古水深曲线在测井资料层序地层分析中的应用

康安; 朱筱敏; 王贵文; 康强

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古水深曲线在测井资料层序地层分析中的应用

康安, 朱筱敏, 王贵文, 康强

文章导航 > 沉积学报 > 2000 > 18(1): 63-67

康安, 朱筱敏, 王贵文, 康强. 古水深曲线在测井资料层序地层分析中的应用[J]. 沉积学报, 2000, 18(1): 63-67.

引用本文:

康安, 朱筱敏, 王贵文, 康强. 古水深曲线在测井资料层序地层分析中的应用[J]. 沉积学报, 2000, 18(1): 63-67.

KANG An, ZHU Xiao min, WANG Gui wen, KANG Qiang. Application of Paleobathymetric Curve in the Sequence Stratigraphy of Well-logging Data[J]. Acta Sedimentologica Sinica, 2000, 18(1): 63-67.

Citation:

KANG An, ZHU Xiao min, WANG Gui wen, KANG Qiang. Application of Paleobathymetric Curve in the Sequence Stratigraphy of Well-logging Data[J]. Acta Sedimentologica Sinica, 2000, 18(1): 63-67.

康安, 朱筱敏, 王贵文, 康强. 古水深曲线在测井资料层序地层分析中的应用[J]. 沉积学报, 2000, 18(1): 63-67.

引用本文:

康安, 朱筱敏, 王贵文, 康强. 古水深曲线在测井资料层序地层分析中的应用[J]. 沉积学报, 2000, 18(1): 63-67.

KANG An, ZHU Xiao min, WANG Gui wen, KANG Qiang. Application of Paleobathymetric Curve in the Sequence Stratigraphy of Well-logging Data[J]. Acta Sedimentologica Sinica, 2000, 18(1): 63-67.

Citation:

KANG An, ZHU Xiao min, WANG Gui wen, KANG Qiang. Application of Paleobathymetric Curve in the Sequence Stratigraphy of Well-logging Data[J]. Acta Sedimentologica Sinica, 2000, 18(1): 63-67.

古水深曲线在测井资料层序地层分析中的应用

石油大学地球科学系北京昌平 102200

详细信息

作者简介:
康安,男,1972年出生,博士研究生,沉积学、层序地层学和盆地分析

中图分类号: P539.2

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文章访问数: 579
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Application of Paleobathymetric Curve in the Sequence Stratigraphy of Well-logging Data

Geoscience Department, University of Petroleum, Changping Beijing 102200

摘要

摘要: 层序地层学的精华就是综合应用露头、钻测井和地震资料进行层序地层分析。因此,在缺乏以陆上暴露不整合面为特征的层序界面的湖相沉积中,如何应用测井资料进行层序划分就成为层序地层学研究中一个重要环节。本文以柴达木盆地金达 1井第四系为例,介绍了一种综合利用岩芯、岩屑和电测曲线等测井资料,通过相对古水深曲线的建立,来进行层序地层分析的快速简便的方法。
- 测井 /
- 古水深曲线 /
- 层序地层
Abstract: It is well known that integrated use of outcrop, well-logging and seismic data is the key to sequence stratigraphy. Therefore, how to identify the sequence boundary by well-logging in the lacustrine sediments which are lack in the unconformity is critical step to sequence stratigraphic analysis. With an example of sequencestratigraphy of Quaternary in well Jinda1, Qaidam basin, this paper presents the basic procedures of new approach for a stratigraphic subdivision of well logs into sequences by reconstruction of paleobathymetric curve. After the log facies analysis, six kinds of lithofacies have been recognized in Quaternary which are dark-grey shale, brown shale, grey silty shale, carbargillite, shaly siltstone and siltstone. For each Lithofacies association a sedimentologically coherent paleoenvironmental interpretation has to be established. Hence, a distinct paleobathymetric range is assigned to each lithofacies unit. Based on this relative paleo-waterdepth, paleobathymetric curve of Quaternary in well Jinda1 has been established from a vertical succession of lithofacies. This water-depth curve helps to identify stratigraphic sequence of different scales.This approach is based on the identification of bathymetry turnaround trends in the lithofacies succession. The maximum regressive surface is placed at the lowest waterdepth values on the smoothed bathymetry curve. The maximum regressive surface is identical to the sequence boundary. The maximum flooding surface is placed at the deepest bathymetry as the closest approximation. This horizon separates underlying transgressive half cycle from overlying regressive half-cycle. Based on the rules above, four sequences are identified in the Quaternary sediment of Jinda1 Well. Each sequence consists of two systems tracts separated by maximum flooding surface. It is clear that there are two scales of waterdepth cycle in the bathymetry curve. More frequent fluctuation in the bathymetry curve can be considered as the response to the high order stratigraphic sequence. At last, the prospective source rock, favorable reservoir and potential caprock have been predicted.
- paleobathymetry /
- sequence stratigraphy /
- well-logging

