上扬子海南缘晚奥陶世赫南特期沉积相特征及海平面变化
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  • 英文篇名:Sedimentary Facies Features and Sea-level Fluctuation during the Upper Ordovician Hirnantian Period on the Southern Margin of the Upper Yangtze Sea
  • 作者:赵明胜 ; 王约
  • 英文作者:ZHAO Ming-sheng;WANG Yue;College of Paleontology, Shenyang Normal University;Key Laboratory of Economic Stratigraphy and Palaeogeography, Nanjing Institute of Geology and Palaeontology,Chinese Academy of Sciences;School of Resources and Environments, Guizhou University;
  • 关键词:沉积特征 ; 海平面变化 ; 观音桥段 ; 上扬子海南缘 ; 赫南特期 ; 晚奥陶世
  • 英文关键词:sedimentary characteristics;;sea-level fluctuation;;Guanyinqiao Member;;southern margin of the Upper Yangtze Sea;;Hirnantian;;Upper Ordovician
  • 中文刊名:DQXB
  • 英文刊名:Acta Geoscientica Sinica
  • 机构:沈阳师范大学古生物学院;中国科学院资源地层学与古地理学重点实验室中国科学院南京地质古生物研究所;贵州大学资源与环境工程学院;
  • 出版日期:2018-01-04 09:49
  • 出版单位:地球学报
  • 年:2018
  • 期:v.39;No.172
  • 基金:国家自然科学基金(编号:41762001);; 沈阳师范大学博士、引进人才科研项目启动基金(编号:BS201701);; 中国科学院资源地层学与古地理学重点实验室开放课题(编号:2016KF03)联合资助~~
  • 语种:中文;
  • 页:DQXB201802007
  • 页数:12
  • CN:02
  • ISSN:11-3474/P
  • 分类号:70-81
摘要
晚奥陶世赫南特期经历了由冈瓦纳冰川事件引起的全球海平面下降和温度降低,以及由此引发的生物集群绝灭事件,同时又是构造-沉积的转换期。因此,该时期成为奥陶—志留纪之交重大的地质事件转折期。本文通过野外露头对上扬子海南缘五峰组观音桥段岩性组合、古生物以及沉积构造的研究发现,晚奥陶世赫南特期上扬子海南缘经历了滨岸潮坪相、浅滩和浅水陆棚相三种沉积相类型的改造。滨岸潮坪相主要为混积潮坪,呈环状分布于滇黔桂古陆周缘及黔中水下隆起。浅滩相可识别出生屑滩和砂屑滩两个微环境,主要分布于近潮坪相带的重庆秀山、贵州松桃以及贵州凤冈等地区。浅水陆棚可分为浅水陆棚下部和浅水陆棚上部两个区域,与潮坪相带相接触并向北过渡,其中浅水陆棚区上部又可划分为浅水混积陆棚和浅水碎屑陆棚两种类型。另外,通过岩性与生物碎屑的组合和分布特征,表明赫南特期至少经历了一次完整的海平面升降变化,并为研究全球海平面的变化提供了新的材料。
        Hirnantian period of Upper Ordovician experienced sea level falling and decreasing temperature caused by Gondwana glacial event, resulting in mass extinction event. It was also a transition stage of structural evolution and sedimentation. It is thus proved to be one of important transition periods of geological event in geological history. Based on the research on lithologic combination, paleontology, and sedimentary structure of the outcrop of Guanyinqiao Member of Wufeng Formation on the southern margin of the Upper Yangtze Sea, whose margin experienced three types of sedimentary facies transformation, i.e., coastal tidal flat facies, shallow facies and shallow sea shelf facies. Coastal tidal flat facies were mainly mixed tidal flat, and distributed in the Yunnan–Guiyang–Guangxi ancient continental margin and the underwater uplift of Guizhou. Shallow facies was distributed in Xiushan of Chongqing, Songtao of Guizhou and Fenggang of Guizhou, located in near tidal flat zone as well as on bioclast beach and clast beach. Shallow sea shelf facies is in contact with coastal tidal flat facies and extends northward, and can be divided into lower shallow shelf and upper shallow shelf. Among these shelves, upper shallow shelf can be subdivided into shallow mixed shelf and shallow clast shelf. In addition, lithological association and biodetritus features indicate that there existed at least one complete sea-level change, which supplied new materials for global sea-level change.
