湖盆无曝露缓坡带层序界面特征及成因——以松辽盆地他拉哈地区上白垩统为例

辛仁臣

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湖盆无曝露缓坡带层序界面特征及成因——以松辽盆地他拉哈地区上白垩统为例

辛仁臣

文章导航 > 沉积学报 > 2008 > 26(1): 77-85

辛仁臣. 湖盆无曝露缓坡带层序界面特征及成因——以松辽盆地他拉哈地区上白垩统为例[J]. 沉积学报, 2008, 26(1): 77-85.

引用本文:

辛仁臣. 湖盆无曝露缓坡带层序界面特征及成因——以松辽盆地他拉哈地区上白垩统为例[J]. 沉积学报, 2008, 26(1): 77-85.

XIN Renchen. Characteristics and Genesis of Sequence Boundaries on Subaqueous 〖JZ〗Gentle Slope of Lacustrine Basin:a case study on Upper Cretaceous in Talaha region of Songliao Basin[J]. Acta Sedimentologica Sinica, 2008, 26(1): 77-85.

Citation:

辛仁臣. 湖盆无曝露缓坡带层序界面特征及成因——以松辽盆地他拉哈地区上白垩统为例[J]. 沉积学报, 2008, 26(1): 77-85.

引用本文:

辛仁臣. 湖盆无曝露缓坡带层序界面特征及成因——以松辽盆地他拉哈地区上白垩统为例[J]. 沉积学报, 2008, 26(1): 77-85.

Citation:

湖盆无曝露缓坡带层序界面特征及成因——以松辽盆地他拉哈地区上白垩统为例

辛仁臣

中国地质大学海洋学院北京 100083

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通讯作者:
辛仁臣

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文章访问数: 1667
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Characteristics and Genesis of Sequence Boundaries on Subaqueous 〖JZ〗Gentle Slope of Lacustrine Basin:a case study on Upper Cretaceous in Talaha region of Songliao Basin

XIN Renchen

School of Marine Sciences, China University of Geosciences, Beijing 100083

More Information

Corresponding author: XIN Renchen

摘要

摘要: 松辽盆地他拉哈地区在泉头组四段—嫩江组三段沉积时期为长期被湖水覆盖的缓坡带，层序地层学研究结果表明，层序界面在岩性—测井曲线特征上，有7种表现形式：(1)砂岩发育段内正反旋回的分界面；(2)砂岩发育段与含砂泥岩层（组）之间的正反旋回的分界面；(3)含砂泥岩层（组）与砂岩发育段之间的正反旋回的分界面；(4)钙质含量较高层段内正反旋回的分界面；(5)钙质含量较高的层（组）与含砂泥岩层（组）之间的正反旋回的分界面；(6)含砂泥岩层（组）与钙质含量较高的层（组）之间的正反旋回的分界面；(7)含砂泥岩层（组）内部的正反旋回的分界面。二级和三级层序界面以砂岩发育段内正反旋回的分界面为主，分别占92％和39％。四级层序，7种类型的界面出现的概率差别较小，表现形式具有真正的层序界面特征多样性。层序界面的特征取决于湖平面的升降、物源供应强度和蒸发作用的强度。
- 层序地层 /
- 层序界面 /
- 成因分析 /
- 缓坡带 /
- 松辽盆地
Abstract: Talaha region in Songliao Basin is the gentle slope which was covered with water in long term during the depositional periods of the Fourth Member of Quantou Formation to Third Member of Nenjinag Formation. On the basis of sequence stratigraphy studies, it is found that there are 7 types of sequence boundaries manifestation in the drilling well data, such as: (1)boundary between uppercoarsing cycle and upperfining cycle within the sandrich part of well profile; (2) boundary between uppercoarsing sandrich cycle and upperfining mudrich cycle of well profile; (3) boundary between uppercoarsing mudrich cycle and upperfining sandrich cycle of well profile; (4) boundary between uppercoarsing cycle and upperfining cycle within carbonaterich part of well profile; (5) boundary between uppercoarsing carbonaterich cycle and upperfining mudrich cycle of well profile; (6) boundary between uppercoarsing mudrich cycle and upperfining carbonaterich cycle of well profile; (7) boundary between uppercoarsing cycle and upperfining cycle within mudrich part of well profile. The secondorder and thirdorder sequence boundaries dominated by the boundary between uppercoarsing cycle and upperfining cycle within the sandrich part of well profile, respectively is 92% and 39%. The fourthorder sequence boundaries are provided with diversity, there are near equal probability of 7 types of sequence boundaries. The characteristics of sequence boundaries are controlled by fluctuation of lake level, supply of source and intensity of evaporation.
- sequence stratigraphy /
- sequence boundary /
- genetic analysis /
- gentle slope /
- Songliao Basin

