四川盆地北缘震旦纪—早寒武世隆-坳格局及其油气勘探意义
|
摘要
四川盆地北部震旦系—下寒武统是继安岳气田发现和绵阳—长宁裂陷提出之后备受关注的另一重点勘探领域,但对其沉积-构造格局的认识存在严重分歧。文中基于露头剖面、地震、钻井和地球化学分析资料并结合前人研究成果,提出四川盆地北缘震旦纪—早寒武世期间存在隆-坳并存的格局。四川盆地北缘震旦系—下寒武统厚度、岩相、地震反射和地球化学等指标的详细分析表明:(1)沉积-构造格局表现为隆-坳相间的特点,即自西向东依次为绵阳—长宁裂陷→汉南—米仓山隆起→万源—通江裂-坳陷→达州—开江隆起→城口—开县裂-坳陷→东安—巫溪隆起→巴东—恩施裂陷→神农架—黄陵隆起;(2)发育台地、斜坡和盆地三种沉积环境,其中斜坡环境以发育大量风暴、重力流、滑塌角砾沉积及同沉积滑移变形等为主要识别标志;(3)经历了三个"隆-坳"旋回,即陡二段末期—灯二段早期、灯二段晚期—灯四段早期、灯四段晚期—筇竹寺组晚期。四川盆地北缘震旦纪—早寒武世隆-坳格局的形成受控于震旦纪基底构造薄弱带、南秦岭地幔上隆底侵和原特提斯洋壳板片拖拽三者的联合作用,与罗迪尼亚大陆裂解和冈瓦纳大陆聚合的全球构造背景密切相关。四川盆地北缘震旦纪—早寒武世隆-坳并存格局的提出不仅有助于进一步认识该时期扬子克拉通区域沉积-构造格局和演化,也为川东北地区下一步油气勘探决策提供了参考依据。川东北地区震旦纪—早寒武世隆-坳格局控制了烃源岩和储集层的发育及源储配置关系,建议首先将裂-坳陷边缘带作为下一步勘探的重点。
The Sinian-Lower Cambrian suite in northern Sichuan Basin is considered one of the key exploration fields following the discovery of the Anyue giant gas field and Mianyang-Changning introcratonic rift.However,different views have emerged regarding its depositional-tectonic pattern.Based on previous studies and recent outcrop,seismic,drilling and geochemical data,we propose in this paper that introcratonic riftsags could coexist with uplifts during the Sinian-Early Cambrian on the northern margin of the Sichuan Basin.Detailed analyses on the thickness,lithofacies,seismic reflection and geochemical indices of the Sinian-Lower Cambrian on the northern margin of the Sichuan Basin indicate(1)the depositional-tectonic pattern is characterized by alternating rift-sags and uplifts which include,from west to east,the MianyangChangning rift, Hannan-Micangshan uplift, Wanyuan-Tongjiang rift-sag, Dazhou-Kaijiang uplift,Chengkou-Kaixian rift-sag,Dong'an-Wuxi uplift,Badong-Enshi rift,and Shennongjia-Huangling uplift;(2)three kinds of sedimentary environments—platform,slope and basin developed at the basin margin,where slope is dominated by a large number of tempestites,gravity flow deposits,slump breccias,syndepositional slip deformation,and so on;(3)the basin experienced three"uplift-depression"cycles,i.e.from the end of the second member of the Doushantuo Formation to the early stage of the second member of the Dengying Formation,from the late stage of the second member of the Dengying Formation to the early stage of the fourth member of the Dengying Formation,and from the late stage of the fourth member of the Dengying Formation to the late stage of the Qiongzhusi Formation.The formation of the uplift-depression framework is controlled in combination by the pre-Sinian basement weak zones,the mantle upwelling in southern Qinling and the slab pull of proto-Tethyan oceanic lithosphere,and all were closely related to the global tectonic setting during the breakup of Rodinia and assembly of Gondwanaland.Our proposed upliftdepression framework not only helps to fully understand the depositional-tectonic pattern and its evolution of the Yangtze Craton during this period,but also provides a reference for future oil-gas exploration in this region.The Sinian-Early Cambrian uplift-depression pattern in northeastern Sichuan Basin controls thedevelopment of source rocks,reservoirs and source-reservoir configuration.It is therefore suggested that the rift-sag marginal zones should be the preferred targets in future exploration.
The Sinian-Lower Cambrian suite in northern Sichuan Basin is considered one of the key exploration fields following the discovery of the Anyue giant gas field and Mianyang-Changning introcratonic rift.However,different views have emerged regarding its depositional-tectonic pattern.Based on previous studies and recent outcrop,seismic,drilling and geochemical data,we propose in this paper that introcratonic riftsags could coexist with uplifts during the Sinian-Early Cambrian on the northern margin of the Sichuan Basin.Detailed analyses on the thickness,lithofacies,seismic reflection and geochemical indices of the Sinian-Lower Cambrian on the northern margin of the Sichuan Basin indicate(1)the depositional-tectonic pattern is characterized by alternating rift-sags and uplifts which include,from west to east,the MianyangChangning rift, Hannan-Micangshan uplift, Wanyuan-Tongjiang rift-sag, Dazhou-Kaijiang uplift,Chengkou-Kaixian rift-sag,Dong'an-Wuxi uplift,Badong-Enshi rift,and Shennongjia-Huangling uplift;(2)three kinds of sedimentary environments—platform,slope and basin developed at the basin margin,where slope is dominated by a large number of tempestites,gravity flow deposits,slump breccias,syndepositional slip deformation,and so on;(3)the basin experienced three"uplift-depression"cycles,i.e.from the end of the second member of the Doushantuo Formation to the early stage of the second member of the Dengying Formation,from the late stage of the second member of the Dengying Formation to the early stage of the fourth member of the Dengying Formation,and from the late stage of the fourth member of the Dengying Formation to the late stage of the Qiongzhusi Formation.The formation of the uplift-depression framework is controlled in combination by the pre-Sinian basement weak zones,the mantle upwelling in southern Qinling and the slab pull of proto-Tethyan oceanic lithosphere,and all were closely related to the global tectonic setting during the breakup of Rodinia and assembly of Gondwanaland.Our proposed upliftdepression framework not only helps to fully understand the depositional-tectonic pattern and its evolution of the Yangtze Craton during this period,but also provides a reference for future oil-gas exploration in this region.The Sinian-Early Cambrian uplift-depression pattern in northeastern Sichuan Basin controls thedevelopment of source rocks,reservoirs and source-reservoir configuration.It is therefore suggested that the rift-sag marginal zones should be the preferred targets in future exploration.