引文
陈旭,樊隽轩,陈清,唐兰,侯旭东.2014.论广西运动的阶段性[J].中国科学:地球科学,44(5):842-850.
    陈旭,戎嘉余,樊隽轩,詹仁斌,MITCHELL C E,HARPER D AT,MELCHIN M J,彭平安,FINNEY S C,汪啸风.2006.奥陶系上统赫南特阶全球层型剖面和点位的建立[J].地层学杂志,30(4):289-305.
    陈旭,戎嘉余,樊隽轩,詹仁斌,张元动,李荣玉,王怿,MITCHELL C E,HARPER D A T.2000a.奥陶-志留系界线地层生物带的全球对比[J].古生物学报,39(1):100-114.
    陈旭,戎嘉余,樊隽轩,詹仁斌,张元动,王志浩,王宗哲,李荣玉,王怿,MITCHELL C E,HARPER D A T.2000b.扬子区奥陶纪末赫南特亚阶的生物地层学研究[J].地层学杂志,24(3):169-175.
    陈旭,戎嘉余,周志毅,张元动,詹仁斌,刘建波,樊隽轩.2001.上扬子区奥陶-志留纪之交的黔中隆起和宜昌上升[J].科学通报,46(2):1052-1056.
    陈源仁.1992.关于底栖组合应用中若干问题的讨论[J].成都地质学院学报,19(4):16-26.
    邓义楠,王约,陈洪德,侯明才,朱江,赵明胜.2010.黔北桐梓五峰组观音桥段双壳类和腹足类的生态意义[J].地层学杂志,34(3):328-333.
    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?[J].古地理学报,10(5):487-494.
    葛祥英,牟传龙,周恳恳,梁薇.2014.湖南晚奥陶世凯迪晚期-赫南特期沉积相及岩相古地理[J].沉积学报,32(1):8-18.
    葛治洲,戎嘉余,杨学长,刘耕武,董得源,伍鸿基.1979.西南地区的志留系[M]//中国科学院南京地质古生物研究所,著.西南地区碳酸盐生物地层.北京:科学出版社:155-220.
    郭峰.2011.碳酸盐岩沉积学[M].北京:石油工业出版社.
    何卫红,卜建军.2003.扬子海盆奥陶纪末介壳动物群的分布及其古地理意义[J].地球科学-中国地质大学学报,28(3):261-267.
    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[J].沉积学报,9(2):1-14.
    李贵鹏,詹仁斌,吴荣昌.2009.四川长宁双河晚奥陶世赫南特贝动物群及其对环境变化的响应[J].高校地质学报,15(3):304-317.
    李越,冯洪真,李军.2002.底栖藻对扬子地台西缘晚奥陶世生态危机的改善作用[J].古生物学报,41(2):211-218.
    李越,王建坡,张园园,顾澄皋.2008.华南奥陶-志留纪之交的碳酸盐岩对古气候事件的诠释[J].自然科学进展,18(10):122-128.
    李志明,龚淑云,陈建强,苏文博.1997.中国南方奥陶-志留纪沉积层序与构造运动的关系[J].地球科学-中国地质大学学报,22(5):526-530.
    刘宝珺,许效松,潘杏南,黄慧群,徐强.1993.中国南方古大陆沉积地壳演化与成矿[M].北京:科学出版社.
    刘本培,李儒峰,尤德宏.1994.黔南独山石炭系层序地层及麦粒蜓带冰川型全球平面变化[J].地球科学,16(5):553-564.
    刘若冰,田景春,魏志宏,张明文,钟水清,张光华,王碧.2006.川东南地区震旦系-志留系下组合有效烃源岩综合研究[J].天然气地球科学,17(6):824-828.
