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层序底界面的物质表现形式——以中国南方海相震旦系—中三叠统为例

田景春,  陈洪德,  覃建雄,  侯明才,  赵俊兴

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文章导航 > 沉积学报  > 2003 >  21(4): 675-682
田景春, 陈洪德, 覃建雄, 侯明才, 赵俊兴. 层序底界面的物质表现形式——以中国南方海相震旦系—中三叠统为例[J]. 沉积学报, 2003, 21(4): 675-682.
引用本文: 田景春, 陈洪德, 覃建雄, 侯明才, 赵俊兴. 层序底界面的物质表现形式——以中国南方海相震旦系—中三叠统为例[J]. 沉积学报, 2003, 21(4): 675-682.
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TIAN Jing chun, CHEN Hong de, QIN Jian xiong, HOU Ming cai, ZHAO Jun xing. The Apparent Types of Sequence Bottom Boundary Surface--Taking marine Sinian System to Middle Triassic Series in South China as an example[J]. Acta Sedimentologica Sinica, 2003, 21(4): 675-682.
Citation: TIAN Jing chun, CHEN Hong de, QIN Jian xiong, HOU Ming cai, ZHAO Jun xing. The Apparent Types of Sequence Bottom Boundary Surface--Taking marine Sinian System to Middle Triassic Series in South China as an example[J]. Acta Sedimentologica Sinica, 2003, 21(4): 675-682.
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层序底界面的物质表现形式——以中国南方海相震旦系—中三叠统为例

  • 油气藏地质及开发工程国家重点实验室成都理工大学沉积地质研究所 成都 610059

详细信息
    作者简介:

    田景春 男 1963 年出生 教授、博士导师 储层沉积学、层序地层学、沉积地球化学

  • 中图分类号: P539.2

The Apparent Types of Sequence Bottom Boundary Surface--Taking marine Sinian System to Middle Triassic Series in South China as an example

  • State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation Institute of Sedimentology, Chengdu University of Technology, Chengdu 610059

    摘要
  • 摘要: 众所周知,在层序地层学研究中最关键的是层序划分,而层序划分的关键是有关界面的识别,可用于确定层序的界面包括层序的底界面,初始海泛面和最大海泛面,其中最为重要的是层序底界面的识别,这是层序划分的基础和前提。以中国南方海相震旦系—中三叠统为例,在大量野外剖面详细观测的基础上,识别出了层序底界面的物质表现形式有 9种类型,它们分别是:①古风化壳,②渣状层,③河流回春作用面,④古喀斯特作用面,⑤斜坡重力流冲刷侵蚀面,⑥盆地内浊流侵蚀面,⑦火山事件作用面,⑧岩性、岩相转换面,⑨上超面。详细讨论了各类型界面的特征,这对于正确识别和划分层序具有重要的意义
    Abstract: It is well known that the key of research on sequence stratigraphy is sequence division, but first of all the key of sequence division is identification of boundary surface. The boundary surface of defined sequence included sequence bottom boundary surface first trangressive surface and maximum marine f looding surface. Among them, the most important is bottom boundary surface indentification because it is sequence division foundation. The paper, taking marine Sinian system to Middle Triassic Series in south China as an example, through anlyses of filed geologic sections, identified nine types sequence bottom boundary surfaces which are: ( 1) weathering crust;(2) Paleosol;(3) Erosion surface of river rejuvenation;(4) Action surface of ancient karst;(5) Washing erosion surface of gravity flow on slop;(6) Erosion surface of turbidity flow in basin;(7) Action surface of volcano event;(8) Transition surface of rock character and facies;(9) onlap surface. Research features of above boundary surfaces in detail is very important for sequence division.
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    • 参考文献(20)
  • [1] 陈洪德,覃建雄,田景春,等.右江盆地层序充填动力学初探[J].沉积学报,2000,18(2):165～171[Chen Hongde,Qin Jianxiong,Tian Jingchun,et al. Sequence filling dynamics of Youjiang basin,Southern China[J]. Acta Sedimentologica Sinica, 2000,17(4):165～171]
    [2] 冯庆来.桂西北早石炭世台槽地区露头层序地层及海平面变化研究[J].地球科学,1994,19(5):609～618[Feng Qinglai. On outcrop sequence stratigraphy of intraplatform trough and sea level change during early Carboniferous in northwestern Guangxi[J]. Earth Science, 1994,19(5):609～618]
    [3] 侯中健,陈洪德,田景春.右江盆地海相泥盆系-中三叠统层序界面成因类型与盆地演化[J].沉积学报,2000,18(2):205～209[Hou Zhongjian,Chen Hongde,Tian Jingchun,et al. Genesis of sequence boundary and basin evolution in Youjiang basin during the Devonian to the Middle Triassic[J]. Acta Sedimentologica Sinica, 2000,17(4):205～209]
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    [5] 李儒峰,刘本培,赵澄林.扬子板块石炭纪沉积层序及全球性对比研究[J].沉积学报,1997,15(3):23～28[Li Rufeng, Liu Benpei, Zhao Chenglin. Correlation of Carboniferous depositional sequences on the Yangtze plate with others on a global scale[J]. Acta Sedimentologica Sinica, 1997,15(3);23～28]
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出版历程
  • 收稿日期:  2002-05-31
  • 修回日期:  2002-09-09
  • 刊出日期:  2003-12-10

