆地研究资料得出华南早古生代造山作用主要发生在455-425Ma,与世界上典型加里东造山带形成的时间相当；基于上述认识和华南缺少泛非运动这一事实,提出华南在志留纪可能与加里东造山带相邻,并以古地磁资料为约束,将华南置于格林兰北部或挪威北部。
基于地层对比、地层厚度、沉积相变化、沉积过程和碎屑锆石物源分析,确定了下扬子晚奥陶世-志留纪盆地是受华南早古生代造山控制形成的前陆盆地,其前渊拗陷位于浙北皖南,前缘隆起位于沿江一带,苏北地区为隆后拗陷；碎屑锆石定年数据表明前陆盆地的物源主要有五个年龄峰,即2500Ma,1800-2100Ma,900-1200Ma,740-860Ma和425-460Ma,其中前三个年龄峰的物源主要来自武夷山元古界-奥陶纪系的再旋回沉积,后两个年龄峰对应于武夷山新元古代的岩浆事件和早古生代的造山事件,并且最年轻的锆石为志留纪茅山组的沉积时代提供了一个约束；根据厚度分布、沉积相特征和物源变化可以将前陆盆地的演化分为晚奥陶世欠充填阶段、早志留世鲁丹期-特里奇早期充填阶段和特里奇晚期过充填阶段。
根据不整合面分布、地层接触关系和断陷盆地的发育,得出下扬子地区早古生代前陆盆地在中新生代主要经历了晚三叠世、中晚侏罗世两期挤压和晚白垩世-古近纪的一期伸展断陷,早期的挤压由北西向南东,主要分布在长江沿岸以北地区,晚期的挤压由南东向北西,主要分布在长江以南地区,二者在长江沿岸地区形成对冲带；结合区域构造演化将下扬子盆地分为七个构造层,从下至上分别是震旦系-中奥陶统、上奥陶统-志留系、上古生界-中三叠统、上三叠统-中下侏罗统、上侏罗统-下白垩统构造层、上白垩统-古近系构造层和新近系-第四系构造层；依据变形的基本特征和变形期次的差异,将研究区分为10个构造单元,分别是江南褶皱带、江阴-无锡滑脱褶皱带、常州-宣城断陷盆地带、茅山褶皱冲断带、南陵-句容断陷盆地带、宁镇褶皱冲断带、铜陵-繁昌褶皱带、沿江盆地带、滁州-宿松褶皱带和苏北盆地。
该区早古生代发育下寒武统和上奥陶统-下志留统两套黑色页岩,二者具有厚度大、分布广、有机碳含量较高、有机质成熟度高、处于生气阶段等特点,具有非常好的页岩气勘探前景,特别是江阴-无锡滑脱褶皱带构造相对稳定,下古生界成藏条件优越,是油气勘探特别是页岩气勘探的有利区带。
Great changes of lithofacies and paleogeography occurred in the Lower Yangtze region during late Ordovician and Silurian, and thick siliciclastic was deposited and covered on the previous carbonate platform. The deposition was coeval with the orogenic event in South china, so study the type of the basin and its evolution has great importance to understand the relationship between the orogenic and basin, as well as the whole tectonic setting. Complex structures were formed in the study area due to multiple phases of compression and extension during Mesozoic and Cenozoic. To analyze the feature and extent of each tectonic event is the key to understand the structure features and also beneficial for the hydrocarbon exploration.
The thesis is focused on the basin formation and evolution. First of all, the method of zircon dating was used to analyze the timing of the orogenic event, in order to study the tectonic setting of the basin; second, comprehensive analyses of sediment thickness, subsidence process and detrital zircon provenance were carried out to study the development and evolution of the foreland basin; and then influence of Mesozoic and Cenozoic tectonic events on the foreland basin was studied in detail; finally, the elements of hydrocarbon and shale gas were evaluated from the aspects of source rocks, reservoir, seal and plays.
Zircon U-Pb dating indicates that the Badu and Chencai group were metamorphosed at about453-442Ma, and the syntectonic granites of Jinxi and Cizu were emplaced at about450Ma and430Ma respectively. Combined with available data of other metamorphic rocks and syntectonic granites as well as information about basin evolution, it is suggested that orogenic ativity mainly took place during455-425Ma, which was nearly coeval with the Caledonian orogeny. Based on above information and absent Pan-Africa orogeny in South China,1tentatively proposed that South China was near the Caledonian orogeny in Silurian, and place it to the north of the Greenland or the north of Scandinavian.
According to the analyses of strata correlation, thickness, sedimentary facies, subsidence and detrital zircon provenance, it is confirmed that the basin in the lower Yangtze region was a foreland basin during late Ordovician to Silurian, which was controlled by the early Paleozoic orogeny in South China. The foredeep was located in North Zhejiang and South Anhui, the forebulge along the Yangtze River, and the backbulge in the north of Jiangsu Provenance. Detrital zircon dating indicates the provenance of the foreland basin has five age populations,2500Ma,1800-2100Ma,900-1200Ma,40-860Ma and425-460Ma. The former three populations were derived from the recycling of the Proterozoic and early Paleozoic rocks in the orogenic belt, and the later two correlated well with the Neoproterozoic and early Paleozoic tectonic events, respectively. The youngest age of425Ma provided an age constrain for the timing of the foreland basin development. Combined with sedimentary features and provenance changes, it is proposed that the foreland basin was in underfilled stage during late Ordovician, filled stage in Llandovery, and overfilled stage in Wenlock.
It is revealed that the foreland basin has experienced two phases of compression during late Triassic and middle to late Jurassic and one phase of extension in late Cretaceous and Paleogene since it formed, according to the distribution of unconformity, the contact relationship of strata and rift basin development. The first compression was from NW toward SE and mainly influenced the area of north Yangtze River, while the late compression was from SE toward NW and mainly influenced the area in the south of Yangtze river. The formation of the basin can be divided into seven tectonic sequences, and from bottom to top they are Sinian-middle Ordovician, upper Ordovician-Silurian, upper Paleozoic-middle Triassic, upper Triassic-middle Jurassic, upper Jurassic-lower Cretaceous, upper Cretaceous-Paleogene and Neogene-Quaternary; according to deformation style and timing, ten tectonic units are divided, including Jiangnan belt, Jiangyin-Wuxi detachment folds, Changzhou-Xuancheng rift, Maoshan thrust belts, Nanling-Jurong rift, Niangzhen thrust belts, Tongling-Fanchang thrust belt, Chuzhou-Susong thrust belts and Subei rift basin.
Studies of source rocks, reservoir, seals and accumulation conditions of hydrocarbon reveal that the black shales of lower Cambrian and upper Ordovician-lower Silurian are thick, wide distribution, high in total organic carbon, and matured enough, which are favourable for shale gas exploration, and the Jiangyin-Wuxi area is the prospect play for the relatively simple structures.
引文
Bradley, D. C.2008. Passive margins through earth history. Earth-Science Reviews 91,1-26.
Cawood, P.A. & Nemchin, A.A.2001. Source regions for Laurentian margin sediments: constraints from U/Pb dating of detrital zircon in the Newfoundland Appalachians. Geological Society of America Bulletin,113:1234-1246.
Cawood, P. A., Nemchin, A. A., Strachan, R. A., Prave, T. & Rabbendam, M.2007. Sedimentary basin and detrital zircon record along East Laurentia and Baltica during assembly and breakup of Rodinia. Journal of the Geological Society, London,164: 257-275.
Charvet, J., Shu, L. S., Shi, Y. S., Guo, L. Z. & Faure, M.1996. The building of South China: collision of Yangtzi and Cathaysia blocks, problems and tentative answers. Journal of Southeast Asian Earth Sciences,13:223-235.
Charvet J., Shu L.S., Faure M., Choulet F., Wang B., Lu H.F., Breton N.L.2010. Structural development of the Lower Paleozoic belt of South China:genesis of an intracontinental orogen. J. Asian Earth Sci.,39:309-330.
Chen, J., Foland, K. A., Xing, F., Xu, X., Zhou, T.1991. Magmatism along the south-eastern margin of the Yangtze block:Precambrian collision of the Yangtze and Cathysia blocks of China. Geology,19:815-818.
Chen, X., Rowley, D., Rong, J., Zhang, J., Zhang, Y. & Zhan, R.1997. Late Precambrian through Early Palaeozoic stratigraphic and tectonic evolution of the Nanling Region, Hunan Province, South China. International Geology Review,39:469-478.
Chen, X., Rong, J. Y., Li, Y. & Boucot, A. J.2004. Facies patterns and geography of the Yangtze region, South China, through the Ordovicican and Silurian transition. Palaeogeography, Palaeoclimatology, Palaeoecology,204:353-372.
Chen, X., Zhou, Z. Y. & Fan, J. X.2010. Ordovician palaeogeography and tectonics of the major palaeoplates of China. In S. C. Finney & W. B. N. Berry (eds) The Ordovician Earth System. Geological Society of America, Special Papers, no.466:85-104.
Cocks, L. R. M. & Torsvic, T.H.2002. Earth geography from 500 to 400 million years ago:a faunal and palaeomagnetic review. Journal of the Geological Society, London 159: 631-644.
Cocks, L. R. M. & Torsvik, T. H.2011. The Palaeozoic geography of Laurentia and western Laurussia:A stable craton with mobile margins. Earth-Science Reviews,106:1-51.
Dewey, J. F. & Strachan, R. A.2003. Changing Silurian-Devonian relative plate motion in the Caledonides:sinistral transpression to sinistral transtension. Journal of the Geological Society, London,160:219-229.
Condie, K. C.2001. Continental growth during formation of Rodinia at 1.35-0.9Ga. Gondwana Research,4:5-16.
Curtis, J. B.2002. Fractured shale-gas systems. AAPG Bulletin,86(11):1921-1938.
Dalziel, I. W. D.1991. Pacific margins of Laurentia and East Antarctica—Australia as a conjugate rift pair:evidence and implications for an Eocambrian supercontinent. Geology,19:598-601.
Dalziel, I. W. D.1997. Neoproterozoic-Paleozoic geography and tectonics:review, hypothesis, environmental speculation. Geol. Soc. Am. Bull.109:16-42.
DeCelles, P. G., Giles, K. A.1996. Foreland basin systems. Basin Research,8:105-123.
Dewey, J. F. & Strachan, R. A.2005. Caledonides of Britain and Ireland. In Encyclopedia of Geology,56-63.
Dickinson, W. R.1974. Plate tectonics and sedimentation.Society of Economic Paleontologists and Mineralogists Special Publication,22:1-27.
EIA.2011a. Review of Emerging Resources:U.S. Shale Gas and Shale Oil Plays.1-105.
EIA.2011b. World shale gas resources:an intial assessment of 14 regions outside the united states.1-365.
Ettensohn, F. R.2004. Modeling the nature and development of major Paleozoic Clastic wedges in the Appalachian Basin, USA. Journal of Geodynamics,37:657-681.
Faure, M., Shu, L. S., Wang, B., Charvet, J., Choulet, F. & Monie, P.2009. Intracontinental subduction:a possiblemechanism for the Early Palaeozoic Orogen of SE China. Terra Nova,21:360-368.
Faure, M., Sun, Y., Shu, L., Monie, P. & Charvet, J.1996. Extensional tectonics within a subduction-type orogen:The case study of the Wugongshan dome (Jiangxi Province, southeastern China). Tectonophysics,263:77-106.
Fortey, R. A. & Cocks, L. R. M.2003. Palaeontological evidence bearing on global Ordovician-Silurian continental reconstructions. Earth-Sciences Reviews,61:245-307.
Gee, D. G., Fossen, H., Henriksen, N. & Higgins, A. K.2008. From the Early Paleozoic Platforms of Baltica and Laurentia to the Caledonide Orogen of Scandinavian and Greenland. Episodes,31:44-51.
Gilder, S., Leloup, P. H., Courtillot, V, Chen, Y, Coe, S. R., Zhao, X., Xiao, W., Halim, N., Cogne, J. P. & Zhu, R.1999. Tectonic evolution of the Tancheng-Lujiang (Tan-Lu) fault via Middle Triassic to early Cenozoic paleomagnetic data:Journal of Geophysical Research,104:365-390.
Greentree, M. R., Li, Z. X., Li, X. H. & Wu, H. C.2006. Late Mesoproterozoic to earliest Neoproterozoic basin record of the Sibao orogenesis in western South China and relationship to the assembly of Rodinia. Precambrian Research,151:79-100.