    刘伟,许效松,余谦,闫剑飞,门玉澎.张海全.2012.中上扬子晚奥陶世赫南特期岩相古地理[J].成都理工大学学报(自然科学版),39(1):32-39.
    梅冥相,马永生,邓军,张海,孟晓庆,陈永红,聂瑞贞,张从.2005.上扬子区下古生界层序地层格架的初步研究[J].现代地质,19(4):551-562.
    牟传龙,葛祥英,许效松,周恳恳,梁薇,王秀平.2014.中上扬子地区晚奥陶世岩相古地理及其油气地质意义[J].古地理学报,16(4):427-440.
    穆恩之,朱兆玲,陈均远,戎嘉余.1978.四川长宁双河附近奥陶纪地层[J].地层学杂志,2(2):105-121.
    聂海宽,金之钧,马鑫,刘忠宝,林拓,杨振恒.2017.四川盆地及邻区上奥陶统五峰组-下志留统龙马溪组底部笔石带及沉积特征[J].石油学报,38(2):160-174.
    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[J].古生物学报,26(5):507-535.
    戎嘉余,詹仁斌.1999.华南奥陶、志留纪腕足动物群的更替兼论奥陶纪末冰川活动的影响[J].现代地质,13(4):390-394.
    戎嘉余.1984.上扬子区晚奥陶世海退的生态地层证据与冰川活动影响[J].地层学杂志,8(1):19-29.
    沙庆安.2001.混合沉积和混积岩的讨论[J].古地理学报,3(3):63-66.
    苏文博,何龙清,王永标,龚淑云.2002.华南奥陶-志留系五峰组及龙马溪组底部斑脱岩与高分辨综合地层[J].中国科学(D辑),32(3):207-219.
    苏文博,李志明,ETTENSOHN F R,JOHNSON M E,HUFF W D,王巍,马超,李录,张磊,赵慧静.2007.华南五峰组-龙马溪组黑色岩系时空展布的主控因素及其启示[J].地球科学-中国地质大学学报,32(6):819-827.
    汤睿.2014.中上扬子地区晚奥陶世岩相古地理研究[D].荆州:长江大学.
    涂珅,王舟,王家生.2012.宜昌王家湾奥陶系-志留系界线地层高分辨率碳、氧稳定同位素记录及其成因[J].地球科学-中国地质大学学报,37(增刊2):165-174.
    王传尚,汪啸风,陈孝红,李志宏.2003.奥陶纪末期层序地层学研究[J].地球科学-中国地质大学学报,28(1):6-10.
    王远翀,梁薇,牟传龙,周恳恳,葛祥英.2015.渝东南-黔北地区赫南特期冰川事件的沉积响应[J].沉积学报,33(2):232-241.
    王远翀.2016.上扬子地区晚奥陶世赫南特期岩相古地理[D].成都:成都理工大学.
    肖传桃,姜衍文,朱忠德,李艺斌,潘云唐.1996a.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[J].高校地质学报,2(3):339-347.
    肖传桃,李建明,郭成贤.1996b.中上扬子地区五峰组沉积环境的再认识[J].四川地质学报,16(4):294-298.
    肖开华,李双建,汪新伟,张荣强,龙胜祥.2008.中上扬子区志留系油气成藏特点与勘探前景[J].石油与天然气地质,29(5):589-596.
    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[J].地质学报,78(6):726-732.
    徐世琦,李国辉,王廷栋.1998.加里东古隆起震旦系的烃源条件[J].天然气勘探与开发,21(4):13-22.
    徐世琦.1999.加里东古隆起震旦-寒武系成藏条件[J].天然气工业,19(6):7-10.
    许效松,万方,尹福光,陈明.2001.奥陶系宝塔组灰岩的环境相、生态相与成岩相[J].矿物岩石,21(3):64-68.
    严德天,陈代钊,王清晨,汪建国.2009.扬子地区奥陶系-志留系界线附近地球化学研究[J].中国科学(D辑):地球科学,39(3):285-299.
    严德天,王清晨,陈代钊,汪建国,王卓卓.2008.扬子及周缘地区上奥陶统-下志留统烃源岩发育环境及其控制因素[J].地质学报,82(3):321-327.