引文
[1]邹才能,杜金虎,徐春春,等.四川叠合盆地震旦系-寒武系特大型气田形成分布、资源潜力及勘探发现[J].石油勘探与开发,2014,41(3):278-293.
[2]杜金虎,邹才能,徐春春,等.川中古隆起龙王庙组特大型气田战略发现与理论技术创新[J].石油勘探与开发,2014,41(3):268-277.
[3]刘树根,孙玮,罗志立,等.兴凯地裂运动与四川盆地下组合油气勘探[J].成都理工大学学报(自然科学版),2013,40(5):511-520.
[4]钟勇,李亚林,张晓斌,等.四川盆地下组合张性构造特征[J].成都理工大学学报(自然科学版),2013,40(5):498-510.
[5]杜金虎,汪泽成,邹才能,等.上扬子克拉通内裂陷的发现及对安岳特大型气田形成的控制作用[J].石油学报,2016,37(1):1-16.
[6]魏国齐,杨威,杜金虎,等.四川盆地震旦纪-早寒武世克拉通内裂陷地质特征[J].天然气工业,2015,35(1):24-35.
[7]周慧,李伟,张宝民,等.四川盆地震旦纪末期-寒武纪早期台盆的形成与演化[J].石油学报,2015,36(3):310-323.
[8]李忠权,赖芳,李应,等.四川盆地震旦系威远-安岳拉张侵蚀槽特征及形成演化[J].石油勘探与开发,2015,42(1):26-33.
[9]刘树根,宋金民,赵异华,等.四川盆地龙王庙组优质储层形成与分布的主控因素[J].成都理工大学学报(自然科学版),2014,41(6):657-670.
[10]刘树根,王一刚,孙玮,等.拉张槽对四川盆地海相油气分布的控制作用[J].成都理工大学学报(自然科学版),2016,43(1):1-23.
[11]徐春春,沈平,杨跃明,等.乐山-龙女寺古隆起震旦系-下寒武统龙王庙组天然气成藏条件与富集规律[J].天然气工业,2014,34(3):1-7.
[12]宋金民,刘树根,孙玮,等.兴凯地裂运动对四川盆地灯影组优质储层的控制作用[J].成都理工大学学报(自然科学版),2013,40(3):658-670.
[13]谷志东,李宗银,袁苗,等.四川盆地及其周缘晚震旦世-早寒武世早期区域抬升运动对岩溶储层发育的影响[J].天然气工业,2014,34(8):37-45.
[14]魏国齐,杨威,杜金虎,等.四川盆地高石梯-磨溪古隆起构造特征及对特大型气田形成的控制作用[J].石油勘探与开发,2015,42(3):257-265.
[15]杨跃明,文龙,罗冰,等.四川盆地乐山-龙女寺古隆起震旦系天然气成藏特征[J].石油勘探与开发,2016,43(2):179-188.
[16]周进高,姚根顺,杨光,等.四川盆地安岳大气田震旦系-寒武系储层的发育机制[J].天然气工业,2015,35(1):36-44.
[17]罗冰,周刚,罗文军,等.川中古隆起下古生界-震旦系勘探发现与天然气富集规律[J].中国石油勘探,2015,20(2):18-29.
[18]刘树根,邓宾,李智武,等.盆山结构与油气分布:以四川盆地为例[J].岩石学报,2011,27(3):621-635.
[19]谷志东,殷积峰,姜华,等.四川盆地西北部晚震旦世-早古生代构造演化与天然气勘探[J].石油勘探与开发,2016,43(1):1-11.
[20]杨跃明,文龙,罗冰,等.四川盆地达州-开江古隆起沉积构造演化及油气成藏条件分析[J].天然气工业,2016,36(8):1-10.
[21]谷志东,殷积峰,姜华,等.四川盆地宣汉-开江古隆起的发现及意义[J].石油勘探与开发,2016,43(6):893-904.
[22]刘树根,孙玮,李智武,等.四川叠合盆地海相碳酸盐岩油气分布特征及其构造主控因素[J].岩性油气藏,2016,28(5):1-17.
[23]赵文智,魏国齐,杨威,等.四川盆地万源-达州克拉通内裂陷的发现及勘探意义[J].石油勘探与开发,2017,44(5):659-669.
[24]刘树根,刘殊,孙玮,等.绵阳-长宁拉张槽北段构造-沉积特征[J].成都理工大学学报(自然科学版),2018,45(1):1-13.
[25]曾允孚,李南豪.我国主要碳酸盐岩油气储集岩的特征[J].成都地质学院学报,1982(3):1-14,135.
[26]四川省地质局.1∶20万城口幅-巫溪幅区域地质测量报告[R].北京:全国地质资料馆,1974.
[27]李耀西,宋礼生,周志强,等.大巴山西段早古生代地层志[M].北京:地质出版社,1975.
[28]汪明洲,成汉钧,陈祥荣,等.大巴山区寒武系的研究[J].西安地质学院学报,1989,11(4):1-9.
[29]汪明洲,许安东.陕南镇巴地区早寒武世地层:火烧店组的建立及其地层学意义[J].长春地质学院学报,1987,17(3):249-264.
[30]成汉钧,汪明洲,陈祥荣,等.论大巴山隆起的镇巴上升[J].地层学杂志,1992,16(3):196-199.