Hibbard, J. P., van Staal, C. R. & Rankin, D. W.2007. A Comparative Analysis of Pre-Silurian Crustal Building Blocks of the Northern and the Southern Appalachian Orogen. American Journal of Science,307:23-45.
Hibbard, J. P., van Staal, C. R. & Rankin, D. W.2010. Comparative analysis of the geological evolution of the northern and southern Appalachian orogen:Late Ordovician-Permian. In R. P. Tello, M. J. Bartholomew, J. P. Hibbard & P. M. Karabinos (eds.) From Rodinia to Pangea:The lithotectonic Record of the Appalachian Region. Geological Society of America, Memoir, no.206:51-69
Hoffman, P. F.1991. Did the breakout of Laurentia turn Gondwanaland inside-out? Science, 252:1409-1412.
Holland, C. H., Sanders, I. S. & Sanders, I.2009. The Geology of Ireland.1-568.
Huang, K., Opdyke, N. & Zhu, R. X.2000. Further paleomagnetic results from the Silurian of the Yangtze Block and their implications. Earth and Planetary Science Letter,175: 191-202.
Ingersoil, R.V.2011. Tectonics of sedimentary basins, with revised nomenclature. InCathy, B. & Antonio, A. P. (eds.) Tectonics of Sedimentary Basins:Recent Advances,3-43.
Jia, D., Wu, L., Li, H. and Deng, F.2009. Provenance of detrital zircons from the late Neoproterozoic to Ordovician sandstones of south China, Geochimica et Cosmochimica Acta,73(13S):A592.
Jia, D., Li, H., Wu, L. and Deng, F.2008. Timing of syn-tectonic granites in the early Paleozoic Wuyishan fold belt (south China) with tectonic implications,33rd International Geological Congress, Abstracts= Congres Geologique International, Resumes,33
Jiang, G., Kennedy, M. J. & Christie-Blick, N.2003. Stable isotopic evidence for methane seeps in Neoproterozoic postglacial cap carbonates. Nature,426:822-826.
Jarvie, D. M., Hill, R. J., Ruble, T. E. & Pollastro, R. M.2007. Unconventional shale-gassystems:The Mississippian Barnett Shale of noth-central Texas as one model for thermogenic shale-gas assessment. AAPG Bulletin,91(4):475-499.
Jiang, G., Sohl, L. E. & Christie-Blick, N.2003. Neoproterozoic stratigraphic comparison of the Lesser Himalaya (India) and Yangtze block (south China):Paleogeographic implications. Geology,31:917-920.
Johnson, D. D. & Beaumont, C.1995. Preliminary results from a planform kinematic model of orogen evolution, surface processes and the development of clastic foreland basin stratigraphy, in Dorobek, S.L.,and Ross, G.M. (eds.) Stratigraphic evolution of foreland basins. SEPM (Society for Sedimentary Geology) Special Publication,52:3-24.
Johnston, S. M., Hartz, E. H., Brueckner, H. K, & Gehrels, G. E.2010. U-Pb zircon geochronology and tectonostratigraphy of southern Liverpool Land, East Greenland: Implications for deformation in the overriding plates of continental collisions. EPSL,297: 512-524.
Keller, G. R. & Hatcher, R. D. J.1999. Some comparisons of the structure and evolution of the southern Appalachian-Ouachita orogen and portions of the Trans-European Suture Zone region. Tectonophysics,314:43-68.
Kneller, B. C.1991. A foreland basin on the southern margin of Iapetus. Geology,148:207-210.
Li, H. B., Jia, D., Wu, L., Zhang, Y., Yin, H. W., Wei, G. Q., Li, B. L.2013. Detrital zircon provenance of the Lower Yangtze foreland basin deposits:constraints on the evolution of the early Palaeozoic Wuyi-Yunkai orogenic belt in South China.Geological magazine, doi:10.1017/S0016756812000969..
Li, W. X., Li, X. H. & Li, Z. X.2005. Neoproterozoic bimodal magmatism in the Cathaysia Block of South China and its tectonic significance. Precambrian Research,136:51-66.
Li, W. X., Li, X. H., Li, Z. X. & Lou, F. S.2008a. Obduction-type granites within the NE Jiangxi ophiolite:Implications for the final amalgamation between the Yangtze and Cathaysia blocks. Gondwana Research,13:288-301.
Li, X. H., Li, W. X., Li, Z. X. & Liu, Y.2008b.850-790 Ma bimodal volcanic and intrusive rocks in northern Zhejiang, South China:A major episode of continental rift magmatism during the breakup of Rodinia. Lithos,102:341-57.
Li, X. H., Li, W.X., Li, Z. X., Lo, C.H., Wang, J., Ye, M. F. Yang, Y. H.2009. Amalgamation between the Yangtze and Cathaysia Blocks in South China:Constraints from SHRIMP U-Pb zircon ages, geochemistry and Nd-Hf isotopes of the Shuangxiwu volcanic rocks. Precambrian Research,174:117-128.
Li, Z. X., Bogdanova, S.V., Collins, A.S., Davidson, A., De, W.B., Ernst, R.E., Fitzsimons, I.C., Fuck, R.A., Gladkochub, D.P., Jacobs, J., Karlstrom, K.E., Lu, S., Natapov, L.M., Pease, V, Pisarevsky, S.A., Thrane, K. & Vernikovsky, V.2008c. Assembly, Configuration, and Break-Up History of Rodinia:A Synthesis. Precambrian Research, 160(1-2):179-210.
Li, Z. X.1994. Collision between the North and South China blocks:A crustal-detachment model for suturing in the region east of the Tanlu fault. Geology,22:739-742.
Li, Z. X., Li, X. H., Zhou, H. W. & Kinny, P. D.2002. Grenvillian continental collision in South China:New SHRIMP U-Pb zircon results and implications for the configuration of Rodinia. Geology,30:163-166.
Li, Z. X., Li, X. H., Kinny, P. D., Wang, J., Zhang, S. & Zhou, H.2003. Geochronology of Neoproterozoic syn-rift magmatism in the Yangtze Craton, South China and correlations with other continents:evidence for a mantle superplume that broke up Rodinia. Precambrian Research,122:85-109.
Li, Z. X., Zhang, L. & Powell, C. M.1995. South China in Rodinia:Part of the Missing Link Between Australia-East Antarctica and Laurentia? Geology,23(5):407-410.
Li, Z. X.1998. Tectonic history of the major East Asian lithospheric blocks since the mid-Proterozoic-A synthesis:American Geophysical Union Geodynamics Series,27: 221-243.
Li, Z. X. & Li, X. H.2007. Formation of the 1300 km-wide intracontinental orogen and postorogenic magmatic province in Mesozoic South China A flat-slab subduction model. Geology,35:179-182.
Li, Z. X., Li, X. H., Wartho, J. A., Clark, C., Li, W. X., Zhang, C. L. & Bao, C.2010. Magmatic an metamorphic events during the early Palaeozoic Wuyi-Yunkai orogeny, southeastern South China:new age constraints and pressure-temperature conditions. Geological Society of America Bulletin,122:772-793.
Ludwig, K. R.1999. User's Manual for Isoplot/Ex, V2.06, a Geochronological Tookit for Microsoft Excel. In Berkely Geochronological Center Special Publication.
Macqueen, R. W. & Leekie, D. A.1992. Forelnad Basins and Fold Belt. AAPG Memoir 55. 1-456.
Mann P, Gahagan L, Gordon M B.2003.Tectonic setting of the world's giant oil and gas fields. In Halbouty M. T. (eds.) Giant Oil and Gas Fields of the Decade 1990-1999, AAPG Memoir 78:15-105.
Martini, A. M., Walter, L. M., Budai, J. M., Ku, T. C. W., Kaiser, C. J. & Schoell, M.1998. Genetic and temporal relations between formation waters and biogenic methane-Upper Devonian Antrim Shale, Michigan basin, USA. Geochimica et Cosmochimica Acta, 62(10):1699-1720.
Maruyama, S.1997. Pacific-type orogeny revisited:Miyashiro-type orogeny proposed. Isl. Arc,6:91-120.
McKerrow, W. S., MacNiociall, C. & Dewey, J. F.2000. The Caledonian Orogeny redefined. Journal of the Geological Society, London,157:1149-1154.
Metcalfe, I.1996. Gondwana dispersion, and Asian accretion and evolution of eastern Tethys. Australian Journal of Earth Sciences,43:605-623.
Moores, E. M.1991. Southwest U.S.-East Antarctic (SWEAT) connection:a hypothesis. Geology,19:425-428.
Mosher, S.1998. Tectonic evolution of the southern Laurentian Grenville orogenic belt: Geological Society of America Bulletin,110:1357-1375.
Northrup, C. J., Royden, L. H. & Burchfiel, B. C.1995. Motion of the Pacific plate relative to Eurasia and its potential relation to Cenozoic extension along the eastern margin of Eurasia. Geology,23(8):719-722.
Opdyke, N. D., Huang, K., Xu, G., Zhang, W. Y. & Kent, D. V.1987. Paleomagnetic results from the Silurian of the Yangtze paraplatform.Tectonophysics,139:123-132.
Qiu, Y. M., Gao, S., McNaughton, N. J., Groves, D. I. & Ling, W. L.2000. First evidence of >3.2 Ga continental crust in the Yangtze Craton of south China and its implications for Archean crustal evolution and Phanerozoic tectonics. Geology,28:11-14.
Rey, P., Burg, J. P. Casey M.1997. The Scandinavian Caledonides and their relationship to the Variscan belt. In Burg, J.P. & Ford, M. (eds) Orogeny Through Time. Spec. Publ. Geol. Soc. London:179-200.
Rino, S., Kon, Y., Sato, W., Maruyama, S., Santosh, M & Zhao, D.2008. The Grenvillian and Pan-African orogens:World's largest orogenies through geologic time, and their implications on the origin of superplume. Gondwana Research,14:51-72.
Roberts, D.2003. The Scandinavian Caledonides:event chronology, palaeogeographic settings and likely modern analogues. Tectonophysics,365:283-299.
Rogers, J. J. W., Santosh, M.2002. Configuration of Columbia, a Mesoproterozoic Supercontinent. Gondwana Research,5:5-22.
Rong, J. Y, Chen, X., Zheng, S. Y., Ni, Y. N., Zhan, R. B., Chen, T. E., Fu, L. P., Li, R. Y.& Fan, J. X.2003. Silurian Palaeogeography of China. In Landing, E.&Johnson, M. E. (eds.) Silurian Lands and Seas, Palaeogeography Outside of Laurentia New York State Museum Bulletin, no.493:243-98.
Schwab, F. L.1976. Modern and ancient sedimentary basins:comparative accumulation rates. Geology,4:723-727.
Shu, L. S., Faure, M., Wang, B., Zhou, X. M., Song, B.2008. Late Palaeozoic-Early Mesozoic geological features of South China:Response to the Indosinian collision events in Southeast Asia. C.R. Geoscience,340:151-165.
Sinclair, H.D.1997. Tectonostratigraphic model for underfilled peripheral foreland basins:an Alpine perspective. Geological Society of America Bulletin,109:324-346.
Stephenson, D., Bevins, R. E, Millward, D., Stone, P., Parsons, I., Highton, A. J. & Wadsworth, W. J.2000. Caledonian Igneous Rocks of Great Britain. Geological Conservation Review Series, No.17:1-648.
Tapponnier, P., Peltzer, G., Le Dain, A. Y., Armijo, R. & Cobbold, P.1982. Propagating extrusion tectonics in Asia:New insights from simple experiments with plasticine: Geology,10:611-616.
Tucker, R. D., Robinson, P., Solli, A., Gee, D. G., Thorsnes, T., Krogh, T.E., Nordgulen, Q. & Bickford, M. E.2004. Thrusting and extension in the Scandian Hinterland, Norway:New U-Pb ages and Tectonostratigraphic evidence. American Journal of Science,304: 477-532.
Veevers J J.2007. Pan-Gondwanaland Post-Collisional Extension Marked by 650-500 Ma Alkaline Rocks and Carbonatites and Related Detrital Zircons:A Review. Earth-Science Reviews,83(1-2):1-47.
Vergel, P., Hou, J. M., Wang Y. M. & Mercier, J. L.2007. The kinematics of the Tan-Lu Fault zone during the Mesozoic-Palaeocen and its relations with the North China-South China block collision (Anhui Province, China). Bulletin Society geology France,178:353-365.