    杨永剑,刘家铎,田景春,孟万斌,张翔,祝贺.2011.塔里木盆地上奥陶统桑塔木组混合沉积特征及控制因素[J].地质论评,57(2):185-192.
    尹伯传.1988.扬子区晚奥陶世到早志留世海洋生物群的阶段性更替及观音桥组的时代[J].江汉石油学院学报,10(1):32-37.
    尹福光,许效松,万方,陈明.2001.华南地区加里东期前陆盆地演化过程中的沉积响应[J].地球学报,22(5):425-428.
    尹福光,许效松,万方,陈明.2002.加里东期上扬子区前陆盆地演化过程中的层序特征与地层划分[J].地层学杂志,26(4):315-319.
    张靖宇,陆永潮,付孝悦,张士万.2017.四川盆地涪陵地区五峰组-龙马溪组一段层序格架与沉积演化[J].地质科技情报,36(4):65-72.
    张琳娜,樊隽轩,陈清.2016.华南上奥陶统观音桥层的空间分布和古地理重建[J].科学通报,61(18):2053-2063.
    张鹏飞,陈世悦,杨怀宇,马士坤.2013.中上扬子地区碎屑岩-碳酸盐岩混积相发育特征及组合模式研究[J].天然气地球科学,24(2):365-371.
    赵明胜,田景春,王约.2013.黔中织金下寒武统牛蹄塘组黑色页岩中的白云岩及其沉积环境意义[J].地层学杂志,37(3):331-335.
    郑荣才,周刚,董霞,胡忠贵.2010.龙门山甘溪组谢家湾段混积相和混积层序地层学特征[J].沉积学报,28(1):33-41.
    BOUCOT A J.1975.Eovlution and extincition rate controls[M].Amsterdam:Scientific Publishing Company(Elsevier):427.
    CHEN Yuan-ren.1992.Discussion on some questions of the benthic assemblage application(BA1-6)[J].Journal of Chengdu College of Geology,19(4):16-26(in Chinese with English abstract).
    CHEN Xu,FAN Jun-xuan,CHEN Qing,TANG Lan,HOUXu-dong.2014.Toward a stepwise kwangsian orogeny[J].Science China Earth Sciences,44(5):842-850(in Chinese with English abstract).
    CHEN Xu,RONG Jia-yu,FAN Jun-xuan,ZHAN Ren-bin,MITCHELL C E,HARPER D A T,MELCHIN M J,PENGPing-an,FINNEY S C,WANG Xiao-feng.2006.A final report on the global stratotype section and point(GSSP)for the Hirnantian stage(Upper Ordovician)[J].Journal of Stratigraphy,30(4):289-305(in Chinese with English abstract).
    CHEN Xu,RONG JIA-yu,FAN Jun-xuan,ZHAN Ren-bin,ZHANG Yuan-dong,LI Rong-yu,WANG Yi,MITCHELL C E,HARPER D A T.2000a.A global correlation of Biozones across the Ordovician-Silurian boundary[J].Acta Palaeontologica Sinica,39(1):100-114(in Chinese with English abstract).
    CHEN Xu,RONG Jia-yu,FAN Jun-xuan,ZHAN Ren-bin,ZHANGYuan-dong,WANG Zhi-hao,WANG Zong-zhe,LI Rong-yu,WANG Yi,MITCHELL C E,HARPER D A T.2000b.Biostratigraphy of the Hirnantian Substage in the Yangtze region[J].Journal of Stratigraphy,24(3):169-175(in Chinese with English abstract).
    CHEN Xu,RONG Jia-yu,LI Yue,BOUCOT A J.2004.Facies patterns and geography of the Yangtze region,South China,through the Ordovician and Silurian transition[J].Palaeogeogr Palaeoclimatol Palaeoecol,204:353-372.
    CHEN Xu,RONG Jia-yu,MITCHELL C E,HARPER D A T,FANJun-xuan,ZHAN Ren-bin,ZHANG Yuan-dong,LI Rong-yu,WANG Yi.2000.Late Ordovician to earliest Silurian graptolite and brachiopod biozonation from the Yangtze region,South China,with a global correlation[J].Geological Magazine,137(6):623-650.
