合肥盆地中生界的地层时代判识及意义
|
摘要
合肥盆地由于构造演化过程复杂、古生物资料缺乏等,在地层时代研究上存在着诸多疑义;本文以地震层序为框架辅以生物地层学和岩石地层学等证据,参照区域构造事件,建立了新的地层层序,主要提出了:①周公山组和圆筒山组的岩石学、地球物理学和古生物学等特征相似,二者合并统称为圆筒山组,原先的周公山组和圆筒山组分别视为该地层组的上部岩性段和下部岩性段,时代为中侏罗统;②朱巷组与黑石渡组属于异地同期异相,为上侏罗统;③响导铺组为下白垩统;④定远组与戚家桥组属于异地同期异相,为古近系;这是探索以层序地层学方法为主判识地层时代的综合性研究成果,为低勘查程度地区的地层时代确定提供了一个实例,也为大别山造山带、郯—庐断裂带中生代构造演化研究提供了依据。
Many disputes still exist in the stratigraphic zonation and correlation of Hefei Basin due to its complex tectonic evolution and the lack of paleontological data. This paper established new stratigraphical sequences based on seismic sequences, in combination of the evidence from biostratigraphy and lithology and regional tectonic movements. The following are proposed: ① The Middle Jurassic Zhougongshan Formation and Yuantongshan Formation are classified to Yuantongshan Formation due to their similar lothological, geophysical and paleontological features, which could be respectively taken as the upper and lower parts of Yuantongshan Formation. ② The Zhuxiang Formation and Heishidu Formation are contemporaneous difference facies in different places, and are in the Upper Jurassic stratum. ③ The Xiangdaopu Formation is the stratum of the Lower Cretaceous. ④ The Dingyuan Formation and Qijiaqiao Formation are contemporaneous difference facies in different places, and are in the Tertiary stratum. These new recognitions provide a guideline for stratigraphical study in Hefei Basin, stratigraphical sequence determination in immature exploration areas and tectonic evolution study of Dabieshan orogen and Tan-Lu fault zone.
Many disputes still exist in the stratigraphic zonation and correlation of Hefei Basin due to its complex tectonic evolution and the lack of paleontological data. This paper established new stratigraphical sequences based on seismic sequences, in combination of the evidence from biostratigraphy and lithology and regional tectonic movements. The following are proposed: ① The Middle Jurassic Zhougongshan Formation and Yuantongshan Formation are classified to Yuantongshan Formation due to their similar lothological, geophysical and paleontological features, which could be respectively taken as the upper and lower parts of Yuantongshan Formation. ② The Zhuxiang Formation and Heishidu Formation are contemporaneous difference facies in different places, and are in the Upper Jurassic stratum. ③ The Xiangdaopu Formation is the stratum of the Lower Cretaceous. ④ The Dingyuan Formation and Qijiaqiao Formation are contemporaneous difference facies in different places, and are in the Tertiary stratum. These new recognitions provide a guideline for stratigraphical study in Hefei Basin, stratigraphical sequence determination in immature exploration areas and tectonic evolution study of Dabieshan orogen and Tan-Lu fault zone.
引文
①张交东.2000.合肥盆地物探资料采集方案与质量监督报告.内部报告.
②安徽石油勘探公司,胜利油田有限公司.2000.合肥盆地石油地质条件前期评价.中国石油化工胜利油田科研报告.
③刘德良,张交东,曹高社,谈迎,李振生.2001.合肥盆地油气评价的多元构造动力学背景研究.中国科技大学科研报告.
④胜利油田有限公司.2002.安参1井地质完井报告。中国石油化工胜利油田科研报告.
⑤张交东.2003.华北陆块东南缘燕山期构造演化与油气地质条件.中国科技大学博士学位论文.
安徽省地质矿产局.1978.安徽省区域地质调查报告(合肥幅,定远幅).北京:地质出版社,20~286.
安徽省地质矿产局.1987.安徽省区域地质志.北京:地质出版社,140~257,471~555.
安徽省地质矿产局.1997.安徽省岩石地层.武汉:中国地质大学出版社,64~80.
陈海云,舒良树,张云银.林春明,刘国宏,赵彦彦.2004.合肥盆地中新生代构造演化.高校地质学报,10(2):250~256.