Wan, Y. S., Liu, D., Xu, M., Zhuang, J., Song, B., Shi, Y. & Du, L.2007. SHRIMP U-Pb zircon geochronology and geochemistry of metavolcanic and metasedimentary rocks in NW Fujian, Cathaysian block, China:tectonic implications and the need to redefine lithostratigraphic units. Gondwana Research,12:166-183.
Wan, Y. S., Liu, D. Y., Wilde, S. A., Cao, J. J., Chen, B., Dong, C. Y., Song, B. & Du, L. L. 2010. Evolution of the Yunkai Terrane, South China:evidence from SHRIMP zircon U-Pb dating, geochemistry and Nd isotope. Journal of Asian Earth Sciences,37:140-153.
Wang, X. L., Zhou, J. C., Qiu, J. S., Zhang, W. L., Liu, X. M. & Zhang, G. L.2006. LA-ICP-MS zircon geochronology of the Neoproterozoic igneous rocks from Northern Guangxi, South China:Implications for tectonic evolution. Precambrian Research,145: 111-130.
Wang, X. L., Zhou, J. C., Griffin,W. L., Wang, R. C., Qiu, J. S., O'Reilly, S. Y., Xu, X. S., Liu, X. M. & Zhang, G. L.2007a. Detrital zircon geochronology of Precambrian basement sequences in the Jiangnan orogen:dating the assembly of the Yangtze and Cathaysia Blocks. Precambrian Research,159:117-131.
Wang, Y. J., Fan, W. M., Zhao, G. C., Ji, S. C. & Peng, T. P.2007b. Zircon U-Pb geochronology of gneissic rocks in the Yunkai massif and its implications on the Caledonian event in the South China Block. Gondwana Research,12:404-416.
Wang, Y.J., Zhang, F.F., Fan,W.M., Zhang, G.W., Chen, S.Y., Cawood, P.A., Zhang, A.M., 2010. Tectonic setting of the South China Block in the early Paleozoic:resolving intracontinental and ocean closure models from detrital zircon U-Pb geochronology. Tectonics,29. doi:10.1029/2010TC002750.
Wang, Y. J., Zhang, A. M., Fan, W. M., Zhao, G. C., Zhang, G.W., Zhang, Y. Z., Zhang, F. F. & Li, S. Z.2011. Kwangsian crustal anatexis within the eastern South China Block: Geochemical, zircon U-Pb geochronological and Hf isotopic fingerprints from the gneissoid granites of Wugong and Wuyi-Yunkai Domains. Lithos,127:239-60.
Wang, J. & Li, Z. X.2003. History of Neoproterozoic rift basins in South China:implications for Rodinia break-up. Precambrian Research,122:141-58.
Wu, L., Jia, D., Li, H.B., Deng, F. & Li, Y.Q.2010. Provenance of Detrital Zircons From the Late Neoproterozoic to Ordovician Sandstones of South China:Implications for its Continental Affinity. Geological Magazine,147(6):974-980.
Xiao, W. J., He, A. Q.2005. Early Mesozoic thrust tectonics of the northwest Zhejiang region (Southeast China). Geological Society of America Bulletin,117 (7-8):945-961.
Xu, X. B., Zhang Y. Q., Shu L. S., Jia D.2011. La-ICP-MS U-Pb and 40Ar/39Ar geochronology of the sheared metamorphic rocks in the Wuyishan:Constraints on the timing of Early Paleozoic and Early Mesozoic tectono-thermal events in SE China. Tectonophysics,501:71-86.
Xu, X. S., Suzuki, K, Liu, L. & Wang, D. Z.2010. Petrogenesis and tectonic implications of Late Mesozoic granites in the NE Yangtze Block, China:further insights from the Jiuhuashan-Qingyang complex. Geological Magazine,147(2):219-232.
Yan, D. P., Zhou, M. F., Song, H.L., Wang, X.W. & Malpas, J.2003. Origin and tectonic significance of a Mesozoic multi-layer over-thrusting system within the Yangtze Block (South China). Tectonophysics,361:239-254.
Yang, Z. Y., Sun, Z. M., Yang, T.S. & Pei, J. L.2004. A Long Connection (750-380 Ma) Between South China and Australia:Paleomagnetic Constraints. Earth and Planetary Science Letters,220(3-4):423-434.
Yao, J. L., Shu, L. S. & Santosh, M.2011. Detrital zircon U-Pb geochronology, Hf-isotopes and geochemistry-New clues for the Precambrian crustal evolution of Cathaysia Block, South China. Gondwana Research,20:553-567.
Ye, M. F., Li, X. H., Li, W. X., Liu, Y. & Li, Z. X.2007. SHRIMP zircon U-Pb geochronological and whole-rock geochemical evidence for an early Neoproterozoic Sibaoan magmatic arc along the southeastern margin of the Yangtze Block. Gondwana Research,12:144-156.
Yin, A. & Nie, S.1993. An indentation model for the north and south China collision and the development of the Tan-Lu and Honam fault systems, eastern China. Tectonics,12: 801-813.
Yu, J. H., O'Reilly, S. Y., Wang, L. J., Griffin,W. L., Zhang, M., Wang, R. C., Jiang, S. Y. & Shu, L. S.2008. Where was South China in the Rodinia supercontinent? Evidence from U-Pb geochronology and Hf isotopes of detrital zircons. Precambrian Research,164: 1-15.
Yu, J. H., Wang, L. J., Griffin, W. L., O'Reilly, S.Y., Zhang, M., Li, C.Z. & Shu, L.S.2009. A Paleoproterozoic orogeny recorded in a long-lived cratonic remnant (Wuyishan terrane), eastern Cathaysia Block, China. Precambrian Reseach,174:347-363.
Zhang S.B., Zheng, Y.F., Wu, Y.B., Zhao, Z.F., Gao, S. & Wu, F.Y.2006. Zircon Isotope Evidence for≥3.5 Ga Continental Crust in the Yangtze Craton of China. Precambrian Research,146(1-2):16-34.
Zhao, J. H., Zhou, M. F., Yan, D. P., Zheng, J. P. & Li, J.W.2011. Reappraisal of the Ages of Neoproterozoic Strata in South:No connection with the Grenville orogeny. Geology, 39(4):299-302.
Zheng, J., Griffin, W.L., O'Reilly, S.Y., Zhang, M.2006. Pearson N & Pan Y Widespread Archean Basement Beneath the Yangtze Craton. Geology,34(6):417-420.
Zheng, Y. F., Wu, R. X., Wu, Y. B., Zhang, S. B., Yuan, H. L. & Wu, F. Y.2008. Rift melting of juvenile arc-derived crust:Geochemical evidence from Neoproterozoic volcanic and granitic rocks in the Jiangnan Orogen, South China. Precambrian Research,163:351-83.
Zhou, X.M. & Li, X. W.2003. Origin of late Mesozoic igneous rocks in Southeastern China: implications for lithosphere subduction and underplating of mafic magmas. Tectonophyics,326:269-287.
Zhou, J. C., Wang, X. L. & Qiu, J. S.2009. Geochronology of Neoproterozoic mafic rocks and sandstones from northeastern Guizhou, South China:Coeval arc magmatism and sedimentation. Precambrian Research,170:27-42.
安徽省地质矿产局.1987.安徽省区域地质志.北京：地质出版社,1-721.
敖振宽.1956.试论中国地台南部加里东运动的影响及其大地构造发展史.地质学报,36(3)：273-298.
蔡东升,施央申,卢华复,董火根.1993.苏州西南部的推覆和伸展构造.大地构造与成矿学,6：163-178.
陈安定.2001.苏北箕状断陷形成的动力学机制.高校地质学报,7(4)：408-418.
陈旭,李积金,耿良玉,丘金玉,倪寓南,杨学长.1988.江苏下扬子地区的志留系.见：江苏石油勘探局地质科学研究院,中国科学院南京地质古生物研究所主编.江苏地区下扬子准地台震旦纪-三叠纪生物地层,127-168.
陈旭,戎嘉余,Rowley, D. B.,张进,张元动,詹仁斌.1995.对华南早古生代板溪洋的质疑.地质评论,41(5)：389-400.
陈旭,张元动,樊隽轩,成俊峰,李启剑.2010.赣南奥陶纪笔石地层序列与广西运动.中国科学：地球科学,40(12)：1621-1631.
陈正宏,李寄嵎,谢佩珊,曾雯,周汉文.2008.利用EMP独居石定年法探讨浙闽武夷山地区变质基底岩石与花岗岩的年龄.高校地质学报,14(1)：1-15.
陈志洪,邢光福,郭坤一,董永观,陈荣,曾勇,李龙明,贺振宇,赵玲.2009.浙江平水群角斑岩的成因：锆石U-Pb年龄和Hf同位素制约.科学通报,54(5)：610-617.
陈祖兴,徐明.1999.鹅婆复式深成岩体成岩时代初探,江西地质,13(2)：100-105.
邓必荣,石鉴东.2000.兴国杨村岩体特征及侵位机制探讨.华东地质学院学报.23(2)：141-145.
董大忠,邹才能,李建忠,王社教,李新景,王玉满,李登华,黄金亮.2011.页岩气资源潜力与勘探开发前景.地质通报,30(2-3)：325-336.
董树文,方景爽,李勇,朱洪吉,Schneider, W., Breitkreuz, H. & Mattern, F.1994下扬子中三叠世-中侏罗世沉积相与印支运动.地质论评,40(2)：111-119.
范代读,李从先,蔡进功,邓兵,罗璋.2003.浙江桐庐晚奥陶世晚期沉积层序和沉积环境分析.沉积学报,21(2)：247-254.
方晓思,何胜策.1988.浙西唐家坞组的微古植物及其时代.地质论评,34(4)：327-335.
方一亭,边立曾,俞剑华,冯洪真.1993.晚奥陶世五峰期扬子板块沉积模式.沉积学报,11(3)：7-12.
冯增昭,彭勇民,金振奎,蒋盘良,鲍志东,罗璋,鞠天吟,田海芹,汪红.2001.中国南方寒武纪和奥陶纪岩相古地理.北京：地质出版社,1-239.
冯增昭,彭勇民,金振奎,鲍志东.2004.中国寒武纪和奥陶纪岩相古地理.北京：石油工业出版社,1-233.
甘晓春,季惠民,孙大中,金文山,赵凤清.1995.浙西南早元古代花岗质岩石的年代.岩石矿物学杂志,14(1)：1-8.
甘晓春,季惠民,孙大中,庄建民.1993.闽北前寒武纪基底的地质年代学研究.福建地质,12(1)：17-32.
高振中,何幼斌,李罗照,卿崇文,肖明国,程四洪,张文成,刘伟伟.2008.中国南方上奥陶统五峰组观音桥段成因讨论：是浅水介壳相还是深水异地沉积?古地理学报,10(5)：487-494.
葛肖虹.1987.论宁镇山脉推覆构造的特征与形成.吉林大学学报(地球科学版),2(2)：143-154.
关尹文,丘元禧,顾宝荣.1959.浙西、皖南上奥陶系复理石建造的发现.地质学报,39(2)：187-212.
郭福祥.1998.中国南方中新生代大地构造属性和南华造山带褶皱过程.地质学报,72(1)：25-33.
郭令智,俞剑华,施央申.1965.华南加里东地槽褶皱区大地构造发展的基本特征.中国大地构造问题.北京：北京科学出版社,165-183.
郭令智,施央申,马瑞士.1980.华南大地构造格架和地壳演化.国际交流地质学术论文集.北京：地质出版社,109-116.
郭令智,施央申,孙岩.1988.下扬子区前陆盆地逆冲推覆构造的研究.南京大学学报(自然科学版),24(1)：1-9.
郭令智,施央申,卢华复,马瑞士,董火根.1990.武夷-云开震旦纪-早古生代沟、弧、盆褶皱系.造山带-盆地环太平洋构造论文集.北京：地质出版社,1-116.
何为红.2002.扬子海盆晚奥陶世晚期至志留纪初期海平面升降与奥陶／志留系界限的划分与对比.中国地质科学院博士学位论文,1-69.
侯明金,朱光,Mercier, J., Vergely, P.,王永敏.2007.郯庐断裂带(安徽段)及邻区的动力学分析与区域构造演化.地质科学,42(2)：362-381.
胡恭任,于瑞莲,刘丛强.2001.江西省金溪-南城混合岩和花岗岩的岩石地球化学及同位素地球化学研究.岩石矿物学杂志,20(2)：103-111.
胡受奚,叶瑛.2006.对“华夏古陆”、“华夏地块”及“扬子-华夏古陆统一体”等观点的质疑.高校地质学报,12(4)：432-439.