[31]薛耀松,曹瑞骥,唐天福,等.扬子区震旦纪地层序列和南、北方震旦系对比[J].地层学杂志,2001,25(3):207-234.
[32]薛耀松,周传明,陈哲.湖北南漳地区晚震旦世高家山期微化石的新发现:兼论南江上升运动的地质意义[J].微体古生物学报,2004,21(1):1-12.
[33]薛耀松,周传明.扬子区早寒武世早期磷质小壳化石的再沉积和地层对比问题[J].地层学杂志,2006,30(1):65-75.
[34]STEINER M,LI G X,QIAN Y,et al.Neoproterozoic to early Cambrian small shelly fossil assemblages and a revised biostratigraphic correlation of the Yangtze Platform(China)[J].Palaeogeography,Palaeoclimatology,Palaeoecology,2007,254:67-99.
[35]秦德余,吉让寿,高长林,等.秦岭-大巴拗拉槽[J].石油实验地质,1987,9(2):104-113.
[36]余宽宏,金振奎,董晓东,等.扬子地台北缘寒武纪同沉积断裂控制的斜坡沉积特征[J].古地理学报,2013,15(3):401-412.
[37]余宽宏,金振奎,苏奎,等.中、上扬子地台北缘寒武纪沉积特征及油气勘探意义[J].中国科学:地球科学,2013,43:1418-1435.
[38]郭正吾,邓康龄,韩永辉.四川盆地形成与演化[M].北京:地质出版社,1996.
[39]刘树根,李智武,孙玮,等.四川含油气叠合盆地基本特征[J].地质科学,2011,46(1):233-257.
[40]何登发,李德生,张国伟,等.四川多旋回叠合盆地的形成与演化[J].地质科学,2011,46(3):589-606.
[41]张国伟,张本仁,袁学诚.秦岭造山带与大陆动力学[M].北京:科学出版社,2000.
[42]刘树根,李智武,刘顺,等.大巴山前陆盆地-冲断带的形成演化[M].北京:地质出版社,2006.
[43]STEINER M,LI G X,QIAN Y,et al.Lower Cambrian Small Shelly Fossils of northern Sichuan and southern Shaanxi(China),and their biostratigraphic importance[J].Geobios,2004,37(2):259-275.
[44]四川省地质矿产局.四川省区域地质志[M].北京:地质出版社,1991.
[45]LI Z X,LI X H,KINNY P D,et al.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[J].Precambrian Research,2003,122:85-109.
[46]WANG J,LI Z X.History of Neoproterozoic rift basins in South China:implications for Rodinia breakup[J].Precambrian Research,2003,122(1/2/3/4):141-158.
[47]ZHU X Y,CHEN F K,NIE H,et al.Neoproterozoic tectonic evolution of South Qinling,China:evidence from zircon ages and geochemistry of the Yaolinghe volcanic rocks[J].Precambrian Research,2014,245:115-130.
[48]管树巍,吴林,任荣,等.中国主要克拉通前寒武纪裂谷分布与油气勘探前景[J].石油学报,2017,38(1):9-22.
[49]DONG S W,GAO R,YIN A,et al.What drove continued continent-continent convergence after ocean closure?Insights from high-resolution seismic-reflection profiling across the Daba Shan in central China[J].Geology,2013,41(6):671-674.
[50]杨志如,王学军,冯许魁,等.川中地区前震旦系裂谷研究及其地质意义[J].天然气工业,2014,34(3):80-85.
[51]谷志东,汪泽成.四川盆地川中地块新元古代伸展构造的发现及其在天然气勘探中的意义[J].中国科学:地球科学,2014,44:2210-2220.
[52]MERDITH A S,COLLINS A S,WILLIAMS S E,et al.Afull-plate global reconstruction of the Neoproterozoic[J].Gondwana Research,2017,50:84-134.
[53]刘静江,李伟,张宝民,等.上扬子地区震旦纪沉积古地理[J].古地理学报,2015,17(6):735-753.
[54]JIANG G Q,SHI X Y,ZHANG S H,et al.Stratigraphy and paleogeography of the Ediacaran Doushantuo Formation(ca.635-551Ma)in South China[J].Gondwana Research,2011,19:831-849.
[55]汪泽成,姜华,王铜山,等.四川盆地桐湾期古地貌特征及成藏意义[J].石油勘探与开发,2014,41(3):305-312.
[56]李伟,刘静江,邓胜徽,等.四川盆地及邻区震旦纪末-寒武纪早期构造运动性质与作用[J].石油学报,2015,36(5):546-556,563.
[57]罗志立.略论地裂运动与中国油气分布[J].中国地质科学学院院报,1984(3):93-101.
[58]陈旭,徐均涛,成汉钧,等.论汉南古陆及大巴山隆起[J].地层学杂志,1990,14(2):81-116.
[59]CHEN D Z,WANG J G,QING H R,et al.Hydrothermal venting activities in the Early Cambrian,South China:petrological,geochronological and stable isotopic constraints[J].Chemical Geology,2009,258:168-181.
[60]CHEN D Z,ZHOU X Q,FU Y,et al.New U-Pb zircon ages of the Ediacaran-Cambrian boundary strata in South China[J].Terra Nova,2015,27:62-68.
[61]ZHU M,ZHANG J,YANG A.Integrated Ediacaran(Sinian)chronostratigraphy of South China[J].Palaeogeography,Palaeoclimatology,Palaeoecology.2007,254(1/2):7-61.
[62]刘鹏举,尹崇玉,高林志,等.湖北宜昌樟村坪埃迪卡拉系陡山沱组微体化石新材料及锆石SHRIMP U-Pb年龄[J].科学通报,2009,54(6):774-780.
[63]ZHOU C M,LI X H,XIAO S H,et al.A new SIMS zircon U-Pb date from the Ediacaran Doushantuo Formation:age constraint on the Weng’an biota[J].Geological Magazine,2017,154(6):1193-1201.