陈建平.2005.合肥盆地中新生代构造演化与油气地质特征.北京:地质出版社,32~118.
曹忠祥.2007.合肥盆地白垩纪伸展构造格局.南京大学学报(自然科学),43(5):526~534.
戴圣潜,邓晋福,吴宗絮,赵海玲,陈江峰,杜建国.2003.大别造山带燕山期造山作用的岩浆岩石学证据.中国地质,30(2):159~164.
董树文,张岳桥,龙长兴,杨振宇,季强,王涛,胡建民,陈宣华.2007.中国侏罗纪构造变革与燕山运动新诠释.地质学报,81(11):1449~1461.
方小东,朱光,徐春华,刘国生.2005.合肥盆地安参1井同位素年代地层学研究.安徽地质,15(4):246~250.
高金慧,许化政,周新科.2006.合肥盆地侏罗纪构造沉积特征与含油气性.石油实验地质,28(6):529~534.
侯明金,王永敏,Jacques Mercier,Pierre Vergely,王永敏.2003.郯庐断裂带(安徽部分)动力学演化及其构造意义.地质通报,22(2):105~112.
胡博,张岳桥.2007.安徽张八岭隆起东缘基底走滑韧性剪切带的发现及其构造意义.地质通报,26(3):256~265.
韩树棻.1996.安徽北部中新生代沉积盆地分析.北京:地质出版社,5~98.
介霖,朱儒勋,陈瑞庚,吴少华,张清,罗益策,郑遥芳,姚雪根,徐克定.1992.中国石油地质志(卷八)苏浙皖闽油气区.北京:石油工业出版社,398~409.
李洪涛,宋之光,邹艳荣,王成善,季强.2008.冀北-辽西早白垩世沉积有机质特征与古气候环境演变.地质学报,82(1):72~76.
李三忠,王金铎,刘建忠,于建国,吕海青,侯方辉.2005.鲁西地块中生代构造格局及其形成背景.地质学报,79(4):487~497.
李丕龙,李学田,宋明水,宋国奇,徐春华,黄开权.2003.合肥盆地石油地质与地球物理特征研究及进展.北京:地质出版社,32~206.
李忠,孙枢,李任伟,江茂生.2000.合肥盆地中生代充填序列及其对大别山造山作用的指示.中国科学(D辑),30(3):256~264.
李云平,吴时国,韩文功,张岳桥.2006.合肥盆地和郯庐断裂带南段深部地球物理特征研究.地球物理学报,49(1):115~122.
刘德良,曹高社,李振生,杨晓勇,巩翔.2002.郯庐断裂南段主断裂韧性剪切带形成历时时限的探索.地学前缘,9(2):475~482.
刘顺,沈忠民,司建涛.2006.郯庐断裂带演化动力学———多力源多时期分段作用模式.成都理工大学学报,33(5):473~477.
鲁国明,朱光,李学田,王道轩,宋传中,刘国生.2002.郯-庐断裂带对合肥盆地油气地质条件的控制.石油实验地质,24(3):216~222.
邱连贵,辛忠斌,徐春华,徐佑德.2002.安参1井中生界沉积相及储层特征研究.石油实验地质,24(3):228~231.
施凤成,陈平,徐春华.2005.合肥盆地侏罗系高精度层序地层格架研究.地质科技情报,24(2):17~21.
宋明水,江来利,李学田,储东如,杜森官.2002.大别造山带对合肥盆地的构造控制.石油实验地质,24(3):209~215.
汤加富,李怀坤,娄清.2003.郯庐断裂南段研究进展与断裂性质讨论.地质通报,22(6):426~436.
滕吉文,闫雅芬,王光杰,熊熊.2006.大别造山带与郯庐断裂带壳、幔结构和陆内“俯冲”的耦合效应.地球物理学报,49(2):449~457.
王亚琳,张交东,邱连贵,裴磊,徐春华.2002.试论合肥中新生代盆地构造单元划分.安徽地质,12(2):97~103.
吴海权,江来利,戴圣潜.2002.安徽霍山毛坦厂地区中生代地层层序的厘定.地层学杂志,26(1):9~15.
吴根耀,梁兴,陈焕疆.2007.试论郯城-庐江断裂带的形成、演化及其性质.地质科学,42(1):160~175.
吴因业,顾家裕.2002.油气层序地层学.北京:石油工业出版社,155~162.