胡雄健,许金坤,康海男,童朝旭,陈程华,叶国贵.1991.浙西南下元古界八都群的地质特征及意义.中国区域地质,3：234-240.
胡雄健.1994.浙西南下元古界八都群的地质年代学.地球化学,23：18-24.
胡艳华,顾明光,徐岩,余盛强,王加恩,贺跃.2011.浙江诸暨地区陈蔡群加里东期变质年龄的确认及其地质意义.地质通报,30(11)：1661-1670.
黄汲清.1941.江南大陆—扬子江以南之加里东山脉.地质论评,6(Z2)：293-294.
黄汲清.1960.中国地质构造基本特征的初步总结.地质学报,40(1)：1-32.
黄钟瑾,沈修志,孙岩.1984.苏、皖、浙交界逆掩-推覆构造及构造分带性的成因研究.南京大学学报,2：335-344.
黄钟瑾,沈修志,孙岩.1987.江苏靖江一苏州地区侏罗山式褶皱及滑脱断层的研究.山东矿业学院学报,1：58-64.
黄志诚,黄钟瑾,陈智娜.1991.下扬子区五峰组火山碎屑岩与放射虫硅质岩.沉积学报,9(2)：1-13.
贾东,武龙,闫兵,李海滨,李一泉,王毛毛.2011.全球大型油气田的盆地类型与分布规律.高校地质学报,17(2)：170-184.
贾承造,何登发,雷振宇,周路,贾进斗,王桂宏.2000.前陆冲断带油气勘探.北京：石油工业出版社,1-351.
晋慧娟,李育慈.1998.浙西上奥陶统于潜组Spirodesmos遗迹化石组合的环境意义.地质科学,33(3)：282-289.
江苏省地质局.1976.无锡-苏州幅1：20万区域地质调查报告.
江苏省地质矿产局.1984.江苏省及上海市区域地质志.北京：地质出版社,1-857.
江苏省地质矿产局.1989.宁镇山脉地质志.南京：江苏科学技术出版社,1-505.
江西省地质矿产局.1984.江西省地质矿产局.北京：地质出版社,1-921.
孔祥生,李志飞,冯长根,顾明光,马剑萍.1995.浙江陈蔡地区前寒武纪地质.北京： 地质出版社,1-136.
李本亮,魏国齐,贾承造.2009.中国前陆盆地构造地质特征综述与油气勘探.地学前缘,16(4)：190-202.
李海滨,贾东,武龙,张勇.2011.下扬子地区中-新生代的挤压变形与伸展改造及其油气勘探意义.岩石学报,27(3)：770-778.
李继亮,陈昌明,高文学,陈瑞君,黄家宽,田兴有,刘杰汉.1978.我国几个地区浊积岩系的特征.地质科学,1(1)：26-44.
李献华.2000.赣东北蛇绿混杂岩带中硅质岩的地球化学特征及构造意义.中国科学D辑,30(3)：284-290.
李志才.1982.广西加里东运动的特征及其对区域地质区域成矿的重要.中国区域地质,1：8-54.
梁狄刚,郭彤楼,陈建平,边立曾,赵喆.2008.南方四套区域性海相烃源岩的分布.海相油气地质,13(2)：1-16.
梁狄刚,郭彤楼,陈建平,边立曾,赵喆.2009.南方四套区域性海相烃源岩的地球化学特征.海相油气地质,14(1)：1-13.
吕洪波,夏邦栋.1987.浙西上奥陶统复理石韵律的马尔可夫链模拟.石油与天然气地质,8(2)：219-230.
刘宝珺,许效松,杏南.1993.古大陆沉积地壳演化与成矿,北京：科学出版社1-236.
刘宝珺,许效松.1994.中国南方岩相古地理图集(震旦纪—三叠纪).北京：科学出版社,1-188.
刘锐,周汉文,张利,钟增球,曾雯,向华,靳松,吕新前,李春忠.2009.华夏地块古元古代陆壳再造：锆石微量元素与U-Pb和Lu-Hf同位素证据.科学通报,54(7)：906-917.
刘晓,张元动,周传明.2012.浙西北上奥陶统文昌组和堰口组沉积特征及其意义.古地理学报,14(1)：101-116.
刘小平,潘继平,董清源,刘东鹰,段宏亮,李华东,董谦.2011.苏北地区古生界页岩气形成地质条件.天然气地质科学,22(6)：1100-1108.
卢华复.2006.关于华夏古陆.高校地质学报,12(4)：413-417.
马力,陈焕疆,甘克文,徐克定,许效松,吴根耀.2004.中国南方大地构造和海相油 气地质(上册).北京：地质出版社,1-451.
马瑞士.2006.华南构造演化新思考兼论“华夏古陆”说中的几个问题.高校地质学报,12(4)：448-456.
马永生,陈洪德,王国力.2009.中国南方层序地层与古地理.北京：科学出版社,1-603.
穆恩之.1954.论五峰页岩.古生物学报,2(2)：153-170.
南京大学地质系.1981.华南不同时代花岗岩类及其成矿关系.北京：科学出版社,1-395.
彭亚鸣,苏丽美.1983.中国东南部加里东期花岗岩的特征和成因.南京大学学报,1：140-152.
邱旭明,刘玉瑞,傅强.2006.苏北盆地上白垩统-第三系层序地层与沉积演化.北京：地质出版社,1-154.
任纪舜.1960.试论中国东南部的大地构造性质.地质论评.20(3)：132-133.
任纪舜.1964.中国东南部泥盆纪前几个大地构造问题的初步探讨.地质学报,44(4)：418-432.
任纪舜.1990.论中国南部的大地构造.地质学报,4：275-288.
戎嘉余,陈旭.1987.华南晚奥陶世的动物群分异及生物相、岩相分布模式.古生物学报,26(5)：507-535.
戎嘉余,詹仁斌,许红根,黄冰,俞国华.2010.华夏古陆于奥陶-志留纪之交的扩展证据和机制探索.中国科学,40(1)：1-17.
沈修志,孙岩,黄钟瑾,杜定全,熊斌辉.1986.江苏宜兴地区推覆构造的发现及其油气勘探的意义.南京大学学报,22(3)：510-518..
舒良树,卢华复,贾东,夏菲,福赫.1999.华南武夷山早古生代构造事件的40Ar/39Ar同位素年龄研究.南京大学学报(自然科学版),35(6)：668-674.
舒良树.2006.华南前泥盆纪构造演化：从华夏地块到加里东期造山带.高校地质学报,12(4)：418-431.
舒良树,于津海,贾东,王博,沈渭洲,张岳桥.2008.华南东段早古生代造山带研究.地质通报,27(10)：1581-1593.
舒良树.2012.华南构造演化的基本特征.地质通报,31(7)：1035-2053.
孙涛.2006.新编华南花岗岩分布图及其说明.地质通报,25(3)：332-337.
苏浙皖闽油气区石油地质志编写组.1992.中国石油地质志卷8苏浙皖闽油气区.北京：石油工业出版社,1-615.
唐显春,曾辉,张培先,汪凯明,何贵松.2011.宣城地区荷塘组页岩含气性浅析.油气藏评价与开发,1(1-2)：78-84.
涂荫玖,刘湘培,汪祥云,吴明安.2001.下扬子北缘滁州—巢湖前陆褶皱冲断带研究.大地构造与成矿学,25(1)：9-26.
王德滋,林承毅,周新民.1978.江西慈竹英云闪长岩体及其周围区域变质岩石的成因.南京大学学报,1：81-99.
王鸿祯.1985.中国古地理图集.北京：地图出版社,1-143.
王剑.2000.华南新元古代裂谷盆地沉积演化-兼论与Rodinia解体的关系.北京：地质出版社,1-146.
王金权.2006.皖南休宁新元古界-下寒武统沉积岩的有机碳同位素记录.古生物学报,45(4)：568-579.
王金渝,周荔青,郭念发,杨方子.2000.苏浙皖石油天然气地质.北京：石油工业出版社,1-234.
王俊卿.1997.苏皖志留纪鱼群及相关问题讨论.古脊椎动物学报,35(4)：307-311.
王涛,王晓霞,郑亚东,洪大卫,王新社.2007.花岗岩构造研究及花岗岩构造动力学刍议.地质科学,42(1)：91-113.
王茵,曾勇,陈松.2007.安徽巢北地区下志留统坟头组沉积环境分析.安徽地质,17(3)：166-170.
王玉净,张元动.2011.江苏仑山地区上奥陶统五峰组放射虫动物群及其地质意义.微体古生物学报,28(3)：251-260.
汪新伟,沃玉进,张荣强.2008.扬子克拉通南华纪-早古生代的构造-沉积旋回.现代地质,22(4)：525-533.
武龙.2011.华南陆块早古生代构造—沉积演化及大陆亲缘性分析.南京大学硕士论文.
夏邦栋.1986.一个加里东期的裂陷槽—对浙西早古生代沉积盆地成因类型的新认识.石油实验地质,8(1)：8-21.
夏邦栋,吕洪波.1988a.浙西皖南晚奥陶世复理石的沉积环境,兼谈鲍马层序应用问题.沉积学报,6(4)：44-51.
夏邦栋,吕洪波.1988b.苏、浙、皖地区沉积-大地构造演化.地质学报,4：301-310.
夏邦栋,吕洪波.1990.一个已埋藏的古造山带探讨.沉积学报,8(2)：1-8.
夏树芳.1978.苏南、浙北、皖南地区志留系与泥盆系的分界问题.地层学杂志,2(2)： 152-159.
向磊,舒良树.2010.华南东段前泥盆纪构造演化：来自碎屑锆石的证据.中国科学地球科学,40(10)：1377-1388.
肖传桃,姜衍文,朱忠德,李艺斌,潘云唐.1996.湖北宜昌地区奥陶纪层序地层及扬子地区五峰组沉积环境的讨论.高校地质学报,12(3)：339-347.
熊振.2010.南京地区地震构造环境研究.中国地震局地球物理研究所博士论文,1-130.
徐克勤,刘英俊,俞受鉴,王鹤年,魏秀喆.1960.江西南部加里东期花岗岩的发现.地质论评,3：112-114.
徐论勋,肖传桃,龚文平,何幼斌.2004.论扬子地区上奥陶统五峰组观音桥段的深海成因.地质学报,78(6)：726-732.
徐先兵,张岳桥,舒良树,贾东,王瑞瑞,许怀智.2010.武夷山地区前寒武纪地层沉积时代研究.地层学杂志,34(92)：254-267.
徐学思.1997.江苏省岩石地层.北京：中国地质大学出版社,1-288.
薛怀民,马芳,宋永勤,谢亚平.2010.江南造山带东段新元古代花岗岩组合的年代学和地球化学：对扬子与华夏地块拼合时间与过程的约束.岩石学报,26(11)：3215-3244.
薛耀松,俞从流.1979.浙西、赣东北寒武系下统荷塘组岩石特征及沉积环境分析.地层学杂志,3(4)：283-295.
姚保华,章振铨,王家林,火恩杰,张先康,刘保金,吴健生,王夫运,于鹏,王雅萍.2007.上海地区地壳精细结构的综合地球物理探测研究.地球物理学报,50(2)：482-491.
姚柏平,陆红,郭念发.1999.论下扬子地区多期构造格局叠加及其油气地质意义.石油勘探与开发,26(4)：10-13.
闫峻,刘海泉,宋传中,徐夕生,安亚军,刘佳,戴立群.2009.长江中下游繁昌-宁芜火山盆地火山岩锆石U-Pb年代学及其地质意义.科学通报,54(12)：1716-1724.
杨树锋,陈汉林,武光海.1995.闽北早古生代岛弧火山岩的发现及其大地构造意义.地质科学,30(2)：105-116
杨树锋,顾光明,卢成忠.2009.浙江章村地区中元古代岛弧火山岩的地球化学及构造意义.吉林大学学报,39(4)：689-698.
页岩气地质与勘探开发实践从书编委会.2009.北美地区页岩气勘探开发新进展.北京：石油工业出版社,1-271.
尹赞勋.1949.中国南部志留纪地层之分类与对比.中国地质学会会志第29卷,1-61.
俞凯,郭念发.2001.下扬子区下古生界油气地质条件评价.石油实验地质,23(1)：41-47.
岳文浙,业治铮.1996.扬子陆块东南缘早古生代的巨型斜坡带.江苏地质,20(1)：9-17.
曾萍.2007.G78区域大剖面综合解释与苏北盆地构造特征.石油天然气学报,29(3)：82-86.