[64]安志辉.黄陵周缘埃迪卡拉纪地层对比及沉积古地理演变[D].武汉:中国地质大学(武汉),2016.
[65]郭俊锋.湖北宜昌早寒武世岩家河生物群研究[D].西安:西北大学,2009.
[66]郑亚娟.陕南川北地区下寒武统下部微体化石研究[D].西安:长安大学,2012.
[67]王相人.湖北峡东地区寒武系水井沱组古杯化石研究[D].西安:西北大学,2012.
[68]BONATTI E.Metallogenesis at oceanic spreading centers[J].Annual Review of Earth&Planetary Sciences,1975,3(1):401-431.
[69]LOTTERMOSER B G.Trace element composition of exhalites associated with the Broken Hill sulfide deposit,Australia[J].Economic Geology,1991,86(4):870-877.
[70]SUGITANI K,YAMAMOTO K,WADA H,et al.Geochemistry of Archean carbonaceous cherts deposited at immature island-arc setting in the Pilbara Block,Western Australia[J].Sedimentary Geology,2002,151(1/2):45-66.
[71]CHEN D,QING H,YAN X,et al.Hydrothermal venting and basin evolution(Devonian,South China):constraints from rare earth element geochemistry of chert[J].Sedimentary Geology,2006,183(3):203-216.
[72]BONATTI E,FISHER D E,JOENSUU O,et al.Iron-manganese-barium Deposit from the Northern Afar Rift(Ethiopia)[J].Economic Geology,1972,67(6):717-730.
[73]SWEERE T,BOORN S V D,DICKSON A J,et al.Definition of new trace-metal proxies for the controls on organic matter enrichment in marine sediments based on Mn,Co,Mo and Cd concentrations[J].Chemical Geology,2016,441:235-245.
[74]丁林,钟大赉.滇西昌宁-孟连带古特提斯洋硅质岩稀土元素和铈异常特征[J].中国科学:化学生命科学地学,1995(1):93-100.
[75]KUNIMARU T,SHIMIZU H,TAKAHASHI K,et al.Differences in geochemical features between Permian and Triassic cherts from the Southern Chichibu terrane,southwest Japan:REE abundances,major element compositions and Sr isotopic ratios[J].Sedimentary Geology,1998,119(3/4):195-217.
[76]吕志成,刘丛强,刘家军,等.北大巴山下寒武统毒重石矿床赋矿硅质岩地球化学研究[J].地质学报,2004,78(3):390-406.
[77]李晓彪,罗远良,罗泰义,等.重庆城口地区早前寒武系黑色岩系研究:(2)早寒武世硅质岩的沉积环境研究[J].矿物学报,2007,27(增刊1):302-314.
[78]刘家军,吕志成,吴胜华,等.南秦岭大巴山大型钡成矿带中锶同位素组成及其成因意义[J].地学前缘,2014,21(5):23-30.
[79]刘明博.汉南地区新元古代晚期沉积相和地层年代学研究[D].西安:西北大学,2015.
[80]四川省地质局.1∶20万南江幅区域地质测量报告[R].北京:全国地质资料馆,1965.
[81]ZHU M,LU M,ZHANG J,et al.Carbon isotope chemostratigraphy and sedimentary facies evolution of the Ediacaran Doushantuo Formation in western Hubei,South China[J].Precambrian Research,2013,225(1):7-28.
[82]四川省地质局.1∶20万镇巴幅区域地质测量报告[R].北京:全国地质资料馆,1970.
[83]LI Z X,BOGDANOVA S V,COLLINS A S,et al.Assembly,configuration,and break-up history of Rodinia:a synthesis[J].Precambrian Research.2008,160(1/2):179-210.
[84]LI Z X,EVANS D A D,HALVERSON G P.Neoproterozoic glaciations in a revised global palaeogeography from the breakup of Rodinia to the assembly of Gondwanaland[J].Sedimentary Geology,2013,294:219-232.
[85]ERNST R E,WINGATE M T D,BUCHAN K L,et al.Global record of 1600-700 Ma Large Igneous Provinces(LIPs):implications for the reconstruction of the proposed Nuna(Columbia)and Rodinia supercontinents[J].Precambrian Research,2008,160(1/2):159-178.
[86]卓皆文,江新胜,王剑,等.华南扬子古大陆西缘新元古代康滇裂谷盆地的开启时间与充填样式[J].中国科学:地球科学,2013,43:1952-1963.
[87]崔晓庄,江新胜,王剑,等.扬子西缘澄江组底部玄武岩形成时代新证据及其地质意义[J].岩石矿物学杂志,2015,34(1):1-13.
[88]ZHOU M F,YAN D P,KENNEDY A K,et al.SHRIMPU-Pb zircon geochronological and geochemical evidence for Neoproterozoic arc-magmatism along the western margin of the Yangtze Block,South China[J].Earth and Planetary Science Letters,2002,196:51-67.
[89]ZHOU M,MA Y X,YAN D P,et al.The Yanbian Terrane(Southern Sichuan Province,SW China):a Neoproterozoic arc assemblage in the western margin of the Yangtze Block[J].Precambrian Research,2006,144:19-38.
[90]ZHOU M,ZHAO X,CHEN W T,et al.Proterozoic Fe-Cu metallogeny and supercontinental cycles of the southwestern Yangtze Block,southern China and northern Vietnam[J].Earth-Science Reviews,2014,139:59-82.
[91]YANG Z,SUN Z,YANG T,et al.A long connection(750-380Ma)between South China and Australia:paleomagnetic constraints[J].Earth and Planetary Science Letters,2004,220(3/4):423-434.
[92]DONG Y,SANTOSH M.Tectonic architecture and multiple orogeny of the Qinling Orogenic Belt,Central China[J].Gondwana Research,2016,29(1):1-40.
[93]CAWOOD P A,ZHAO G,YAO J,et al.Reconstructing South China in Phanerozoic and Precambrian supercontinents[J].Earth-Science Reviews,2018,186:173-194.