万天丰,朱鸿.2002.中国大陆及邻区中生代—新生代大地构造与环境变迁.现代地质,16(2):107~120.
万天丰.2004.中国大地构造学纲要.北京:地质出版社,4~25,118~250.
徐春华,朱光,刘国生,谢成龙,王勇生,李长城.2005.合肥盆地钻井地层的同位素测年与地层划分.安徽地质,15(4):251~255.
徐佑德,赵明,徐春华,徐明,邱连贵.2002.合肥盆地安参1井中生代地层特征.石油实验地质,24(3):223~227.
邢光福,卢清地,陈荣,张正义,聂童春,李龙明,黄家龙,林敏.2008.华南晚中生代构造体制转折结束时限研究———兼与华北燕山地区对比.地质学报,82(4):451~463.
杨晓勇.2006.郯庐断裂带南段沙溪含铜斑岩体的40Ar/39Ar年代学研究及意义.矿物岩石,26(2):52~56.
邹才能,池英柳,李明,薛叔洁.2004.陆相层序地层学分析技术.北京:石油工业出版社,5~150.
赵越,徐刚,张拴宏,杨振宇,张岳桥,胡健民.2004.燕山运动与东亚构造体制的转变.地学前缘,1l(3):319~328.
朱光,宋传中,王道轩,刘国生,徐嘉炜.2001.郯庐断裂带走滑时代的40Ar/39Ar年代学研究及其构造意义.中国科学D辑:地球科学,31(3):250~256.
张交东,李学田,徐春华.2002.合肥坳陷表层地质与地震采集技术的关系研究.见:刘兴材,李丕龙主编,复式油气田论文集(胜利油田地学开拓者奖).北京:石油工业出版社,385~388.
张交东,刘成斋,刘德良,赵玉华,张升平,陈红梅.2003a.晚侏罗世大别山强烈隆升的地层证据.地学前缘,10(1):168.
张交东,刘德良,林会喜,邱连贵,徐佑德,任风楼,裴磊.2003b.郯庐断裂带南段巨型正花状构造的发现与地质意义.中国科技大学学报,33(4):401~404.
张交东,刘德良,杨晓勇,谈迎,曹国滨,张旭,耿绍宇.2003c.物化探测线编码系统的设计与实践.石油地球物理勘探,38(1):84~87.
张岳桥,赵越,董树文,杨农.2004.中国东部及邻区早白垩世裂陷盆地构造演化阶段.地学前缘,l1(3):123~133.
Christopher J.Modica,Eugene R.Brush.2004.Postrift sequencestratigraphy,paleogeography,and fill history of the deep-waterSantos Basin,offshore southeast Brazil.AAPG Bulletin,88(7):923~945.
Chen F,Guo J,Jiang L,Siebel W,Cong B,Satir M.2003.Provenance of the Beihuaiyanglower-grade metamorphic zone ofthe Dabie ultrahigh-pressure collisional orogen,China:Evidence fromzircon ages.Journal of Asian Earth Sciences,22:343~352.
Chen Duofu,Chen Xianpei,Chen Guangqian.2003.Sea-level changesand hydrothermal sedi mentary mineralization of large-superlargeore deposits among Sinian to Triassic in South China.Science inChina Series D-Earth,46(S):154~163.
David W.Houseknecht,Kenneth J.Bird.2004.Sequencestratigraphy of the Kingak Shale(Jurassic Lower Cretaceous),National Petroleum Reserve in Alaska.AAPG Bulletin,88(3):279~302.
Gale A S,Huggett J M,Like H P,Laurie E,E A Hail wood,Hardenbol J.2006.Correlation of Eocene-Oligocene marine andcontinental records:orbital cyclicity,magnetostratigraphy andsequence stratigraphy of the Solent Group,Isle of Wight,UK.Journal of the Geological Society,163:401~415.
Graham D.Moss,Donna L.Cathro,James A.Austin.2004.Sequence biostratigraphy of prograding cinoforms,NorthernCarnarvon Basin,Western Australia:a proxy for variations inOligocene to Pliocene Global Sea Level.PALAIOS,19:206~226.