    CHEN Xu,RONG Jia-yu,ZHOU Zhi-yi,ZHANG Yuan-dong,ZHAN Ren-bin,LIU Jian-bo,FAN Jun-xuan.2001.The central Guizhou and Yichang uplifts,Upper Yangtze region,between Ordovician and Silurian[J].Chinese Science Bulletin,46(2):1052-1056(in Chinese with English abstract).
    DENG Yi-nan,WANG Yue,CHEN Hong-de,HOU Ming-cai,ZHUJiang,ZHAO Ming-sheng.2010.Bivalves and gastropods from the ordovician guanyinqiao member of the wufeng formation in Tongzi,Guizhou,South China,and their ecological significance[J].Journal of Stratigraphy,34(3):328-333(in Chinese with English abstract).
    FINNEY S C.2005.Global series and stages for the Ordovician system:A progress report[J].Geologica Acta,3(4):309-316.
    GAO Zhen-zhong,HE You-bin,LI Luo-zhao,QING Chong-wen,XIAO Ming-guo,CHENG Si-hong,ZHANG Wen-cheng,LIUWei-wei.2008.Genesis of the Guanyinqiao Member of Upper Ordovician Wufeng Formation in South China:“shallow water shelly facies”or deep water allogene sediments?[J].Journal of Palaeogeography,10(5):487-494(in Chinese with English abstract).
    GE Xiang-ying,MOU Chuan-long,ZHOU Ken-ken,LIANG Wei.2014.Sedimentary Facies and Lithofacies Palaeogeography in the Late Katian-Hirnantian of late Ordovician in Hunan Province[J].Acta Sedimentologica Sinica,32(1):8-18(in Chinese with English abstract).
    GE Zhi-zhou,RONG Jia-yu,YANG Xue-chang,LIU Geng-wu,DONG De-yuan,WU Hong-ji.1979.Silurian of Southwest China.In:Nanjing Institute of Geology and Palaeontology Carbonate,biostratigraphy in the Southwest China[M].Beijing:Science Press:155-220(in Chinese).
    GUO Feng.2011.Carbonate sedimentology[M].Beijing:Petroleum Industry Press(in Chinese).
    HE Wei-hong,BU Jian-jun.2003.Distribution of latest-Ordovician shell fauna in Yangtze basin and its paleogeographic significance[J].Earth science-journal of China University of Geosciences,28(3):261-267(in Chinese with English abstract).
    HUANG Zhi-cheng,HUANG Zhong-jin,CHENG Zhi-na.1991.Volcanic rock and radiolarian silicilith of Wufeng Formation lower Yangtze region[J].Acta Sedimentologica Sinica,9(2):1-14(in Chinese with English abstract).
    LI Gui-peng,ZHAN Ren-bin,WU Rong-chang.2009.Response of Hirnantia fauna to the environmental changes before the second phase of late Ordovician mass extinction:example from the Kuanyinchiao Formation at Shuanghe,Southern Sichuan,Southwest China[J].Geological Journal of China Universities,15(3):304-317(in Chinese with English abstract).
    LI Yue,FENG Hong-zhen,LI Jun.2002.Benthic algae in improvement of ecologic crisis of the late Ordovician in the west margin of the Yangtze platform[J].Acta Palaeontologica Sinica,41(2):211-218(in Chinese with English abstract).
    LI Yue,WANG Jian-po,ZHANG Yuan-yuan,GU Cheng-gao.2008.The annotation on climate from the Ordovician-Silurian in South China[J].Progress in Natural Science,18(10):122-128(in Chinese).
    LI Zhi-ming,GONG Shu-yun,CHEN Jian-qiang,SU Wen-bo.1997.Ordovician-Silurian depositional sequences and their relations with tectonic movement in South China[J].Earth Science-Journal of China University of Geosciences,22(5):526-530(in Chinese with English abstract).