[94]TORSVIK T H.The Rodinia jigsaw puzzle[J].Science,2003,300:1379-1381.
[95]李献华,李正祥,周汉文,等.川西新元古代玄武质岩浆岩的锆石U-Pb年代学、元素和Nd同位素研究:岩石成因与地球动力学意义[J].地学前缘,2002,9(4):329-338.
[96]李献华,王选策,李武显,等.华南新元古代玄武质岩石成因与构造意义:从造山运动到陆内裂谷[J].地球化学,2008,37(4):382-398.
[97]王孝磊,周金城,陈昕,等.江南造山带的形成与演化[J].矿物岩石地球化学通报,2017,36(5):714-735.
[98]SHARMA K K.Malani magmatism:an extensional lithospheric tectonic origin[M]∥FOULGER G R,NATLAND JH,PRESNALL D C,et al.Plates,plumes,and paradigms.Geological Society of America Special Paper,2005,388:463-476.
[99]ZHAO J H,ZHOU M F.Geochemistry of Neoproterozoic mafic intrusions in the Panzhihua distric(Sichuan Province,SW China):implications for subduction-related metasomatism in the upper mantle[J].Precambrian Research,2007,152:27-47.
[100]MOGHADAM H S,KHADEMI M,HU Z C,et al.Cadomian(Ediacaran-Cambrian)arc magmatism in the ChahJam-Biarjmand metamorphic complex(Iran):magmatism along the northern active margin of Gondwana[J].Gondwana Research,2015,27:439-452.
[101]XU L G,LEHAMANN B,MAO J W,et al.Strontium,sulfur,carbon,and oxygen isotope geochemistry of the Early Cambrian strata-bound barite and witherite deposits of the Qinling-Daba region,northern margin of the Yangtze Craton,China[J].Economic Geology,2016,111(3):695-718.
[102]HOFMANN M H,LI X H,CHEN J,et al.Provenance and temporal constraints of the Early Cambrian Maotianshan Shale,Yunnan Province,China[J].Gondwana Research,2016,37:348-361.
[103]周恳恳,许效松.扬子陆块西部古隆起演化及其对郁南运动的反映[J].地质论评,2016,62(5):1125-1133.
[104]MYROW P M,HUGHES N C,GOODGE J W,et al.Extraordinary transport and mixing of sediment across Himalayan central Gondwana during the Cambrian-Ordovician[J].Geological Society of America Bulletin,2010,122(9/10):1660-1670.
[105]FORSYTH D,UYEDA S.On the relative importance of the driving forces of plate motion[J].Geophysical Journal of the Royal Astronomical Society,1975,43(1):163-200.
[106]CONRAD C P,LITHGOW-BERTELLONI C.Faster seafloor spreading and lithosphere production during the midCenozoic[J].Geology,2007,35(1):29-32.
[107]STECKLER M S.Uplift and extension at the Gulf of Suez:indications of induced mantle convection[J].Nature,1985,317(6033):135-139.
[108]BUCK W R.Small-scale convection induced by passive rifting:the cause for uplift of rift shoulders[J].Earth and Planetary Science Letters,1986,77(3/4):362-372.
[109]汪泽成,赵文智,胡素云,等.克拉通盆地构造分异对大油气田形成的控制作用:以四川盆地震旦系-三叠系为例[J].天然气工业,2017,37(1):9-23.
[2]杜金虎,邹才能,徐春春,等.川中古隆起龙王庙组特大型气田战略发现与理论技术创新[J].石油勘探与开发,2014,41(3):268-277.
[3]刘树根,孙玮,罗志立,等.兴凯地裂运动与四川盆地下组合油气勘探[J].成都理工大学学报(自然科学版),2013,40(5):511-520.
[4]钟勇,李亚林,张晓斌,等.四川盆地下组合张性构造特征[J].成都理工大学学报(自然科学版),2013,40(5):498-510.
[5]杜金虎,汪泽成,邹才能,等.上扬子克拉通内裂陷的发现及对安岳特大型气田形成的控制作用[J].石油学报,2016,37(1):1-16.
[6]魏国齐,杨威,杜金虎,等.四川盆地震旦纪-早寒武世克拉通内裂陷地质特征[J].天然气工业,2015,35(1):24-35.
[7]周慧,李伟,张宝民,等.四川盆地震旦纪末期-寒武纪早期台盆的形成与演化[J].石油学报,2015,36(3):310-323.
[8]李忠权,赖芳,李应,等.四川盆地震旦系威远-安岳拉张侵蚀槽特征及形成演化[J].石油勘探与开发,2015,42(1):26-33.
[9]刘树根,宋金民,赵异华,等.四川盆地龙王庙组优质储层形成与分布的主控因素[J].成都理工大学学报(自然科学版),2014,41(6):657-670.
[10]刘树根,王一刚,孙玮,等.拉张槽对四川盆地海相油气分布的控制作用[J].成都理工大学学报(自然科学版),2016,43(1):1-23.
[11]徐春春,沈平,杨跃明,等.乐山-龙女寺古隆起震旦系-下寒武统龙王庙组天然气成藏条件与富集规律[J].天然气工业,2014,34(3):1-7.
[12]宋金民,刘树根,孙玮,等.兴凯地裂运动对四川盆地灯影组优质储层的控制作用[J].成都理工大学学报(自然科学版),2013,40(3):658-670.
[13]谷志东,李宗银,袁苗,等.四川盆地及其周缘晚震旦世-早寒武世早期区域抬升运动对岩溶储层发育的影响[J].天然气工业,2014,34(8):37-45.
[14]魏国齐,杨威,杜金虎,等.四川盆地高石梯-磨溪古隆起构造特征及对特大型气田形成的控制作用[J].石油勘探与开发,2015,42(3):257-265.
[15]杨跃明,文龙,罗冰,等.四川盆地乐山-龙女寺古隆起震旦系天然气成藏特征[J].石油勘探与开发,2016,43(2):179-188.