Gilder S A,Leloup P H,Courtillot V,Chen Y,Coe R,Zhao X,Wang W,Hali m N,Cogne J P,Zhu R.1999.Tectonicevolution of the Tancheng Lujiang(Tan-Lu)fault via MiddleTriassic to Early Cenozoic paleomagnetic data.Journal ofGeophysical Research,104:15365~15390.
Gri mmer J C,Jonckheere R,Enkel mann E,Ratschbacher L,HackerB R,Blythe A E,Wagner G A,Wu Q,Liu S,Dong S.2002.Cretaceous-Cenozoic history of the southern Tan-Lu fault zone:apatite fission-track and structural constraints from the DabieShan(eastern China).Tectonophysics,359:225~253.
Li X H.2000.Cretaceous magmatismand lithospheric extension insoutheast China.Journal of Asian Earth Sciences,18:293~305.
Lin W,Faure M,Wang Q,Moni P,Panis D.2005.Triassicpolyphase deformation in the Feidong-Zhangbaling massif(Eastern China)andits place in the collision between the northChina and South China blocks.Journal of Asian Earth Sciences,25:121~136.
Li Z,Li R,Sun S,Wang Q.2004.Jurassic depositional records andsandstone provenances in Hefei Basin,central China:I mplication for Dabie orogenesis Source.The Island Arc,13:346~358.
Li Z,Li Y,Zheng J P,Han D.2007.Late Mesozoic tectonictransition of the eastern North China Craton:evidence frombasin-fill records.Geological Society,280:239~265.
Li Zhong,Sun Shu,Li Renwei,Jiang Maosheng.2001.Mesozoic fill-sequences in Hefei Basin:I mplication for Dabie Orogenesis,central China.Science in China Ser.D Earth Sciences,44(1):52~63.
Li Renwei,Wan Yusheng,Cheng Zhenu,Zhou Jianiong,XuYunhua,Li Zhong,Jiang Maosheng.2005a.The Dabie Orogenas the early Jurassic sedi mentary provenance:Constraints fromthe detrital zircon SHRI MP U-Pb dating.Science in China Ser.D Earth Sciences,48(2):145~155.
Li Renwei,Wan Yusheng,Cheng Zhenyu,Zhou Jianxiong,LiShuangying,Jin Fuquan,Meng Qingren,Li Zhong,JiangMaosheng.2005b.Provenance of Jurassic sedi ments in theHefei Basin,east-central China and the contribution of high-pressure and ultrahigh-pressure metamorphic rocks from theDabie Shan.Earth and Planetary Science Letters,231:279~294.
Hao T Y,Xu Y,Suh M,Xu Y,Liu J H,Zhang L L,Dai M G.2007.East Marginal Fault of the Yellow Sea:a part of theConjunction zone between Sino-Korea and Yangtze Block?geological society,Special Publication,280:281~291.
Meng Q R,Li S Y,Li R W.2007.Mesozoic evolution of the Hefeibasin in eastern China:sedi mentary response to deformationsinthe adjacent Dabieshan and along the Tan-Lu fault.GeologicSociety of American Bulletin,119:897~916.
Ren J,Tamaki K,Li S,Zhang J.2002.Late Mesozoic andCretaceous rifting and its dynamic setting in eastern China andadjacent areas.Tectonophysics,344:175~205.
Wang Xunlian.2002.On steps and methods for the establishment ofglobal boundary stratotype section and point(GSSP)fromtheviewpoint of integrated stratigraphy.Science in China Ser.DEarth Sciences,45(11):1027~1041.
Xie Xin,Xu Xisheng,Zou Haibo,Jiang Shaoyong,Zhang Ming,Qiu Jiansheng.2006.Early J2basaltsin SE China:Incipience oflarge-scale late Mesozoic magmatism.Sciencein China Series D-Earth Sciences,49(8):796~815.
②安徽石油勘探公司,胜利油田有限公司.2000.合肥盆地石油地质条件前期评价.中国石油化工胜利油田科研报告.
③刘德良,张交东,曹高社,谈迎,李振生.2001.合肥盆地油气评价的多元构造动力学背景研究.中国科技大学科研报告.
④胜利油田有限公司.2002.安参1井地质完井报告。中国石油化工胜利油田科研报告.
⑤张交东.2003.华北陆块东南缘燕山期构造演化与油气地质条件.中国科技大学博士学位论文.