    LIU Bao-jun,XU Xiao-song,PAN Xing-nan,HUANG Hui-qun,XU Qiang.1993.Depositional crustal evolution and Mineralization of paleo-continent in Southern China[M].Beijing:Science Press(in Chinese).
    LIU Ben-pei,LI Ru-feng,YOU De-hong.1994.Carboniferous sequence stratigraphy and glacio-eustasy of triticites zone in Southern Guizhou China[J].Earth Science-Journal of China University of Geosciences,16(5):553-564(in Chinese with English abstract).
    LIU Ruo-bing,TIAN Jing-chun,WEI Zhi-hong,ZHANGMing-wen,ZHONG Shui-qing,ZHANG Guang-hua,WANGBi.2006.Comprehensive research of effective hydrocarbon source rock of lower strata from Sinian to Silurian system in Southeast area of Sichuan Province[J].Natural Gas Geoscience,17(6):824-828(in Chinese with English abstract).
    LIU Wei,XU Xiao-song,YU Qian,YAN Jian-fei,MEN Yu-peng,ZHANG Hai-quan.2012.Lithofacies palaeography of the late Ordovician Hirnantian in the Middle-Upper Yangtze region of China[J].Journal of Chengdu University of Technology:Natural Science Edition,39(1):32-39(in Chinese with English abstract).
    MEI Ming-xiang,MA Yong-sheng,DENG Jun,ZHANG Hai,MENG Xiao-qing,CHEN Yong-hong,NIE Rui-zhen,ZHANGCong.2005.Sequence-stratigraphic framework for the early palaeozoic of the uppe-Yangtze region[J].Geoscience,19(4):551-562(in Chinese with English abstract).
    MOU Chuan-long,GE Xiang-ying,XU Xiao-song,ZHOUKen-ken,LIANG Wei,WANG Xiu-ping.2014.Lithofacies palaeogeography of the late Ordovician and its petroleum geological significance in Middle-Upper Yangtze region[J].Journal of Palaeogeography,16(4):427-440(in Chinese with English abstract).
    MU En-zhi,ZHU Zhao-ling,CHEN Jun-yuan,RONG Jia-yu.1978.Ordovicianstrata nearby the Shuanghe,Changning of Sichuan[J].Journal of Stratigraphy,2(2):105-121(in Chinese).
    NIE Hai-kuan,JIN Zhi-jun,MA Xin,LIU Zhong-bao,LIN Tuo,YANG Zhen-heng.2017.Graptolites zone and sedimentary characteristics of Upper Ordovician Wufeng Formation-lower Silurian Longmaxi Formation in Sichuan basin and its adjacent areas[J].Acta Petrolei Sinica,38(2):160-174(in Chinese with English abstract).
    RONG Jia-yu,CHEN Xu.1987.Faunal differentiation,biofacies and lithofacies pattern of late Ordovician(ashgillian)in South China[J].Acta Palaeontologica Sinica,26(5):507-535(in Chinese with English abstract).
    RONG Jia-yu,SHEN Shu-zhong.2002.Comparative analysis of the end-Permian and end-Ordovician brachiopod mass extinctions and survivals in South China[J].Palaeogeography Palaeoclimatology Palaeoecology,188:25-38.
    RONG Jia-yu,ZHAN Ren-bin.1999.Ordovician-Silurian brachiopod turnover in South China[J].Geoscience,13(4):390-394(in Chinese with English abstract).
    RONG Jia-yu.1984.Ecostratigraphical evidence of the regression in the Late Ordovician and influences of glacier activities in the Upper South China[J].Journal of Stratigraphy,8(1):19-29(in Chinese with English abstract).
    SHA Qing-an.2001.Discussion on mixing deposit and hunji rock[J].Journal of Palaeogeography,3(3):63-66(in Chinese with English abstract).
    SHEEHAN P M.1988.Late Ordovician events and the terminal Ordovician extinction[J].New Mexico Bureau of Mines and Mineral Resources Memoirs,44:405-415.
    SHEEHAN P M.2001.The Late Ordovician mass extinction[J].Annual Reviews of Earth and Planetary Science,29:331-364.