赵风清.1999.华夏地块前加里东期变质基底的年代构造格架.前寒武纪研究进展,22(2)：39-46.
赵国春,孙德有,贺同兴.1994.陈蔡群构造变形特征及变形时代讨论.浙江地质,10(1)：38-46.
张爱梅,王岳军,范蔚茗,张菲菲,张玉芝.2010.闽西南清流地区加里东期花岗岩锆石U-Pb年代学及Hf同位素组成研究.大地构造与成矿学,34(3)：408-418.
张芳荣.2011.江西中-南部加里东期花岗岩地质地球化学特征及其成因.南京大学博士论文,1-115.
张菲菲,王岳军,范蔚茗,张爱梅,张玉芝.2010.湘东-赣西地区早古生代晚期花岗岩体的LA-ICPMS锆石U-Pb定年研究.地球化学,39(5)：414-426.
张淮,郭念发.2004.苏北盆地黄桥CO2气田储集层裂隙特征.江苏地质,28(4)：201-206.
张开均,施央申.1993.安徽下扬子区北缘薄皮构造研究.南京大学学报(自然科学版),29(3)：468-477.
张妮.2009.江苏侏罗系-白垩系火山岩地层对比及划分探讨.地层学杂志,33(1)：91-97.
张旗,金惟俊,李承东,王元龙.2009.中国东部燕山期大规模岩浆活动与岩石圈减薄：与大火成岩省的关系.地学前缘,16(2)：21-51.
张文佑,张步春,李荫槐.1974.中国大地构造基本特征及其发展的初步探讨.地质科学,1(1)：1-15.
张苑,舒良树,陈祥云.2011.华南早古生代花岗岩的地球化学、年代学及其成因研究—以赣中南为例.中国科学,41(98)：1061-1079.
张永军,黄钟瑾.1998.张八岭推覆体特征及其成因机制.高校地质学报,4(4)：444-451.
张岳桥,徐先兵,贾东,舒良舒,王瑞瑞.2009.华南早中生代从印支期碰撞构造体系向燕山期俯冲构造体系转换的形变记录.地学前缘,16(1)：234-247.
浙江省地质局.1966.区域地质矿产调查报告金华幅,1-117.
浙江省地质矿产局.1989.浙江省区域地质志,北京：地质出版社,1-688.
浙江省地质矿产局.2008.浙江省岩石地层.武汉：中国地质大学出版社,1-236.
钟华邦.1991.对茅山群时代的新认识.中国区域地质,4：366-372.
周金城,王孝磊,邱检生.2008.江南造山带是否格林威尔期造山带?—关于华南前寒武纪地质的几个问题.高校地质学报,14(1)：64-72.
周新民.2003.对华南花岗岩研究的若干思考.高校地质学报,9(4)：556-565.
朱光,朱光,徐嘉炜,刘国生,李双应,虞培玉.1998.下扬子地区沿江前陆盆地形成的构造控制.地质论评,44(2)：120-119.
朱光,刘国生.2000.皖南江南陆内造山带的基本特征.大地构造与成矿学,84(2)：103-111.
朱光,王勇生,王道轩,牛漫兰,刘国生,谢成龙.2006.前陆沉积与变形对郯庐断裂带同造山运动的制约.地质科学,41(1)：102-121.
朱兆玲,林焕令,章森桂.1988.江苏地区下扬子准地台寒武纪生物地层.江苏地区下扬子准地台震旦纪-三叠纪生物,35-80.
邹才能.2011.非常规油气地质.北京：地质出版社,1-310.
Cawood, P.A. & Nemchin, A.A.2001. Source regions for Laurentian margin sediments: constraints from U/Pb dating of detrital zircon in the Newfoundland Appalachians. Geological Society of America Bulletin,113:1234-1246.
Cawood, P. A., Nemchin, A. A., Strachan, R. A., Prave, T. & Rabbendam, M.2007. Sedimentary basin and detrital zircon record along East Laurentia and Baltica during assembly and breakup of Rodinia. Journal of the Geological Society, London,164: 257-275.
Charvet, J., Shu, L. S., Shi, Y. S., Guo, L. Z. & Faure, M.1996. The building of South China: collision of Yangtzi and Cathaysia blocks, problems and tentative answers. Journal of Southeast Asian Earth Sciences,13:223-235.
Charvet J., Shu L.S., Faure M., Choulet F., Wang B., Lu H.F., Breton N.L.2010. Structural development of the Lower Paleozoic belt of South China:genesis of an intracontinental orogen. J. Asian Earth Sci.,39:309-330.
Chen, J., Foland, K. A., Xing, F., Xu, X., Zhou, T.1991. Magmatism along the south-eastern margin of the Yangtze block:Precambrian collision of the Yangtze and Cathysia blocks of China. Geology,19:815-818.
Chen, X., Rowley, D., Rong, J., Zhang, J., Zhang, Y. & Zhan, R.1997. Late Precambrian through Early Palaeozoic stratigraphic and tectonic evolution of the Nanling Region, Hunan Province, South China. International Geology Review,39:469-478.
Chen, X., Rong, J. Y., Li, Y. & Boucot, A. J.2004. Facies patterns and geography of the Yangtze region, South China, through the Ordovicican and Silurian transition. Palaeogeography, Palaeoclimatology, Palaeoecology,204:353-372.
Chen, X., Zhou, Z. Y. & Fan, J. X.2010. Ordovician palaeogeography and tectonics of the major palaeoplates of China. In S. C. Finney & W. B. N. Berry (eds) The Ordovician Earth System. Geological Society of America, Special Papers, no.466:85-104.
Cocks, L. R. M. & Torsvic, T.H.2002. Earth geography from 500 to 400 million years ago:a faunal and palaeomagnetic review. Journal of the Geological Society, London 159: 631-644.
Cocks, L. R. M. & Torsvik, T. H.2011. The Palaeozoic geography of Laurentia and western Laurussia:A stable craton with mobile margins. Earth-Science Reviews,106:1-51.
Dewey, J. F. & Strachan, R. A.2003. Changing Silurian-Devonian relative plate motion in the Caledonides:sinistral transpression to sinistral transtension. Journal of the Geological Society, London,160:219-229.
Condie, K. C.2001. Continental growth during formation of Rodinia at 1.35-0.9Ga. Gondwana Research,4:5-16.
Curtis, J. B.2002. Fractured shale-gas systems. AAPG Bulletin,86(11):1921-1938.
Dalziel, I. W. D.1991. Pacific margins of Laurentia and East Antarctica—Australia as a conjugate rift pair:evidence and implications for an Eocambrian supercontinent. Geology,19:598-601.
Dalziel, I. W. D.1997. Neoproterozoic-Paleozoic geography and tectonics:review, hypothesis, environmental speculation. Geol. Soc. Am. Bull.109:16-42.
DeCelles, P. G., Giles, K. A.1996. Foreland basin systems. Basin Research,8:105-123.
Dewey, J. F. & Strachan, R. A.2005. Caledonides of Britain and Ireland. In Encyclopedia of Geology,56-63.
Dickinson, W. R.1974. Plate tectonics and sedimentation.Society of Economic Paleontologists and Mineralogists Special Publication,22:1-27.
EIA.2011a. Review of Emerging Resources:U.S. Shale Gas and Shale Oil Plays.1-105.
EIA.2011b. World shale gas resources:an intial assessment of 14 regions outside the united states.1-365.
Ettensohn, F. R.2004. Modeling the nature and development of major Paleozoic Clastic wedges in the Appalachian Basin, USA. Journal of Geodynamics,37:657-681.
Faure, M., Shu, L. S., Wang, B., Charvet, J., Choulet, F. & Monie, P.2009. Intracontinental subduction:a possiblemechanism for the Early Palaeozoic Orogen of SE China. Terra Nova,21:360-368.
Faure, M., Sun, Y., Shu, L., Monie, P. & Charvet, J.1996. Extensional tectonics within a subduction-type orogen:The case study of the Wugongshan dome (Jiangxi Province, southeastern China). Tectonophysics,263:77-106.
Fortey, R. A. & Cocks, L. R. M.2003. Palaeontological evidence bearing on global Ordovician-Silurian continental reconstructions. Earth-Sciences Reviews,61:245-307.
Gee, D. G., Fossen, H., Henriksen, N. & Higgins, A. K.2008. From the Early Paleozoic Platforms of Baltica and Laurentia to the Caledonide Orogen of Scandinavian and Greenland. Episodes,31:44-51.
Gilder, S., Leloup, P. H., Courtillot, V, Chen, Y, Coe, S. R., Zhao, X., Xiao, W., Halim, N., Cogne, J. P. & Zhu, R.1999. Tectonic evolution of the Tancheng-Lujiang (Tan-Lu) fault via Middle Triassic to early Cenozoic paleomagnetic data:Journal of Geophysical Research,104:365-390.
Greentree, M. R., Li, Z. X., Li, X. H. & Wu, H. C.2006. Late Mesoproterozoic to earliest Neoproterozoic basin record of the Sibao orogenesis in western South China and relationship to the assembly of Rodinia. Precambrian Research,151:79-100.
Hibbard, J. P., van Staal, C. R. & Rankin, D. W.2007. A Comparative Analysis of Pre-Silurian Crustal Building Blocks of the Northern and the Southern Appalachian Orogen. American Journal of Science,307:23-45.
Hibbard, J. P., van Staal, C. R. & Rankin, D. W.2010. Comparative analysis of the geological evolution of the northern and southern Appalachian orogen:Late Ordovician-Permian. In R. P. Tello, M. J. Bartholomew, J. P. Hibbard & P. M. Karabinos (eds.) From Rodinia to Pangea:The lithotectonic Record of the Appalachian Region. Geological Society of America, Memoir, no.206:51-69
Hoffman, P. F.1991. Did the breakout of Laurentia turn Gondwanaland inside-out? Science, 252:1409-1412.
Holland, C. H., Sanders, I. S. & Sanders, I.2009. The Geology of Ireland.1-568.
Huang, K., Opdyke, N. & Zhu, R. X.2000. Further paleomagnetic results from the Silurian of the Yangtze Block and their implications. Earth and Planetary Science Letter,175: 191-202.
Ingersoil, R.V.2011. Tectonics of sedimentary basins, with revised nomenclature. InCathy, B. & Antonio, A. P. (eds.) Tectonics of Sedimentary Basins:Recent Advances,3-43.
Jia, D., Wu, L., Li, H. and Deng, F.2009. Provenance of detrital zircons from the late Neoproterozoic to Ordovician sandstones of south China, Geochimica et Cosmochimica Acta,73(13S):A592.
Jia, D., Li, H., Wu, L. and Deng, F.2008. Timing of syn-tectonic granites in the early Paleozoic Wuyishan fold belt (south China) with tectonic implications,33rd International Geological Congress, Abstracts= Congres Geologique International, Resumes,33
Jiang, G., Kennedy, M. J. & Christie-Blick, N.2003. Stable isotopic evidence for methane seeps in Neoproterozoic postglacial cap carbonates. Nature,426:822-826.
Jarvie, D. M., Hill, R. J., Ruble, T. E. & Pollastro, R. M.2007. Unconventional shale-gassystems:The Mississippian Barnett Shale of noth-central Texas as one model for thermogenic shale-gas assessment. AAPG Bulletin,91(4):475-499.
Jiang, G., Sohl, L. E. & Christie-Blick, N.2003. Neoproterozoic stratigraphic comparison of the Lesser Himalaya (India) and Yangtze block (south China):Paleogeographic implications. Geology,31:917-920.
Johnson, D. D. & Beaumont, C.1995. Preliminary results from a planform kinematic model of orogen evolution, surface processes and the development of clastic foreland basin stratigraphy, in Dorobek, S.L.,and Ross, G.M. (eds.) Stratigraphic evolution of foreland basins. SEPM (Society for Sedimentary Geology) Special Publication,52:3-24.
Johnston, S. M., Hartz, E. H., Brueckner, H. K, & Gehrels, G. E.2010. U-Pb zircon geochronology and tectonostratigraphy of southern Liverpool Land, East Greenland: Implications for deformation in the overriding plates of continental collisions. EPSL,297: 512-524.
Keller, G. R. & Hatcher, R. D. J.1999. Some comparisons of the structure and evolution of the southern Appalachian-Ouachita orogen and portions of the Trans-European Suture Zone region. Tectonophysics,314:43-68.
Kneller, B. C.1991. A foreland basin on the southern margin of Iapetus. Geology,148:207-210.