[16]周进高,姚根顺,杨光,等.四川盆地安岳大气田震旦系-寒武系储层的发育机制[J].天然气工业,2015,35(1):36-44.
[17]罗冰,周刚,罗文军,等.川中古隆起下古生界-震旦系勘探发现与天然气富集规律[J].中国石油勘探,2015,20(2):18-29.
[18]刘树根,邓宾,李智武,等.盆山结构与油气分布:以四川盆地为例[J].岩石学报,2011,27(3):621-635.
[19]谷志东,殷积峰,姜华,等.四川盆地西北部晚震旦世-早古生代构造演化与天然气勘探[J].石油勘探与开发,2016,43(1):1-11.
[20]杨跃明,文龙,罗冰,等.四川盆地达州-开江古隆起沉积构造演化及油气成藏条件分析[J].天然气工业,2016,36(8):1-10.
[21]谷志东,殷积峰,姜华,等.四川盆地宣汉-开江古隆起的发现及意义[J].石油勘探与开发,2016,43(6):893-904.
[22]刘树根,孙玮,李智武,等.四川叠合盆地海相碳酸盐岩油气分布特征及其构造主控因素[J].岩性油气藏,2016,28(5):1-17.
[23]赵文智,魏国齐,杨威,等.四川盆地万源-达州克拉通内裂陷的发现及勘探意义[J].石油勘探与开发,2017,44(5):659-669.
[24]刘树根,刘殊,孙玮,等.绵阳-长宁拉张槽北段构造-沉积特征[J].成都理工大学学报(自然科学版),2018,45(1):1-13.
[25]曾允孚,李南豪.我国主要碳酸盐岩油气储集岩的特征[J].成都地质学院学报,1982(3):1-14,135.
[26]四川省地质局.1∶20万城口幅-巫溪幅区域地质测量报告[R].北京:全国地质资料馆,1974.
[27]李耀西,宋礼生,周志强,等.大巴山西段早古生代地层志[M].北京:地质出版社,1975.
[28]汪明洲,成汉钧,陈祥荣,等.大巴山区寒武系的研究[J].西安地质学院学报,1989,11(4):1-9.
[29]汪明洲,许安东.陕南镇巴地区早寒武世地层:火烧店组的建立及其地层学意义[J].长春地质学院学报,1987,17(3):249-264.
[30]成汉钧,汪明洲,陈祥荣,等.论大巴山隆起的镇巴上升[J].地层学杂志,1992,16(3):196-199.
[31]薛耀松,曹瑞骥,唐天福,等.扬子区震旦纪地层序列和南、北方震旦系对比[J].地层学杂志,2001,25(3):207-234.
[32]薛耀松,周传明,陈哲.湖北南漳地区晚震旦世高家山期微化石的新发现:兼论南江上升运动的地质意义[J].微体古生物学报,2004,21(1):1-12.
[33]薛耀松,周传明.扬子区早寒武世早期磷质小壳化石的再沉积和地层对比问题[J].地层学杂志,2006,30(1):65-75.
[34]STEINER M,LI G X,QIAN Y,et al.Neoproterozoic to early Cambrian small shelly fossil assemblages and a revised biostratigraphic correlation of the Yangtze Platform(China)[J].Palaeogeography,Palaeoclimatology,Palaeoecology,2007,254:67-99.
[35]秦德余,吉让寿,高长林,等.秦岭-大巴拗拉槽[J].石油实验地质,1987,9(2):104-113.
[36]余宽宏,金振奎,董晓东,等.扬子地台北缘寒武纪同沉积断裂控制的斜坡沉积特征[J].古地理学报,2013,15(3):401-412.
[37]余宽宏,金振奎,苏奎,等.中、上扬子地台北缘寒武纪沉积特征及油气勘探意义[J].中国科学:地球科学,2013,43:1418-1435.
[38]郭正吾,邓康龄,韩永辉.四川盆地形成与演化[M].北京:地质出版社,1996.
[39]刘树根,李智武,孙玮,等.四川含油气叠合盆地基本特征[J].地质科学,2011,46(1):233-257.
[40]何登发,李德生,张国伟,等.四川多旋回叠合盆地的形成与演化[J].地质科学,2011,46(3):589-606.
[41]张国伟,张本仁,袁学诚.秦岭造山带与大陆动力学[M].北京:科学出版社,2000.
[42]刘树根,李智武,刘顺,等.大巴山前陆盆地-冲断带的形成演化[M].北京:地质出版社,2006.
[43]STEINER M,LI G X,QIAN Y,et al.Lower Cambrian Small Shelly Fossils of northern Sichuan and southern Shaanxi(China),and their biostratigraphic importance[J].Geobios,2004,37(2):259-275.
[44]四川省地质矿产局.四川省区域地质志[M].北京:地质出版社,1991.
[45]LI Z X,LI X H,KINNY P D,et al.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[J].Precambrian Research,2003,122:85-109.
[46]WANG J,LI Z X.History of Neoproterozoic rift basins in South China:implications for Rodinia breakup[J].Precambrian Research,2003,122(1/2/3/4):141-158.
[47]ZHU X Y,CHEN F K,NIE H,et al.Neoproterozoic tectonic evolution of South Qinling,China:evidence from zircon ages and geochemistry of the Yaolinghe volcanic rocks[J].Precambrian Research,2014,245:115-130.
[48]管树巍,吴林,任荣,等.中国主要克拉通前寒武纪裂谷分布与油气勘探前景[J].石油学报,2017,38(1):9-22.
[49]DONG S W,GAO R,YIN A,et al.What drove continued continent-continent convergence after ocean closure?Insights from high-resolution seismic-reflection profiling across the Daba Shan in central China[J].Geology,2013,41(6):671-674.
[50]杨志如,王学军,冯许魁,等.川中地区前震旦系裂谷研究及其地质意义[J].天然气工业,2014,34(3):80-85.
[51]谷志东,汪泽成.四川盆地川中地块新元古代伸展构造的发现及其在天然气勘探中的意义[J].中国科学:地球科学,2014,44:2210-2220.