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[1]	谈明轩, 朱筱敏, 张自力, 孙浩南. 构造掀斜主导的断陷湖盆缓坡层序“源—汇”正演模拟定量研究 . 沉积学报, 2022, 40(6): 1481-1493. doi: 10.14027/j.issn.1000-0550.2022.061
[2]	张晨晨, 张顺, 魏巍, 吴朝东. 松辽盆地嫩江组凝缩层形成机制及其地质意义 . 沉积学报, 2015, 33(5): 891-898. doi: 10.14027/j.cnki.cjxb.2015.05.005
[3]	. 鄂尔多斯盆地奥陶系层序地层格架 . 沉积学报, 2014, 32(1): 44-60.
[4]	. 松辽盆地嫩江组层序构型及其沉积演化 . 沉积学报, 2013, 31(05): 920-927.
[5]	. 地层记录中旋回层序界面的识别方法及原理 . 沉积学报, 2012, 30(6): 991-998.
[6]	梁宏斌. 断陷湖盆缓坡带高位三角洲体系与油气成藏组合特征分析——以二连盆地吉尔嘎朗图凹陷为例 . 沉积学报, 2011, 29(4): 783-792.
[7]	张世广. 高分辨率层序地层学在储层宏观非均质性研究中的应用——以松辽盆地朝阳沟油田朝1—朝气3区块扶余油层为例 . 沉积学报, 2009, 27(3): 458-469.
[8]	刘新颖. 印尼Sunda盆地裂陷期层序地层与沉积充填特征 . 沉积学报, 2009, 27(2): 280-288.
[9]	罗忠. 层序界面对砂岩成岩作用及储层质量的影响——以鄂尔多斯盆地延河露头上三叠统延长组为例 . 沉积学报, 2007, 25(6): 903-914.
[10]	. 鄂尔多斯盆地陇东地区延长组沉积相特征与层序地层分析 . 沉积学报, 2006, 24(4): 549-554.
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[12]	辛仁臣, 蔡希源, 王英民. 松辽坳陷深水湖盆层序界面特征及低位域沉积模式 . 沉积学报, 2004, 22(3): 387-392.
[13]	李凤杰, 王多云, 宋广寿, 郑希民, 刘自亮, 王峰, 王志坤, 李树同. 陕甘宁盆地坳陷型湖盆缓坡带三角洲前缘短期基准面旋回与储层成因分析 . 沉积学报, 2004, 22(1): 73-78.
[14]	操应长, 姜在兴, 夏斌, 杨伟利, 张家震. 声波时差测井资料识别层序地层单元界面的方法、原理及实例 . 沉积学报, 2003, 21(2): 318-323.
[15]	杨玉峰, 王占国, 张维琴. 松辽盆地湖相泥岩地层有机碳分布特征及层序分析 . 沉积学报, 2003, 21(2): 340-344.
[16]	李凤杰, 王多云, 郑希民, 刘自亮, 王峰, 李树同, 王志坤. 陕甘宁盆地华池地区延长组缓坡带三角洲前缘的微相构成 . 沉积学报, 2002, 20(4): 582-587.
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湖盆无曝露缓坡带层序界面特征及成因——以松辽盆地他拉哈地区上白垩统为例

辛仁臣

中国地质大学海洋学院北京 100083

通讯作者: 辛仁臣

收稿日期: 1900-01-01
修回日期: 1900-01-01
刊出日期: 2008-02-10

关键词:

缓坡带 /

摘要: 松辽盆地他拉哈地区在泉头组四段—嫩江组三段沉积时期为长期被湖水覆盖的缓坡带，层序地层学研究结果表明，层序界面在岩性—测井曲线特征上，有7种表现形式：(1)砂岩发育段内正反旋回的分界面；(2)砂岩发育段与含砂泥岩层（组）之间的正反旋回的分界面；(3)含砂泥岩层（组）与砂岩发育段之间的正反旋回的分界面；(4)钙质含量较高层段内正反旋回的分界面；(5)钙质含量较高的层（组）与含砂泥岩层（组）之间的正反旋回的分界面；(6)含砂泥岩层（组）与钙质含量较高的层（组）之间的正反旋回的分界面；(7)含砂泥岩层（组）内部的正反旋回的分界面。二级和三级层序界面以砂岩发育段内正反旋回的分界面为主，分别占92％和39％。四级层序，7种类型的界面出现的概率差别较小，表现形式具有真正的层序界面特征多样性。层序界面的特征取决于湖平面的升降、物源供应强度和蒸发作用的强度。