Li, H. B., Jia, D., Wu, L., Zhang, Y., Yin, H. W., Wei, G. Q., Li, B. L.2013. Detrital zircon provenance of the Lower Yangtze foreland basin deposits:constraints on the evolution of the early Palaeozoic Wuyi-Yunkai orogenic belt in South China.Geological magazine, doi:10.1017/S0016756812000969..
Li, W. X., Li, X. H. & Li, Z. X.2005. Neoproterozoic bimodal magmatism in the Cathaysia Block of South China and its tectonic significance. Precambrian Research,136:51-66.
Li, W. X., Li, X. H., Li, Z. X. & Lou, F. S.2008a. Obduction-type granites within the NE Jiangxi ophiolite:Implications for the final amalgamation between the Yangtze and Cathaysia blocks. Gondwana Research,13:288-301.
Li, X. H., Li, W. X., Li, Z. X. & Liu, Y.2008b.850-790 Ma bimodal volcanic and intrusive rocks in northern Zhejiang, South China:A major episode of continental rift magmatism during the breakup of Rodinia. Lithos,102:341-57.
Li, X. H., Li, W.X., Li, Z. X., Lo, C.H., Wang, J., Ye, M. F. Yang, Y. H.2009. Amalgamation between the Yangtze and Cathaysia Blocks in South China:Constraints from SHRIMP U-Pb zircon ages, geochemistry and Nd-Hf isotopes of the Shuangxiwu volcanic rocks. Precambrian Research,174:117-128.
Li, Z. X., Bogdanova, S.V., Collins, A.S., Davidson, A., De, W.B., Ernst, R.E., Fitzsimons, I.C., Fuck, R.A., Gladkochub, D.P., Jacobs, J., Karlstrom, K.E., Lu, S., Natapov, L.M., Pease, V, Pisarevsky, S.A., Thrane, K. & Vernikovsky, V.2008c. Assembly, Configuration, and Break-Up History of Rodinia:A Synthesis. Precambrian Research, 160(1-2):179-210.
Li, Z. X.1994. Collision between the North and South China blocks:A crustal-detachment model for suturing in the region east of the Tanlu fault. Geology,22:739-742.
Li, Z. X., Li, X. H., Zhou, H. W. & Kinny, P. D.2002. Grenvillian continental collision in South China:New SHRIMP U-Pb zircon results and implications for the configuration of Rodinia. Geology,30:163-166.
Li, Z. X., Li, X. H., Kinny, P. D., Wang, J., Zhang, S. & Zhou, H.2003. Geochronology of Neoproterozoic syn-rift magmatism in the Yangtze Craton, South China and correlations with other continents:evidence for a mantle superplume that broke up Rodinia. Precambrian Research,122:85-109.
Li, Z. X., Zhang, L. & Powell, C. M.1995. South China in Rodinia:Part of the Missing Link Between Australia-East Antarctica and Laurentia? Geology,23(5):407-410.
Li, Z. X.1998. Tectonic history of the major East Asian lithospheric blocks since the mid-Proterozoic-A synthesis:American Geophysical Union Geodynamics Series,27: 221-243.
Li, Z. X. & Li, X. H.2007. Formation of the 1300 km-wide intracontinental orogen and postorogenic magmatic province in Mesozoic South China A flat-slab subduction model. Geology,35:179-182.
Li, Z. X., Li, X. H., Wartho, J. A., Clark, C., Li, W. X., Zhang, C. L. & Bao, C.2010. Magmatic an metamorphic events during the early Palaeozoic Wuyi-Yunkai orogeny, southeastern South China:new age constraints and pressure-temperature conditions. Geological Society of America Bulletin,122:772-793.
Ludwig, K. R.1999. User's Manual for Isoplot/Ex, V2.06, a Geochronological Tookit for Microsoft Excel. In Berkely Geochronological Center Special Publication.
Macqueen, R. W. & Leekie, D. A.1992. Forelnad Basins and Fold Belt. AAPG Memoir 55. 1-456.
Mann P, Gahagan L, Gordon M B.2003.Tectonic setting of the world's giant oil and gas fields. In Halbouty M. T. (eds.) Giant Oil and Gas Fields of the Decade 1990-1999, AAPG Memoir 78:15-105.
Martini, A. M., Walter, L. M., Budai, J. M., Ku, T. C. W., Kaiser, C. J. & Schoell, M.1998. Genetic and temporal relations between formation waters and biogenic methane-Upper Devonian Antrim Shale, Michigan basin, USA. Geochimica et Cosmochimica Acta, 62(10):1699-1720.
Maruyama, S.1997. Pacific-type orogeny revisited:Miyashiro-type orogeny proposed. Isl. Arc,6:91-120.
McKerrow, W. S., MacNiociall, C. & Dewey, J. F.2000. The Caledonian Orogeny redefined. Journal of the Geological Society, London,157:1149-1154.
Metcalfe, I.1996. Gondwana dispersion, and Asian accretion and evolution of eastern Tethys. Australian Journal of Earth Sciences,43:605-623.
Moores, E. M.1991. Southwest U.S.-East Antarctic (SWEAT) connection:a hypothesis. Geology,19:425-428.
Mosher, S.1998. Tectonic evolution of the southern Laurentian Grenville orogenic belt: Geological Society of America Bulletin,110:1357-1375.
Northrup, C. J., Royden, L. H. & Burchfiel, B. C.1995. Motion of the Pacific plate relative to Eurasia and its potential relation to Cenozoic extension along the eastern margin of Eurasia. Geology,23(8):719-722.
Opdyke, N. D., Huang, K., Xu, G., Zhang, W. Y. & Kent, D. V.1987. Paleomagnetic results from the Silurian of the Yangtze paraplatform.Tectonophysics,139:123-132.
Qiu, Y. M., Gao, S., McNaughton, N. J., Groves, D. I. & Ling, W. L.2000. First evidence of >3.2 Ga continental crust in the Yangtze Craton of south China and its implications for Archean crustal evolution and Phanerozoic tectonics. Geology,28:11-14.
Rey, P., Burg, J. P. Casey M.1997. The Scandinavian Caledonides and their relationship to the Variscan belt. In Burg, J.P. & Ford, M. (eds) Orogeny Through Time. Spec. Publ. Geol. Soc. London:179-200.
Rino, S., Kon, Y., Sato, W., Maruyama, S., Santosh, M & Zhao, D.2008. The Grenvillian and Pan-African orogens:World's largest orogenies through geologic time, and their implications on the origin of superplume. Gondwana Research,14:51-72.
Roberts, D.2003. The Scandinavian Caledonides:event chronology, palaeogeographic settings and likely modern analogues. Tectonophysics,365:283-299.
Rogers, J. J. W., Santosh, M.2002. Configuration of Columbia, a Mesoproterozoic Supercontinent. Gondwana Research,5:5-22.
Rong, J. Y, Chen, X., Zheng, S. Y., Ni, Y. N., Zhan, R. B., Chen, T. E., Fu, L. P., Li, R. Y.& Fan, J. X.2003. Silurian Palaeogeography of China. In Landing, E.&Johnson, M. E. (eds.) Silurian Lands and Seas, Palaeogeography Outside of Laurentia New York State Museum Bulletin, no.493:243-98.
Schwab, F. L.1976. Modern and ancient sedimentary basins:comparative accumulation rates. Geology,4:723-727.
Shu, L. S., Faure, M., Wang, B., Zhou, X. M., Song, B.2008. Late Palaeozoic-Early Mesozoic geological features of South China:Response to the Indosinian collision events in Southeast Asia. C.R. Geoscience,340:151-165.
Sinclair, H.D.1997. Tectonostratigraphic model for underfilled peripheral foreland basins:an Alpine perspective. Geological Society of America Bulletin,109:324-346.
Stephenson, D., Bevins, R. E, Millward, D., Stone, P., Parsons, I., Highton, A. J. & Wadsworth, W. J.2000. Caledonian Igneous Rocks of Great Britain. Geological Conservation Review Series, No.17:1-648.
Tapponnier, P., Peltzer, G., Le Dain, A. Y., Armijo, R. & Cobbold, P.1982. Propagating extrusion tectonics in Asia:New insights from simple experiments with plasticine: Geology,10:611-616.
Tucker, R. D., Robinson, P., Solli, A., Gee, D. G., Thorsnes, T., Krogh, T.E., Nordgulen, Q. & Bickford, M. E.2004. Thrusting and extension in the Scandian Hinterland, Norway:New U-Pb ages and Tectonostratigraphic evidence. American Journal of Science,304: 477-532.
Veevers J J.2007. Pan-Gondwanaland Post-Collisional Extension Marked by 650-500 Ma Alkaline Rocks and Carbonatites and Related Detrital Zircons:A Review. Earth-Science Reviews,83(1-2):1-47.
Vergel, P., Hou, J. M., Wang Y. M. & Mercier, J. L.2007. The kinematics of the Tan-Lu Fault zone during the Mesozoic-Palaeocen and its relations with the North China-South China block collision (Anhui Province, China). Bulletin Society geology France,178:353-365.
Wan, Y. S., Liu, D., Xu, M., Zhuang, J., Song, B., Shi, Y. & Du, L.2007. SHRIMP U-Pb zircon geochronology and geochemistry of metavolcanic and metasedimentary rocks in NW Fujian, Cathaysian block, China:tectonic implications and the need to redefine lithostratigraphic units. Gondwana Research,12:166-183.
Wan, Y. S., Liu, D. Y., Wilde, S. A., Cao, J. J., Chen, B., Dong, C. Y., Song, B. & Du, L. L. 2010. Evolution of the Yunkai Terrane, South China:evidence from SHRIMP zircon U-Pb dating, geochemistry and Nd isotope. Journal of Asian Earth Sciences,37:140-153.
Wang, X. L., Zhou, J. C., Qiu, J. S., Zhang, W. L., Liu, X. M. & Zhang, G. L.2006. LA-ICP-MS zircon geochronology of the Neoproterozoic igneous rocks from Northern Guangxi, South China:Implications for tectonic evolution. Precambrian Research,145: 111-130.
Wang, X. L., Zhou, J. C., Griffin,W. L., Wang, R. C., Qiu, J. S., O'Reilly, S. Y., Xu, X. S., Liu, X. M. & Zhang, G. L.2007a. Detrital zircon geochronology of Precambrian basement sequences in the Jiangnan orogen:dating the assembly of the Yangtze and Cathaysia Blocks. Precambrian Research,159:117-131.
Wang, Y. J., Fan, W. M., Zhao, G. C., Ji, S. C. & Peng, T. P.2007b. Zircon U-Pb geochronology of gneissic rocks in the Yunkai massif and its implications on the Caledonian event in the South China Block. Gondwana Research,12:404-416.
Wang, Y.J., Zhang, F.F., Fan,W.M., Zhang, G.W., Chen, S.Y., Cawood, P.A., Zhang, A.M., 2010. Tectonic setting of the South China Block in the early Paleozoic:resolving intracontinental and ocean closure models from detrital zircon U-Pb geochronology. Tectonics,29. doi:10.1029/2010TC002750.
Wang, Y. J., Zhang, A. M., Fan, W. M., Zhao, G. C., Zhang, G.W., Zhang, Y. Z., Zhang, F. F. & Li, S. Z.2011. Kwangsian crustal anatexis within the eastern South China Block: Geochemical, zircon U-Pb geochronological and Hf isotopic fingerprints from the gneissoid granites of Wugong and Wuyi-Yunkai Domains. Lithos,127:239-60.
Wang, J. & Li, Z. X.2003. History of Neoproterozoic rift basins in South China:implications for Rodinia break-up. Precambrian Research,122:141-58.
Wu, L., Jia, D., Li, H.B., Deng, F. & Li, Y.Q.2010. Provenance of Detrital Zircons From the Late Neoproterozoic to Ordovician Sandstones of South China:Implications for its Continental Affinity. Geological Magazine,147(6):974-980.
Xiao, W. J., He, A. Q.2005. Early Mesozoic thrust tectonics of the northwest Zhejiang region (Southeast China). Geological Society of America Bulletin,117 (7-8):945-961.
Xu, X. B., Zhang Y. Q., Shu L. S., Jia D.2011. La-ICP-MS U-Pb and 40Ar/39Ar geochronology of the sheared metamorphic rocks in the Wuyishan:Constraints on the timing of Early Paleozoic and Early Mesozoic tectono-thermal events in SE China. Tectonophysics,501:71-86.
Xu, X. S., Suzuki, K, Liu, L. & Wang, D. Z.2010. Petrogenesis and tectonic implications of Late Mesozoic granites in the NE Yangtze Block, China:further insights from the Jiuhuashan-Qingyang complex. Geological Magazine,147(2):219-232.