[52]MERDITH A S,COLLINS A S,WILLIAMS S E,et al.Afull-plate global reconstruction of the Neoproterozoic[J].Gondwana Research,2017,50:84-134.
[53]刘静江,李伟,张宝民,等.上扬子地区震旦纪沉积古地理[J].古地理学报,2015,17(6):735-753.
[54]JIANG G Q,SHI X Y,ZHANG S H,et al.Stratigraphy and paleogeography of the Ediacaran Doushantuo Formation(ca.635-551Ma)in South China[J].Gondwana Research,2011,19:831-849.
[55]汪泽成,姜华,王铜山,等.四川盆地桐湾期古地貌特征及成藏意义[J].石油勘探与开发,2014,41(3):305-312.
[56]李伟,刘静江,邓胜徽,等.四川盆地及邻区震旦纪末-寒武纪早期构造运动性质与作用[J].石油学报,2015,36(5):546-556,563.
[57]罗志立.略论地裂运动与中国油气分布[J].中国地质科学学院院报,1984(3):93-101.
[58]陈旭,徐均涛,成汉钧,等.论汉南古陆及大巴山隆起[J].地层学杂志,1990,14(2):81-116.
[59]CHEN D Z,WANG J G,QING H R,et al.Hydrothermal venting activities in the Early Cambrian,South China:petrological,geochronological and stable isotopic constraints[J].Chemical Geology,2009,258:168-181.
[60]CHEN D Z,ZHOU X Q,FU Y,et al.New U-Pb zircon ages of the Ediacaran-Cambrian boundary strata in South China[J].Terra Nova,2015,27:62-68.
[61]ZHU M,ZHANG J,YANG A.Integrated Ediacaran(Sinian)chronostratigraphy of South China[J].Palaeogeography,Palaeoclimatology,Palaeoecology.2007,254(1/2):7-61.
[62]刘鹏举,尹崇玉,高林志,等.湖北宜昌樟村坪埃迪卡拉系陡山沱组微体化石新材料及锆石SHRIMP U-Pb年龄[J].科学通报,2009,54(6):774-780.
[63]ZHOU C M,LI X H,XIAO S H,et al.A new SIMS zircon U-Pb date from the Ediacaran Doushantuo Formation:age constraint on the Weng’an biota[J].Geological Magazine,2017,154(6):1193-1201.
[64]安志辉.黄陵周缘埃迪卡拉纪地层对比及沉积古地理演变[D].武汉:中国地质大学(武汉),2016.
[65]郭俊锋.湖北宜昌早寒武世岩家河生物群研究[D].西安:西北大学,2009.
[66]郑亚娟.陕南川北地区下寒武统下部微体化石研究[D].西安:长安大学,2012.
[67]王相人.湖北峡东地区寒武系水井沱组古杯化石研究[D].西安:西北大学,2012.
[68]BONATTI E.Metallogenesis at oceanic spreading centers[J].Annual Review of Earth&Planetary Sciences,1975,3(1):401-431.
[69]LOTTERMOSER B G.Trace element composition of exhalites associated with the Broken Hill sulfide deposit,Australia[J].Economic Geology,1991,86(4):870-877.
[70]SUGITANI K,YAMAMOTO K,WADA H,et al.Geochemistry of Archean carbonaceous cherts deposited at immature island-arc setting in the Pilbara Block,Western Australia[J].Sedimentary Geology,2002,151(1/2):45-66.
[71]CHEN D,QING H,YAN X,et al.Hydrothermal venting and basin evolution(Devonian,South China):constraints from rare earth element geochemistry of chert[J].Sedimentary Geology,2006,183(3):203-216.
[72]BONATTI E,FISHER D E,JOENSUU O,et al.Iron-manganese-barium Deposit from the Northern Afar Rift(Ethiopia)[J].Economic Geology,1972,67(6):717-730.
[73]SWEERE T,BOORN S V D,DICKSON A J,et al.Definition of new trace-metal proxies for the controls on organic matter enrichment in marine sediments based on Mn,Co,Mo and Cd concentrations[J].Chemical Geology,2016,441:235-245.
[74]丁林,钟大赉.滇西昌宁-孟连带古特提斯洋硅质岩稀土元素和铈异常特征[J].中国科学:化学生命科学地学,1995(1):93-100.
[75]KUNIMARU T,SHIMIZU H,TAKAHASHI K,et al.Differences in geochemical features between Permian and Triassic cherts from the Southern Chichibu terrane,southwest Japan:REE abundances,major element compositions and Sr isotopic ratios[J].Sedimentary Geology,1998,119(3/4):195-217.
[76]吕志成,刘丛强,刘家军,等.北大巴山下寒武统毒重石矿床赋矿硅质岩地球化学研究[J].地质学报,2004,78(3):390-406.
[77]李晓彪,罗远良,罗泰义,等.重庆城口地区早前寒武系黑色岩系研究:(2)早寒武世硅质岩的沉积环境研究[J].矿物学报,2007,27(增刊1):302-314.
[78]刘家军,吕志成,吴胜华,等.南秦岭大巴山大型钡成矿带中锶同位素组成及其成因意义[J].地学前缘,2014,21(5):23-30.
[79]刘明博.汉南地区新元古代晚期沉积相和地层年代学研究[D].西安:西北大学,2015.
[80]四川省地质局.1∶20万南江幅区域地质测量报告[R].北京:全国地质资料馆,1965.
[81]ZHU M,LU M,ZHANG J,et al.Carbon isotope chemostratigraphy and sedimentary facies evolution of the Ediacaran Doushantuo Formation in western Hubei,South China[J].Precambrian Research,2013,225(1):7-28.
[82]四川省地质局.1∶20万镇巴幅区域地质测量报告[R].北京:全国地质资料馆,1970.
[83]LI Z X,BOGDANOVA S V,COLLINS A S,et al.Assembly,configuration,and break-up history of Rodinia:a synthesis[J].Precambrian Research.2008,160(1/2):179-210.