English Abstract

Characteristics and Genesis of Sequence Boundaries on Subaqueous 〖JZ〗Gentle Slope of Lacustrine Basin:a case study on Upper Cretaceous in Talaha region of Songliao Basin

XIN Renchen

School of Marine Sciences, China University of Geosciences, Beijing 100083

Corresponding author: XIN Renchen

Received Date: 1900-01-01
Rev Recd Date: 1900-01-01
Publish Date: 2008-02-10

Keywords:

Abstract: Talaha region in Songliao Basin is the gentle slope which was covered with water in long term during the depositional periods of the Fourth Member of Quantou Formation to Third Member of Nenjinag Formation. On the basis of sequence stratigraphy studies, it is found that there are 7 types of sequence boundaries manifestation in the drilling well data, such as: (1)boundary between uppercoarsing cycle and upperfining cycle within the sandrich part of well profile; (2) boundary between uppercoarsing sandrich cycle and upperfining mudrich cycle of well profile; (3) boundary between uppercoarsing mudrich cycle and upperfining sandrich cycle of well profile; (4) boundary between uppercoarsing cycle and upperfining cycle within carbonaterich part of well profile; (5) boundary between uppercoarsing carbonaterich cycle and upperfining mudrich cycle of well profile; (6) boundary between uppercoarsing mudrich cycle and upperfining carbonaterich cycle of well profile; (7) boundary between uppercoarsing cycle and upperfining cycle within mudrich part of well profile. The secondorder and thirdorder sequence boundaries dominated by the boundary between uppercoarsing cycle and upperfining cycle within the sandrich part of well profile, respectively is 92% and 39%. The fourthorder sequence boundaries are provided with diversity, there are near equal probability of 7 types of sequence boundaries. The characteristics of sequence boundaries are controlled by fluctuation of lake level, supply of source and intensity of evaporation.

辛仁臣. 湖盆无曝露缓坡带层序界面特征及成因——以松辽盆地他拉哈地区上白垩统为例[J]. 沉积学报, 2008, 26(1): 77-85.

引用本文:

辛仁臣. 湖盆无曝露缓坡带层序界面特征及成因——以松辽盆地他拉哈地区上白垩统为例[J]. 沉积学报, 2008, 26(1): 77-85.

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湖盆无曝露缓坡带层序界面特征及成因——以松辽盆地他拉哈地区上白垩统为例

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辛仁臣

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Characteristics and Genesis of Sequence Boundaries on Subaqueous 〖JZ〗Gentle Slope of Lacustrine Basin:a case study on Upper Cretaceous in Talaha region of Songliao Basin

Corresponding author: XIN Renchen

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湖盆无曝露缓坡带层序界面特征及成因——以松辽盆地他拉哈地区上白垩统为例

中国地质大学海洋学院北京 100083

通讯作者: 辛仁臣

English Abstract

Characteristics and Genesis of Sequence Boundaries on Subaqueous 〖JZ〗Gentle Slope of Lacustrine Basin:a case study on Upper Cretaceous in Talaha region of Songliao Basin

School of Marine Sciences, China University of Geosciences, Beijing 100083

Corresponding author: XIN Renchen

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湖盆无曝露缓坡带层序界面特征及成因——以松辽盆地他拉哈地区上白垩统为例

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Characteristics and Genesis of Sequence Boundaries on Subaqueous 〖JZ〗Gentle Slope of Lacustrine Basin:a case study on Upper Cretaceous in Talaha region of Songliao Basin

Corresponding author: XIN Renchen

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湖盆无曝露缓坡带层序界面特征及成因——以松辽盆地他拉哈地区上白垩统为例

中国地质大学 海洋学院 北京 100083

通讯作者: 辛仁臣

English Abstract

Characteristics and Genesis of Sequence Boundaries on Subaqueous 〖JZ〗Gentle Slope of Lacustrine Basin:a case study on Upper Cretaceous in Talaha region of Songliao Basin

School of Marine Sciences, China University of Geosciences, Beijing 100083

Corresponding author: XIN Renchen

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通讯作者:
辛仁臣

中国地质大学海洋学院北京 100083