Yan, D. P., Zhou, M. F., Song, H.L., Wang, X.W. & Malpas, J.2003. Origin and tectonic significance of a Mesozoic multi-layer over-thrusting system within the Yangtze Block (South China). Tectonophysics,361:239-254.
Yang, Z. Y., Sun, Z. M., Yang, T.S. & Pei, J. L.2004. A Long Connection (750-380 Ma) Between South China and Australia:Paleomagnetic Constraints. Earth and Planetary Science Letters,220(3-4):423-434.
Yao, J. L., Shu, L. S. & Santosh, M.2011. Detrital zircon U-Pb geochronology, Hf-isotopes and geochemistry-New clues for the Precambrian crustal evolution of Cathaysia Block, South China. Gondwana Research,20:553-567.
Ye, M. F., Li, X. H., Li, W. X., Liu, Y. & Li, Z. X.2007. SHRIMP zircon U-Pb geochronological and whole-rock geochemical evidence for an early Neoproterozoic Sibaoan magmatic arc along the southeastern margin of the Yangtze Block. Gondwana Research,12:144-156.
Yin, A. & Nie, S.1993. An indentation model for the north and south China collision and the development of the Tan-Lu and Honam fault systems, eastern China. Tectonics,12: 801-813.
Yu, J. H., O'Reilly, S. Y., Wang, L. J., Griffin,W. L., Zhang, M., Wang, R. C., Jiang, S. Y. & Shu, L. S.2008. Where was South China in the Rodinia supercontinent? Evidence from U-Pb geochronology and Hf isotopes of detrital zircons. Precambrian Research,164: 1-15.
Yu, J. H., Wang, L. J., Griffin, W. L., O'Reilly, S.Y., Zhang, M., Li, C.Z. & Shu, L.S.2009. A Paleoproterozoic orogeny recorded in a long-lived cratonic remnant (Wuyishan terrane), eastern Cathaysia Block, China. Precambrian Reseach,174:347-363.
Zhang S.B., Zheng, Y.F., Wu, Y.B., Zhao, Z.F., Gao, S. & Wu, F.Y.2006. Zircon Isotope Evidence for≥3.5 Ga Continental Crust in the Yangtze Craton of China. Precambrian Research,146(1-2):16-34.
Zhao, J. H., Zhou, M. F., Yan, D. P., Zheng, J. P. & Li, J.W.2011. Reappraisal of the Ages of Neoproterozoic Strata in South:No connection with the Grenville orogeny. Geology, 39(4):299-302.
Zheng, J., Griffin, W.L., O'Reilly, S.Y., Zhang, M.2006. Pearson N & Pan Y Widespread Archean Basement Beneath the Yangtze Craton. Geology,34(6):417-420.
Zheng, Y. F., Wu, R. X., Wu, Y. B., Zhang, S. B., Yuan, H. L. & Wu, F. Y.2008. Rift melting of juvenile arc-derived crust:Geochemical evidence from Neoproterozoic volcanic and granitic rocks in the Jiangnan Orogen, South China. Precambrian Research,163:351-83.
Zhou, X.M. & Li, X. W.2003. Origin of late Mesozoic igneous rocks in Southeastern China: implications for lithosphere subduction and underplating of mafic magmas. Tectonophyics,326:269-287.
Zhou, J. C., Wang, X. L. & Qiu, J. S.2009. Geochronology of Neoproterozoic mafic rocks and sandstones from northeastern Guizhou, South China:Coeval arc magmatism and sedimentation. Precambrian Research,170:27-42.
安徽省地质矿产局.1987.安徽省区域地质志.北京：地质出版社,1-721.
敖振宽.1956.试论中国地台南部加里东运动的影响及其大地构造发展史.地质学报,36(3)：273-298.
蔡东升,施央申,卢华复,董火根.1993.苏州西南部的推覆和伸展构造.大地构造与成矿学,6：163-178.
陈安定.2001.苏北箕状断陷形成的动力学机制.高校地质学报,7(4)：408-418.
陈旭,李积金,耿良玉,丘金玉,倪寓南,杨学长.1988.江苏下扬子地区的志留系.见：江苏石油勘探局地质科学研究院,中国科学院南京地质古生物研究所主编.江苏地区下扬子准地台震旦纪-三叠纪生物地层,127-168.
陈旭,戎嘉余,Rowley, D. B.,张进,张元动,詹仁斌.1995.对华南早古生代板溪洋的质疑.地质评论,41(5)：389-400.
陈旭,张元动,樊隽轩,成俊峰,李启剑.2010.赣南奥陶纪笔石地层序列与广西运动.中国科学：地球科学,40(12)：1621-1631.
陈正宏,李寄嵎,谢佩珊,曾雯,周汉文.2008.利用EMP独居石定年法探讨浙闽武夷山地区变质基底岩石与花岗岩的年龄.高校地质学报,14(1)：1-15.
陈志洪,邢光福,郭坤一,董永观,陈荣,曾勇,李龙明,贺振宇,赵玲.2009.浙江平水群角斑岩的成因：锆石U-Pb年龄和Hf同位素制约.科学通报,54(5)：610-617.
陈祖兴,徐明.1999.鹅婆复式深成岩体成岩时代初探,江西地质,13(2)：100-105.
邓必荣,石鉴东.2000.兴国杨村岩体特征及侵位机制探讨.华东地质学院学报.23(2)：141-145.
董大忠,邹才能,李建忠,王社教,李新景,王玉满,李登华,黄金亮.2011.页岩气资源潜力与勘探开发前景.地质通报,30(2-3)：325-336.
董树文,方景爽,李勇,朱洪吉,Schneider, W., Breitkreuz, H. & Mattern, F.1994下扬子中三叠世-中侏罗世沉积相与印支运动.地质论评,40(2)：111-119.
范代读,李从先,蔡进功,邓兵,罗璋.2003.浙江桐庐晚奥陶世晚期沉积层序和沉积环境分析.沉积学报,21(2)：247-254.
方晓思,何胜策.1988.浙西唐家坞组的微古植物及其时代.地质论评,34(4)：327-335.
方一亭,边立曾,俞剑华,冯洪真.1993.晚奥陶世五峰期扬子板块沉积模式.沉积学报,11(3)：7-12.
冯增昭,彭勇民,金振奎,蒋盘良,鲍志东,罗璋,鞠天吟,田海芹,汪红.2001.中国南方寒武纪和奥陶纪岩相古地理.北京：地质出版社,1-239.
冯增昭,彭勇民,金振奎,鲍志东.2004.中国寒武纪和奥陶纪岩相古地理.北京：石油工业出版社,1-233.
甘晓春,季惠民,孙大中,金文山,赵凤清.1995.浙西南早元古代花岗质岩石的年代.岩石矿物学杂志,14(1)：1-8.
甘晓春,季惠民,孙大中,庄建民.1993.闽北前寒武纪基底的地质年代学研究.福建地质,12(1)：17-32.
高振中,何幼斌,李罗照,卿崇文,肖明国,程四洪,张文成,刘伟伟.2008.中国南方上奥陶统五峰组观音桥段成因讨论：是浅水介壳相还是深水异地沉积?古地理学报,10(5)：487-494.
葛肖虹.1987.论宁镇山脉推覆构造的特征与形成.吉林大学学报(地球科学版),2(2)：143-154.
关尹文,丘元禧,顾宝荣.1959.浙西、皖南上奥陶系复理石建造的发现.地质学报,39(2)：187-212.
郭福祥.1998.中国南方中新生代大地构造属性和南华造山带褶皱过程.地质学报,72(1)：25-33.
郭令智,俞剑华,施央申.1965.华南加里东地槽褶皱区大地构造发展的基本特征.中国大地构造问题.北京：北京科学出版社,165-183.
郭令智,施央申,马瑞士.1980.华南大地构造格架和地壳演化.国际交流地质学术论文集.北京：地质出版社,109-116.
郭令智,施央申,孙岩.1988.下扬子区前陆盆地逆冲推覆构造的研究.南京大学学报(自然科学版),24(1)：1-9.
郭令智,施央申,卢华复,马瑞士,董火根.1990.武夷-云开震旦纪-早古生代沟、弧、盆褶皱系.造山带-盆地环太平洋构造论文集.北京：地质出版社,1-116.
何为红.2002.扬子海盆晚奥陶世晚期至志留纪初期海平面升降与奥陶／志留系界限的划分与对比.中国地质科学院博士学位论文,1-69.
侯明金,朱光,Mercier, J., Vergely, P.,王永敏.2007.郯庐断裂带(安徽段)及邻区的动力学分析与区域构造演化.地质科学,42(2)：362-381.
胡恭任,于瑞莲,刘丛强.2001.江西省金溪-南城混合岩和花岗岩的岩石地球化学及同位素地球化学研究.岩石矿物学杂志,20(2)：103-111.
胡受奚,叶瑛.2006.对“华夏古陆”、“华夏地块”及“扬子-华夏古陆统一体”等观点的质疑.高校地质学报,12(4)：432-439.
胡雄健,许金坤,康海男,童朝旭,陈程华,叶国贵.1991.浙西南下元古界八都群的地质特征及意义.中国区域地质,3：234-240.
胡雄健.1994.浙西南下元古界八都群的地质年代学.地球化学,23：18-24.
胡艳华,顾明光,徐岩,余盛强,王加恩,贺跃.2011.浙江诸暨地区陈蔡群加里东期变质年龄的确认及其地质意义.地质通报,30(11)：1661-1670.
黄汲清.1941.江南大陆—扬子江以南之加里东山脉.地质论评,6(Z2)：293-294.
黄汲清.1960.中国地质构造基本特征的初步总结.地质学报,40(1)：1-32.
黄钟瑾,沈修志,孙岩.1984.苏、皖、浙交界逆掩-推覆构造及构造分带性的成因研究.南京大学学报,2：335-344.
黄钟瑾,沈修志,孙岩.1987.江苏靖江一苏州地区侏罗山式褶皱及滑脱断层的研究.山东矿业学院学报,1：58-64.
黄志诚,黄钟瑾,陈智娜.1991.下扬子区五峰组火山碎屑岩与放射虫硅质岩.沉积学报,9(2)：1-13.
贾东,武龙,闫兵,李海滨,李一泉,王毛毛.2011.全球大型油气田的盆地类型与分布规律.高校地质学报,17(2)：170-184.
贾承造,何登发,雷振宇,周路,贾进斗,王桂宏.2000.前陆冲断带油气勘探.北京：石油工业出版社,1-351.
晋慧娟,李育慈.1998.浙西上奥陶统于潜组Spirodesmos遗迹化石组合的环境意义.地质科学,33(3)：282-289.
江苏省地质局.1976.无锡-苏州幅1：20万区域地质调查报告.
江苏省地质矿产局.1984.江苏省及上海市区域地质志.北京：地质出版社,1-857.
江苏省地质矿产局.1989.宁镇山脉地质志.南京：江苏科学技术出版社,1-505.
江西省地质矿产局.1984.江西省地质矿产局.北京：地质出版社,1-921.
孔祥生,李志飞,冯长根,顾明光,马剑萍.1995.浙江陈蔡地区前寒武纪地质.北京： 地质出版社,1-136.
李本亮,魏国齐,贾承造.2009.中国前陆盆地构造地质特征综述与油气勘探.地学前缘,16(4)：190-202.
李海滨,贾东,武龙,张勇.2011.下扬子地区中-新生代的挤压变形与伸展改造及其油气勘探意义.岩石学报,27(3)：770-778.
李继亮,陈昌明,高文学,陈瑞君,黄家宽,田兴有,刘杰汉.1978.我国几个地区浊积岩系的特征.地质科学,1(1)：26-44.
李献华.2000.赣东北蛇绿混杂岩带中硅质岩的地球化学特征及构造意义.中国科学D辑,30(3)：284-290.
李志才.1982.广西加里东运动的特征及其对区域地质区域成矿的重要.中国区域地质,1：8-54.
梁狄刚,郭彤楼,陈建平,边立曾,赵喆.2008.南方四套区域性海相烃源岩的分布.海相油气地质,13(2)：1-16.
梁狄刚,郭彤楼,陈建平,边立曾,赵喆.2009.南方四套区域性海相烃源岩的地球化学特征.海相油气地质,14(1)：1-13.
吕洪波,夏邦栋.1987.浙西上奥陶统复理石韵律的马尔可夫链模拟.石油与天然气地质,8(2)：219-230.