[84]LI Z X,EVANS D A D,HALVERSON G P.Neoproterozoic glaciations in a revised global palaeogeography from the breakup of Rodinia to the assembly of Gondwanaland[J].Sedimentary Geology,2013,294:219-232.
[85]ERNST R E,WINGATE M T D,BUCHAN K L,et al.Global record of 1600-700 Ma Large Igneous Provinces(LIPs):implications for the reconstruction of the proposed Nuna(Columbia)and Rodinia supercontinents[J].Precambrian Research,2008,160(1/2):159-178.
[86]卓皆文,江新胜,王剑,等.华南扬子古大陆西缘新元古代康滇裂谷盆地的开启时间与充填样式[J].中国科学:地球科学,2013,43:1952-1963.
[87]崔晓庄,江新胜,王剑,等.扬子西缘澄江组底部玄武岩形成时代新证据及其地质意义[J].岩石矿物学杂志,2015,34(1):1-13.
[88]ZHOU M F,YAN D P,KENNEDY A K,et al.SHRIMPU-Pb zircon geochronological and geochemical evidence for Neoproterozoic arc-magmatism along the western margin of the Yangtze Block,South China[J].Earth and Planetary Science Letters,2002,196:51-67.
[89]ZHOU M,MA Y X,YAN D P,et al.The Yanbian Terrane(Southern Sichuan Province,SW China):a Neoproterozoic arc assemblage in the western margin of the Yangtze Block[J].Precambrian Research,2006,144:19-38.
[90]ZHOU M,ZHAO X,CHEN W T,et al.Proterozoic Fe-Cu metallogeny and supercontinental cycles of the southwestern Yangtze Block,southern China and northern Vietnam[J].Earth-Science Reviews,2014,139:59-82.
[91]YANG Z,SUN Z,YANG T,et al.A long connection(750-380Ma)between South China and Australia:paleomagnetic constraints[J].Earth and Planetary Science Letters,2004,220(3/4):423-434.
[92]DONG Y,SANTOSH M.Tectonic architecture and multiple orogeny of the Qinling Orogenic Belt,Central China[J].Gondwana Research,2016,29(1):1-40.
[93]CAWOOD P A,ZHAO G,YAO J,et al.Reconstructing South China in Phanerozoic and Precambrian supercontinents[J].Earth-Science Reviews,2018,186:173-194.
[94]TORSVIK T H.The Rodinia jigsaw puzzle[J].Science,2003,300:1379-1381.
[95]李献华,李正祥,周汉文,等.川西新元古代玄武质岩浆岩的锆石U-Pb年代学、元素和Nd同位素研究:岩石成因与地球动力学意义[J].地学前缘,2002,9(4):329-338.
[96]李献华,王选策,李武显,等.华南新元古代玄武质岩石成因与构造意义:从造山运动到陆内裂谷[J].地球化学,2008,37(4):382-398.
[97]王孝磊,周金城,陈昕,等.江南造山带的形成与演化[J].矿物岩石地球化学通报,2017,36(5):714-735.
[98]SHARMA K K.Malani magmatism:an extensional lithospheric tectonic origin[M]∥FOULGER G R,NATLAND JH,PRESNALL D C,et al.Plates,plumes,and paradigms.Geological Society of America Special Paper,2005,388:463-476.
[99]ZHAO J H,ZHOU M F.Geochemistry of Neoproterozoic mafic intrusions in the Panzhihua distric(Sichuan Province,SW China):implications for subduction-related metasomatism in the upper mantle[J].Precambrian Research,2007,152:27-47.
[100]MOGHADAM H S,KHADEMI M,HU Z C,et al.Cadomian(Ediacaran-Cambrian)arc magmatism in the ChahJam-Biarjmand metamorphic complex(Iran):magmatism along the northern active margin of Gondwana[J].Gondwana Research,2015,27:439-452.
[101]XU L G,LEHAMANN B,MAO J W,et al.Strontium,sulfur,carbon,and oxygen isotope geochemistry of the Early Cambrian strata-bound barite and witherite deposits of the Qinling-Daba region,northern margin of the Yangtze Craton,China[J].Economic Geology,2016,111(3):695-718.
[102]HOFMANN M H,LI X H,CHEN J,et al.Provenance and temporal constraints of the Early Cambrian Maotianshan Shale,Yunnan Province,China[J].Gondwana Research,2016,37:348-361.
[103]周恳恳,许效松.扬子陆块西部古隆起演化及其对郁南运动的反映[J].地质论评,2016,62(5):1125-1133.
[104]MYROW P M,HUGHES N C,GOODGE J W,et al.Extraordinary transport and mixing of sediment across Himalayan central Gondwana during the Cambrian-Ordovician[J].Geological Society of America Bulletin,2010,122(9/10):1660-1670.
[105]FORSYTH D,UYEDA S.On the relative importance of the driving forces of plate motion[J].Geophysical Journal of the Royal Astronomical Society,1975,43(1):163-200.
[106]CONRAD C P,LITHGOW-BERTELLONI C.Faster seafloor spreading and lithosphere production during the midCenozoic[J].Geology,2007,35(1):29-32.
[107]STECKLER M S.Uplift and extension at the Gulf of Suez:indications of induced mantle convection[J].Nature,1985,317(6033):135-139.
[108]BUCK W R.Small-scale convection induced by passive rifting:the cause for uplift of rift shoulders[J].Earth and Planetary Science Letters,1986,77(3/4):362-372.
[109]汪泽成,赵文智,胡素云,等.克拉通盆地构造分异对大油气田形成的控制作用:以四川盆地震旦系-三叠系为例[J].天然气工业,2017,37(1):9-23.
© 2004-2018 中国地质图书馆版权所有 京ICP备05064691号 京公网安备11010802017129号 地址：北京市海淀区学院路29号 邮编：100083 电话：办公室：(+86 10)66554848；文献借阅、咨询服务、科技查新：66554700 |