    SU Wen-bo,HE Long-qing,WANG Yong-biao,GONG Shu-yun.2002.K-bentonite beds and high-resolution integrated stratigraphy of the Uppermost Ordovician Wufeng and the lowest Silurian Longmaxi Formations in South China[J].Science in China Series D:Earth Sciences,32(3):207-219(in Chinese with English abstract).
    SU Wen-bo,LI Zhi-ming,ETTENSOHN F R,JOHNSON M E,HUFF W D,WANG Wei,MA Chao,LI Lu,ZHANG Lei,ZHAO Hui-jing.2007.Distribution of Black Shale in the Wufeng-Longmaxi Formations(Ordovician Silurian),South China:major controlling factors and implications[J].Earth science Journal of China University of Geosciences,32(6):819-827(in Chinese with English abstract).
    TANG Rui.2014.Study on lithofacies palaeogeography of late Ordovician in the middle and Upper Yangtze region[D].Jingzhou:Yangtze University(in Chinese with English abstract).
    TU Shen,WANG Zhou,WANG Jia-sheng.2012.Interpretation for high resolution stable carbon and oxygen isotope records across Ordovician-Silurian boundary from Wangjiawan,South China[J].Earth science-Journal of China University of Geosciences,37(suppl 2):165-174(in Chinese with English abstract).
    WANG Chuan-shang,WANG Xiao-feng,CHEN Xiao-hong,LIZhi-hong.2003.Study of sequence stratigraphy at terminal of Ordovician[J].Earth Science-Journal of China University of Geosciences,28(1):6-10(in Chinese with English abstract).
    WANG Yuan-chong,LIANG Wei,MOU Chuan-long,ZHOUKen-ken,GE Xiang-ying.2015.The sedimentary response to gondwana glaciation in Hirnantian(Ordovician)of the eastern Chongqing and the northern Guizhou region,South China[J].Acta Sedimentologica Sinica,33(2):232-241(in Chinese with English abstract).
    WANG Yuan-chong.2016.Lithofacies Paleogeography in Hirnantian Stage of late Ordovician in Upper Yangtze Region[D].Chengdu:Chengdu University of Techonology(in Chinese with English abstract).
    XIAO Chuan-tao,CHEN Zhi-yong,LIU Li,HE You-bin.2006.Ordovician cephalopod biofacies of South China and its provincialization[J].Earth Science-Journal of China University of Geosciences,17(3):221-230.
    XIAO Chuan-tao,JIANG Yan-wen,ZHU Zhong-de,LI Yi-bin,PAN Yun-tang.1996a.A study on Ordovician sequence stratigraphy in Yichang district,Hubei Province and sedimentary environment of the Wufeng Formation in Yangtze area[J].Geological Journal of China Universities,2(3):339-347(in Chinese with English abstract).
    XIAO Chuan-tao,LI Jian-ming,GUO Cheng-xian.1996b.Reunderstanding of sedimentary environ ment of the Wufeng Formation in Mid-Upper Yangtze area[J].Acta Geologica Sichuan,16(4):294-298(in Chinese with English abstract).
    XIAO Kai-hua,LI Shuang-jian,WANG Xin-wei,ZHANGRong-qiang,LONG Sheng-xiang.2008.Hydrocarbon accumulation features and exploration direction in the Silurian of the Middle-Upper Yangtze Platform[J].Oil and Gas Geology,29(5):589-596(in Chinese with English abstract).
    XU Lun-xun,XIAO Chuan-tao,GONG Wen-ping,HE You-bin.2004.A study on the deep-sea sediment of the Guanyinqiao Member of the Upper Ordovician Wufeng Formation in the Yangtze Area[J].Acta Geologica Sinica,78(6):726-732(in Chinese with English abstract).
    XU Shi-qi,LI Guo-hui,WANG Ting-dong.1998.The hydrocarbon source condition of Sinian system of the caledonian palaeo-uplift[J].Natural Gas Exploration and Development,21(4):13-22(in Chinese).