刘宝珺,许效松,杏南.1993.古大陆沉积地壳演化与成矿,北京：科学出版社1-236.
刘宝珺,许效松.1994.中国南方岩相古地理图集(震旦纪—三叠纪).北京：科学出版社,1-188.
刘锐,周汉文,张利,钟增球,曾雯,向华,靳松,吕新前,李春忠.2009.华夏地块古元古代陆壳再造：锆石微量元素与U-Pb和Lu-Hf同位素证据.科学通报,54(7)：906-917.
刘晓,张元动,周传明.2012.浙西北上奥陶统文昌组和堰口组沉积特征及其意义.古地理学报,14(1)：101-116.
刘小平,潘继平,董清源,刘东鹰,段宏亮,李华东,董谦.2011.苏北地区古生界页岩气形成地质条件.天然气地质科学,22(6)：1100-1108.
卢华复.2006.关于华夏古陆.高校地质学报,12(4)：413-417.
马力,陈焕疆,甘克文,徐克定,许效松,吴根耀.2004.中国南方大地构造和海相油 气地质(上册).北京：地质出版社,1-451.
马瑞士.2006.华南构造演化新思考兼论“华夏古陆”说中的几个问题.高校地质学报,12(4)：448-456.
马永生,陈洪德,王国力.2009.中国南方层序地层与古地理.北京：科学出版社,1-603.
穆恩之.1954.论五峰页岩.古生物学报,2(2)：153-170.
南京大学地质系.1981.华南不同时代花岗岩类及其成矿关系.北京：科学出版社,1-395.
彭亚鸣,苏丽美.1983.中国东南部加里东期花岗岩的特征和成因.南京大学学报,1：140-152.
邱旭明,刘玉瑞,傅强.2006.苏北盆地上白垩统-第三系层序地层与沉积演化.北京：地质出版社,1-154.
任纪舜.1960.试论中国东南部的大地构造性质.地质论评.20(3)：132-133.
任纪舜.1964.中国东南部泥盆纪前几个大地构造问题的初步探讨.地质学报,44(4)：418-432.
任纪舜.1990.论中国南部的大地构造.地质学报,4：275-288.
戎嘉余,陈旭.1987.华南晚奥陶世的动物群分异及生物相、岩相分布模式.古生物学报,26(5)：507-535.
戎嘉余,詹仁斌,许红根,黄冰,俞国华.2010.华夏古陆于奥陶-志留纪之交的扩展证据和机制探索.中国科学,40(1)：1-17.
沈修志,孙岩,黄钟瑾,杜定全,熊斌辉.1986.江苏宜兴地区推覆构造的发现及其油气勘探的意义.南京大学学报,22(3)：510-518..
舒良树,卢华复,贾东,夏菲,福赫.1999.华南武夷山早古生代构造事件的40Ar/39Ar同位素年龄研究.南京大学学报(自然科学版),35(6)：668-674.
舒良树.2006.华南前泥盆纪构造演化：从华夏地块到加里东期造山带.高校地质学报,12(4)：418-431.
舒良树,于津海,贾东,王博,沈渭洲,张岳桥.2008.华南东段早古生代造山带研究.地质通报,27(10)：1581-1593.
舒良树.2012.华南构造演化的基本特征.地质通报,31(7)：1035-2053.
孙涛.2006.新编华南花岗岩分布图及其说明.地质通报,25(3)：332-337.
苏浙皖闽油气区石油地质志编写组.1992.中国石油地质志卷8苏浙皖闽油气区.北京：石油工业出版社,1-615.
唐显春,曾辉,张培先,汪凯明,何贵松.2011.宣城地区荷塘组页岩含气性浅析.油气藏评价与开发,1(1-2)：78-84.
涂荫玖,刘湘培,汪祥云,吴明安.2001.下扬子北缘滁州—巢湖前陆褶皱冲断带研究.大地构造与成矿学,25(1)：9-26.
王德滋,林承毅,周新民.1978.江西慈竹英云闪长岩体及其周围区域变质岩石的成因.南京大学学报,1：81-99.
王鸿祯.1985.中国古地理图集.北京：地图出版社,1-143.
王剑.2000.华南新元古代裂谷盆地沉积演化-兼论与Rodinia解体的关系.北京：地质出版社,1-146.
王金权.2006.皖南休宁新元古界-下寒武统沉积岩的有机碳同位素记录.古生物学报,45(4)：568-579.
王金渝,周荔青,郭念发,杨方子.2000.苏浙皖石油天然气地质.北京：石油工业出版社,1-234.
王俊卿.1997.苏皖志留纪鱼群及相关问题讨论.古脊椎动物学报,35(4)：307-311.
王涛,王晓霞,郑亚东,洪大卫,王新社.2007.花岗岩构造研究及花岗岩构造动力学刍议.地质科学,42(1)：91-113.
王茵,曾勇,陈松.2007.安徽巢北地区下志留统坟头组沉积环境分析.安徽地质,17(3)：166-170.
王玉净,张元动.2011.江苏仑山地区上奥陶统五峰组放射虫动物群及其地质意义.微体古生物学报,28(3)：251-260.
汪新伟,沃玉进,张荣强.2008.扬子克拉通南华纪-早古生代的构造-沉积旋回.现代地质,22(4)：525-533.
武龙.2011.华南陆块早古生代构造—沉积演化及大陆亲缘性分析.南京大学硕士论文.
夏邦栋.1986.一个加里东期的裂陷槽—对浙西早古生代沉积盆地成因类型的新认识.石油实验地质,8(1)：8-21.
夏邦栋,吕洪波.1988a.浙西皖南晚奥陶世复理石的沉积环境,兼谈鲍马层序应用问题.沉积学报,6(4)：44-51.
夏邦栋,吕洪波.1988b.苏、浙、皖地区沉积-大地构造演化.地质学报,4：301-310.
夏邦栋,吕洪波.1990.一个已埋藏的古造山带探讨.沉积学报,8(2)：1-8.
夏树芳.1978.苏南、浙北、皖南地区志留系与泥盆系的分界问题.地层学杂志,2(2)： 152-159.
向磊,舒良树.2010.华南东段前泥盆纪构造演化：来自碎屑锆石的证据.中国科学地球科学,40(10)：1377-1388.
肖传桃,姜衍文,朱忠德,李艺斌,潘云唐.1996.湖北宜昌地区奥陶纪层序地层及扬子地区五峰组沉积环境的讨论.高校地质学报,12(3)：339-347.
熊振.2010.南京地区地震构造环境研究.中国地震局地球物理研究所博士论文,1-130.
徐克勤,刘英俊,俞受鉴,王鹤年,魏秀喆.1960.江西南部加里东期花岗岩的发现.地质论评,3：112-114.
徐论勋,肖传桃,龚文平,何幼斌.2004.论扬子地区上奥陶统五峰组观音桥段的深海成因.地质学报,78(6)：726-732.
徐先兵,张岳桥,舒良树,贾东,王瑞瑞,许怀智.2010.武夷山地区前寒武纪地层沉积时代研究.地层学杂志,34(92)：254-267.
徐学思.1997.江苏省岩石地层.北京：中国地质大学出版社,1-288.
薛怀民,马芳,宋永勤,谢亚平.2010.江南造山带东段新元古代花岗岩组合的年代学和地球化学：对扬子与华夏地块拼合时间与过程的约束.岩石学报,26(11)：3215-3244.
薛耀松,俞从流.1979.浙西、赣东北寒武系下统荷塘组岩石特征及沉积环境分析.地层学杂志,3(4)：283-295.
姚保华,章振铨,王家林,火恩杰,张先康,刘保金,吴健生,王夫运,于鹏,王雅萍.2007.上海地区地壳精细结构的综合地球物理探测研究.地球物理学报,50(2)：482-491.
姚柏平,陆红,郭念发.1999.论下扬子地区多期构造格局叠加及其油气地质意义.石油勘探与开发,26(4)：10-13.
闫峻,刘海泉,宋传中,徐夕生,安亚军,刘佳,戴立群.2009.长江中下游繁昌-宁芜火山盆地火山岩锆石U-Pb年代学及其地质意义.科学通报,54(12)：1716-1724.
杨树锋,陈汉林,武光海.1995.闽北早古生代岛弧火山岩的发现及其大地构造意义.地质科学,30(2)：105-116
杨树锋,顾光明,卢成忠.2009.浙江章村地区中元古代岛弧火山岩的地球化学及构造意义.吉林大学学报,39(4)：689-698.
页岩气地质与勘探开发实践从书编委会.2009.北美地区页岩气勘探开发新进展.北京：石油工业出版社,1-271.
尹赞勋.1949.中国南部志留纪地层之分类与对比.中国地质学会会志第29卷,1-61.
俞凯,郭念发.2001.下扬子区下古生界油气地质条件评价.石油实验地质,23(1)：41-47.
岳文浙,业治铮.1996.扬子陆块东南缘早古生代的巨型斜坡带.江苏地质,20(1)：9-17.
曾萍.2007.G78区域大剖面综合解释与苏北盆地构造特征.石油天然气学报,29(3)：82-86.
赵风清.1999.华夏地块前加里东期变质基底的年代构造格架.前寒武纪研究进展,22(2)：39-46.
赵国春,孙德有,贺同兴.1994.陈蔡群构造变形特征及变形时代讨论.浙江地质,10(1)：38-46.
张爱梅,王岳军,范蔚茗,张菲菲,张玉芝.2010.闽西南清流地区加里东期花岗岩锆石U-Pb年代学及Hf同位素组成研究.大地构造与成矿学,34(3)：408-418.
张芳荣.2011.江西中-南部加里东期花岗岩地质地球化学特征及其成因.南京大学博士论文,1-115.
张菲菲,王岳军,范蔚茗,张爱梅,张玉芝.2010.湘东-赣西地区早古生代晚期花岗岩体的LA-ICPMS锆石U-Pb定年研究.地球化学,39(5)：414-426.
张淮,郭念发.2004.苏北盆地黄桥CO2气田储集层裂隙特征.江苏地质,28(4)：201-206.
张开均,施央申.1993.安徽下扬子区北缘薄皮构造研究.南京大学学报(自然科学版),29(3)：468-477.
张妮.2009.江苏侏罗系-白垩系火山岩地层对比及划分探讨.地层学杂志,33(1)：91-97.
张旗,金惟俊,李承东,王元龙.2009.中国东部燕山期大规模岩浆活动与岩石圈减薄：与大火成岩省的关系.地学前缘,16(2)：21-51.
张文佑,张步春,李荫槐.1974.中国大地构造基本特征及其发展的初步探讨.地质科学,1(1)：1-15.
张苑,舒良树,陈祥云.2011.华南早古生代花岗岩的地球化学、年代学及其成因研究—以赣中南为例.中国科学,41(98)：1061-1079.
张永军,黄钟瑾.1998.张八岭推覆体特征及其成因机制.高校地质学报,4(4)：444-451.
张岳桥,徐先兵,贾东,舒良舒,王瑞瑞.2009.华南早中生代从印支期碰撞构造体系向燕山期俯冲构造体系转换的形变记录.地学前缘,16(1)：234-247.
浙江省地质局.1966.区域地质矿产调查报告金华幅,1-117.
浙江省地质矿产局.1989.浙江省区域地质志,北京：地质出版社,1-688.
浙江省地质矿产局.2008.浙江省岩石地层.武汉：中国地质大学出版社,1-236.
钟华邦.1991.对茅山群时代的新认识.中国区域地质,4：366-372.
周金城,王孝磊,邱检生.2008.江南造山带是否格林威尔期造山带?—关于华南前寒武纪地质的几个问题.高校地质学报,14(1)：64-72.
周新民.2003.对华南花岗岩研究的若干思考.高校地质学报,9(4)：556-565.
朱光,朱光,徐嘉炜,刘国生,李双应,虞培玉.1998.下扬子地区沿江前陆盆地形成的构造控制.地质论评,44(2)：120-119.
朱光,刘国生.2000.皖南江南陆内造山带的基本特征.大地构造与成矿学,84(2)：103-111.
朱光,王勇生,王道轩,牛漫兰,刘国生,谢成龙.2006.前陆沉积与变形对郯庐断裂带同造山运动的制约.地质科学,41(1)：102-121.
朱兆玲,林焕令,章森桂.1988.江苏地区下扬子准地台寒武纪生物地层.江苏地区下扬子准地台震旦纪-三叠纪生物,35-80.
邹才能.2011.非常规油气地质.北京：地质出版社,1-310.