安徽省地质矿产局.1978.安徽省区域地质调查报告(合肥幅,定远幅).北京:地质出版社,20~286.
安徽省地质矿产局.1987.安徽省区域地质志.北京:地质出版社,140~257,471~555.
安徽省地质矿产局.1997.安徽省岩石地层.武汉:中国地质大学出版社,64~80.
陈海云,舒良树,张云银.林春明,刘国宏,赵彦彦.2004.合肥盆地中新生代构造演化.高校地质学报,10(2):250~256.
陈建平.2005.合肥盆地中新生代构造演化与油气地质特征.北京:地质出版社,32~118.
曹忠祥.2007.合肥盆地白垩纪伸展构造格局.南京大学学报(自然科学),43(5):526~534.
戴圣潜,邓晋福,吴宗絮,赵海玲,陈江峰,杜建国.2003.大别造山带燕山期造山作用的岩浆岩石学证据.中国地质,30(2):159~164.
董树文,张岳桥,龙长兴,杨振宇,季强,王涛,胡建民,陈宣华.2007.中国侏罗纪构造变革与燕山运动新诠释.地质学报,81(11):1449~1461.
方小东,朱光,徐春华,刘国生.2005.合肥盆地安参1井同位素年代地层学研究.安徽地质,15(4):246~250.
高金慧,许化政,周新科.2006.合肥盆地侏罗纪构造沉积特征与含油气性.石油实验地质,28(6):529~534.
侯明金,王永敏,Jacques Mercier,Pierre Vergely,王永敏.2003.郯庐断裂带(安徽部分)动力学演化及其构造意义.地质通报,22(2):105~112.
胡博,张岳桥.2007.安徽张八岭隆起东缘基底走滑韧性剪切带的发现及其构造意义.地质通报,26(3):256~265.
韩树棻.1996.安徽北部中新生代沉积盆地分析.北京:地质出版社,5~98.
介霖,朱儒勋,陈瑞庚,吴少华,张清,罗益策,郑遥芳,姚雪根,徐克定.1992.中国石油地质志(卷八)苏浙皖闽油气区.北京:石油工业出版社,398~409.
李洪涛,宋之光,邹艳荣,王成善,季强.2008.冀北-辽西早白垩世沉积有机质特征与古气候环境演变.地质学报,82(1):72~76.
李三忠,王金铎,刘建忠,于建国,吕海青,侯方辉.2005.鲁西地块中生代构造格局及其形成背景.地质学报,79(4):487~497.
李丕龙,李学田,宋明水,宋国奇,徐春华,黄开权.2003.合肥盆地石油地质与地球物理特征研究及进展.北京:地质出版社,32~206.
李忠,孙枢,李任伟,江茂生.2000.合肥盆地中生代充填序列及其对大别山造山作用的指示.中国科学(D辑),30(3):256~264.
李云平,吴时国,韩文功,张岳桥.2006.合肥盆地和郯庐断裂带南段深部地球物理特征研究.地球物理学报,49(1):115~122.
刘德良,曹高社,李振生,杨晓勇,巩翔.2002.郯庐断裂南段主断裂韧性剪切带形成历时时限的探索.地学前缘,9(2):475~482.
刘顺,沈忠民,司建涛.2006.郯庐断裂带演化动力学———多力源多时期分段作用模式.成都理工大学学报,33(5):473~477.
鲁国明,朱光,李学田,王道轩,宋传中,刘国生.2002.郯-庐断裂带对合肥盆地油气地质条件的控制.石油实验地质,24(3):216~222.
邱连贵,辛忠斌,徐春华,徐佑德.2002.安参1井中生界沉积相及储层特征研究.石油实验地质,24(3):228~231.
施凤成,陈平,徐春华.2005.合肥盆地侏罗系高精度层序地层格架研究.地质科技情报,24(2):17~21.
宋明水,江来利,李学田,储东如,杜森官.2002.大别造山带对合肥盆地的构造控制.石油实验地质,24(3):209~215.
汤加富,李怀坤,娄清.2003.郯庐断裂南段研究进展与断裂性质讨论.地质通报,22(6):426~436.
滕吉文,闫雅芬,王光杰,熊熊.2006.大别造山带与郯庐断裂带壳、幔结构和陆内“俯冲”的耦合效应.地球物理学报,49(2):449~457.