    XU Shi-qi.1999.Conditions of forming reservoirs in Sinian-Cambrian of caledonian ancient uplift[J].Natural Gas Industry,19(6):7-10(in Chinese with English abstract).
    XU Xiao-song,WAN Fang,YIN Fu-guang,CHEN Ming.2001.Environment facies,ecological facies and diagenetic facies of baota formation,of late Ordovician[J].Journal of Mineralogy and Petrology,21(3):64-68(in Chinese with English abstract).
    YAN De-tian,WANG Qing-chen,CHEN Dai-zhao,WANGJian-guo,WANG Zhuo-zhuo.2008.Sedimentary environment and development controls of the hydrocarbon sources beds:the Upper Ordovician Wufeng Formation and the lower Silurian Longmaxi Formation in the Yangtze area[J].Acta Geologica Sinica,82(3):321-327(in Chinese with English abstract).
    YAN De-tian,CHEN Dai-zhao,WANG Qing-chen,WANGJian-guo.2009.Geochemical changes across the Ordovician-Silurian transition on the Yangtze platform,South China[J].Science in China Series D:Earth Sciences,39(3):285-299(in Chinese with English abstract).
    YANG Yong-jian,LIU Jia-duo,TIAN Jing-chun,MENG Wan-bin,ZHANG Xiang,ZHU He.2011.Mixed sedimentaru characteristics and controlling factors of Upper Ordovician Sangtamu Formation in Tarim basin[J].Geologiacal Review,57(2):185-192(in Chinese with English abstract).
    YIN Bo-chuan.1988.A phasic alternation of marine biota from late Ordovician to early Silurian and the geological age of the Guanyinqiao Formation[J].Journal of Jianghan Petroleum Institute,10(1):32-37(in Chinese with English abstract).
    YIN Fu-guang,XU Xiao-song,WAN Fang,CHENG Ming.2001.The sedimentary response to the evolutionary process of Caledonian foreland basin system in South China[J].Acta Geoscientia Sinica,22(5):425-428(in Chinese with English abstract).
    YIN Fu-guang,XU Xiao-song,WAN Fang,CHENG Ming.2002.Characteristic of seqence and stratigraphical division in evolution of Upper Yangtze region during Caledonian[J].Journal of Stratigraphy,26(4):315-319(in Chinese with English abstract).
    ZHANG Jing-yu,LU Yong-chao,FU Xiao-yue,ZHANG Shi-wan.2017.Sequence stratigraphic framework and sedimentary evolution of Wufeng formation-the 1st member of Longmaxi Formation infuling area,Sichuan basin[J].Geological Science and Technology Information,36(4):65-72(in Chinese with English abstract).
    ZHANG Lin-na,FAN Jun-xuan,CHEN Qing.2016.Geographic distribution and palaeogeographic reconstruction of the Upper Ordovician Kuanyinchiao Bed in South China[J].Chinese Science Bulletin,61(18):2053-2063(in Chinese).
    ZHANG Peng-fei,CHEN Shi-yue,WANG Huai-yu,MA Shi-kun.2013.Research of the mixed model and developmental characteristic of the clastic-carbonatite diamictite facies in the middle of Yangzi area[J].Natural Gas Geoscience,24(2):365-371(in Chinese with English abstract).
    ZHANG Tong-gang,SHEN Ya-nan,ZHAN Ren-bin,SHENShu-zhong,CHEN Xu.2009.Large perturbations of the carbon and sulfur cycle associated with the late Ordovician mass extinction in South China[J].Geology,37(4):299-302.
    ZHAO Ming-sheng,TIAN Jing-chun,WANG Yue.2013.The dolostone in lower Cambrian Niutitang formation from Zhijin region of central Guizhou and its sedimentary environment significances[J].Journal of Stratigraphy,37(3):331-335(in Chinese with English abstract).
    ZHENG Rong-cai,ZHOU Gang,DONG Xia,HU Zhong-gui.2010.The Characteristics of hybrid facies and hybrid sequence of Xiejiawan Member of Ganxi Formation in the Longmenshan area[J].Acta Sedimentologica Sinica,28(1):33-41(in Chinese with English abstract).

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