目录

    层序底界面的物质表现形式——以中国南方海相震旦系—中三叠统为例

    • 油气藏地质及开发工程国家重点实验室成都理工大学沉积地质研究所 成都 610059
      • 作者简介:

      田景春 男 1963 年出生 教授、博士导师 储层沉积学、层序地层学、沉积地球化学

    • 收稿日期: 2002-05-31
    • 修回日期: 2002-09-09
    • 刊出日期: 2003-12-10

    • 中图分类号: P539.2

    摘要: 众所周知,在层序地层学研究中最关键的是层序划分,而层序划分的关键是有关界面的识别,可用于确定层序的界面包括层序的底界面,初始海泛面和最大海泛面,其中最为重要的是层序底界面的识别,这是层序划分的基础和前提。以中国南方海相震旦系—中三叠统为例,在大量野外剖面详细观测的基础上,识别出了层序底界面的物质表现形式有 9种类型,它们分别是:①古风化壳,②渣状层,③河流回春作用面,④古喀斯特作用面,⑤斜坡重力流冲刷侵蚀面,⑥盆地内浊流侵蚀面,⑦火山事件作用面,⑧岩性、岩相转换面,⑨上超面。详细讨论了各类型界面的特征,这对于正确识别和划分层序具有重要的意义

    English Abstract

    田景春, 陈洪德, 覃建雄, 侯明才, 赵俊兴. 层序底界面的物质表现形式——以中国南方海相震旦系—中三叠统为例[J]. 沉积学报, 2003, 21(4): 675-682.
    引用本文: 田景春, 陈洪德, 覃建雄, 侯明才, 赵俊兴. 层序底界面的物质表现形式——以中国南方海相震旦系—中三叠统为例[J]. 沉积学报, 2003, 21(4): 675-682.
    shu
    TIAN Jing chun, CHEN Hong de, QIN Jian xiong, HOU Ming cai, ZHAO Jun xing. The Apparent Types of Sequence Bottom Boundary Surface--Taking marine Sinian System to Middle Triassic Series in South China as an example[J]. Acta Sedimentologica Sinica, 2003, 21(4): 675-682.
    Citation: TIAN Jing chun, CHEN Hong de, QIN Jian xiong, HOU Ming cai, ZHAO Jun xing. The Apparent Types of Sequence Bottom Boundary Surface--Taking marine Sinian System to Middle Triassic Series in South China as an example[J]. Acta Sedimentologica Sinica, 2003, 21(4): 675-682.
    shu

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