王亚琳,张交东,邱连贵,裴磊,徐春华.2002.试论合肥中新生代盆地构造单元划分.安徽地质,12(2):97~103.
吴海权,江来利,戴圣潜.2002.安徽霍山毛坦厂地区中生代地层层序的厘定.地层学杂志,26(1):9~15.
吴根耀,梁兴,陈焕疆.2007.试论郯城-庐江断裂带的形成、演化及其性质.地质科学,42(1):160~175.
吴因业,顾家裕.2002.油气层序地层学.北京:石油工业出版社,155~162.
万天丰,朱鸿.2002.中国大陆及邻区中生代—新生代大地构造与环境变迁.现代地质,16(2):107~120.
万天丰.2004.中国大地构造学纲要.北京:地质出版社,4~25,118~250.
徐春华,朱光,刘国生,谢成龙,王勇生,李长城.2005.合肥盆地钻井地层的同位素测年与地层划分.安徽地质,15(4):251~255.
徐佑德,赵明,徐春华,徐明,邱连贵.2002.合肥盆地安参1井中生代地层特征.石油实验地质,24(3):223~227.
邢光福,卢清地,陈荣,张正义,聂童春,李龙明,黄家龙,林敏.2008.华南晚中生代构造体制转折结束时限研究———兼与华北燕山地区对比.地质学报,82(4):451~463.
杨晓勇.2006.郯庐断裂带南段沙溪含铜斑岩体的40Ar/39Ar年代学研究及意义.矿物岩石,26(2):52~56.
邹才能,池英柳,李明,薛叔洁.2004.陆相层序地层学分析技术.北京:石油工业出版社,5~150.
赵越,徐刚,张拴宏,杨振宇,张岳桥,胡健民.2004.燕山运动与东亚构造体制的转变.地学前缘,1l(3):319~328.
朱光,宋传中,王道轩,刘国生,徐嘉炜.2001.郯庐断裂带走滑时代的40Ar/39Ar年代学研究及其构造意义.中国科学D辑:地球科学,31(3):250~256.
张交东,李学田,徐春华.2002.合肥坳陷表层地质与地震采集技术的关系研究.见:刘兴材,李丕龙主编,复式油气田论文集(胜利油田地学开拓者奖).北京:石油工业出版社,385~388.
张交东,刘成斋,刘德良,赵玉华,张升平,陈红梅.2003a.晚侏罗世大别山强烈隆升的地层证据.地学前缘,10(1):168.
张交东,刘德良,林会喜,邱连贵,徐佑德,任风楼,裴磊.2003b.郯庐断裂带南段巨型正花状构造的发现与地质意义.中国科技大学学报,33(4):401~404.
张交东,刘德良,杨晓勇,谈迎,曹国滨,张旭,耿绍宇.2003c.物化探测线编码系统的设计与实践.石油地球物理勘探,38(1):84~87.
张岳桥,赵越,董树文,杨农.2004.中国东部及邻区早白垩世裂陷盆地构造演化阶段.地学前缘,l1(3):123~133.
Christopher J.Modica,Eugene R.Brush.2004.Postrift sequencestratigraphy,paleogeography,and fill history of the deep-waterSantos Basin,offshore southeast Brazil.AAPG Bulletin,88(7):923~945.
Chen F,Guo J,Jiang L,Siebel W,Cong B,Satir M.2003.Provenance of the Beihuaiyanglower-grade metamorphic zone ofthe Dabie ultrahigh-pressure collisional orogen,China:Evidence fromzircon ages.Journal of Asian Earth Sciences,22:343~352.
Chen Duofu,Chen Xianpei,Chen Guangqian.2003.Sea-level changesand hydrothermal sedi mentary mineralization of large-superlargeore deposits among Sinian to Triassic in South China.Science inChina Series D-Earth,46(S):154~163.
David W.Houseknecht,Kenneth J.Bird.2004.Sequencestratigraphy of the Kingak Shale(Jurassic Lower Cretaceous),National Petroleum Reserve in Alaska.AAPG Bulletin,88(3):279~302.
Gale A S,Huggett J M,Like H P,Laurie E,E A Hail wood,Hardenbol J.2006.Correlation of Eocene-Oligocene marine andcontinental records:orbital cyclicity,magnetostratigraphy andsequence stratigraphy of the Solent Group,Isle of Wight,UK.Journal of the Geological Society,163:401~415.
Graham D.Moss,Donna L.Cathro,James A.Austin.2004.Sequence biostratigraphy of prograding cinoforms,NorthernCarnarvon Basin,Western Australia:a proxy for variations inOligocene to Pliocene Global Sea Level.PALAIOS,19:206~226.
Gilder S A,Leloup P H,Courtillot V,Chen Y,Coe R,Zhao X,Wang W,Hali m N,Cogne J P,Zhu R.1999.Tectonicevolution of the Tancheng Lujiang(Tan-Lu)fault via MiddleTriassic to Early Cenozoic paleomagnetic data.Journal ofGeophysical Research,104:15365~15390.
Gri mmer J C,Jonckheere R,Enkel mann E,Ratschbacher L,HackerB R,Blythe A E,Wagner G A,Wu Q,Liu S,Dong S.2002.Cretaceous-Cenozoic history of the southern Tan-Lu fault zone:apatite fission-track and structural constraints from the DabieShan(eastern China).Tectonophysics,359:225~253.
Li X H.2000.Cretaceous magmatismand lithospheric extension insoutheast China.Journal of Asian Earth Sciences,18:293~305.
Lin W,Faure M,Wang Q,Moni P,Panis D.2005.Triassicpolyphase deformation in the Feidong-Zhangbaling massif(Eastern China)andits place in the collision between the northChina and South China blocks.Journal of Asian Earth Sciences,25:121~136.
Li Z,Li R,Sun S,Wang Q.2004.Jurassic depositional records andsandstone provenances in Hefei Basin,central China:I mplication for Dabie orogenesis Source.The Island Arc,13:346~358.
Li Z,Li Y,Zheng J P,Han D.2007.Late Mesozoic tectonictransition of the eastern North China Craton:evidence frombasin-fill records.Geological Society,280:239~265.
Li Zhong,Sun Shu,Li Renwei,Jiang Maosheng.2001.Mesozoic fill-sequences in Hefei Basin:I mplication for Dabie Orogenesis,central China.Science in China Ser.D Earth Sciences,44(1):52~63.
Li Renwei,Wan Yusheng,Cheng Zhenu,Zhou Jianiong,XuYunhua,Li Zhong,Jiang Maosheng.2005a.The Dabie Orogenas the early Jurassic sedi mentary provenance:Constraints fromthe detrital zircon SHRI MP U-Pb dating.Science in China Ser.D Earth Sciences,48(2):145~155.
Li Renwei,Wan Yusheng,Cheng Zhenyu,Zhou Jianxiong,LiShuangying,Jin Fuquan,Meng Qingren,Li Zhong,JiangMaosheng.2005b.Provenance of Jurassic sedi ments in theHefei Basin,east-central China and the contribution of high-pressure and ultrahigh-pressure metamorphic rocks from theDabie Shan.Earth and Planetary Science Letters,231:279~294.
Hao T Y,Xu Y,Suh M,Xu Y,Liu J H,Zhang L L,Dai M G.2007.East Marginal Fault of the Yellow Sea:a part of theConjunction zone between Sino-Korea and Yangtze Block?geological society,Special Publication,280:281~291.
Meng Q R,Li S Y,Li R W.2007.Mesozoic evolution of the Hefeibasin in eastern China:sedi mentary response to deformationsinthe adjacent Dabieshan and along the Tan-Lu fault.GeologicSociety of American Bulletin,119:897~916.
Ren J,Tamaki K,Li S,Zhang J.2002.Late Mesozoic andCretaceous rifting and its dynamic setting in eastern China andadjacent areas.Tectonophysics,344:175~205.
Wang Xunlian.2002.On steps and methods for the establishment ofglobal boundary stratotype section and point(GSSP)fromtheviewpoint of integrated stratigraphy.Science in China Ser.DEarth Sciences,45(11):1027~1041.
Xie Xin,Xu Xisheng,Zou Haibo,Jiang Shaoyong,Zhang Ming,Qiu Jiansheng.2006.Early J2basaltsin SE China:Incipience oflarge-scale late Mesozoic magmatism.Sciencein China Series D-Earth Sciences,49(8):796~815.
版权所有：© 2023 中国地质图书馆 中国地质调查局地学文献中心