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参考文献(4)

[1]	C．K．威尔格斯等编，徐怀大等译，层序地层学原理[M].北京：石油工业出版社，1993，47～255
[2]	朱筱敏.层序地层学原理及应用[M].北京：石油工业出版社，1998，3～102
[3]	郭荣坤，王贵文，唐为清.测井沉积学解释计算机辅助系统[M].石油工业出版社.北京：1996，79～100
[4]	Herbert Th,.Eichenseer，Jean-Pierre Leduc, Automated genetic sequence stratigraphy applied to wireline logs[J]. Bull. Centres Rech. Explor.-Prod. Elf aquitaine. 1996，20(2)：278～307

[1]	汤艳玲, 李凌, 谭秀成, 李明隆, 芦飞凡, 张本健. 川西南部地区下二叠统栖霞阶层序地层特征及岩相古地理 . 沉积学报, 2024, 42(2): 575-592. doi: 10.14027/j.issn.1000-0550.2022.043
[2]	黄献好, 孙玉琦, 王伟超, 刘炳强, 张少林, 张语涛, 邵龙义. 柴北缘西大滩地区下—中侏罗统层序—古地理及聚煤特征 . 沉积学报, 2020, 38(2): 266-283. doi: 10.14027/j.issn.1000-0550.2019.044
[3]	赵迪斐, 郭英海, WangGeoff, 李冠霖, 曾春林, 焦伟伟. 层序地层格架及其对页岩储层发育特征的影响-以四川盆地龙马溪组页岩为例 . 沉积学报, 2020, 38(2): 379-397. doi: 10.14027/j.issn.1000-0550.2019.043
[4]	刘炳强, 祝铠甲, 黄献好, 陈磊, 刘达成, 邵龙义. 柴西缘阿尔金山前下侏罗统层序地层与岩相古地理研究 . 沉积学报, 2019, 37(2): 356-370. doi: 10.14027/j.issn.1000-0550.2018.130
[5]	. 鄂尔多斯盆地奥陶系层序地层格架 . 沉积学报, 2014, 32(1): 44-60.
[6]	. 西南地区晚二叠世层序—古地理及聚煤特征 . 沉积学报, 2013, 31(05): 856-866.
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[8]	郑荣才. 川东北地区飞仙关组层序—岩相古地理特征和鲕滩预测 . 沉积学报, 2009, 27(1): 1-8.
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[10]	唐洪三. 合肥盆地白垩纪层序地层格架、沉积体系配置及演化 . 沉积学报, 2008, 26(6): 982-993.
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[13]	杨剑萍, 许正豪, 姜在兴, 操应长, 陈发亮. 山东惠民凹陷中央隆起带古近系沙河街组层序地层特征及控制因素研究 . 沉积学报, 2003, 21(4): 670-674.
[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]	沈守文, 彭大钧, 颜其彬, 黄先律, 李志军. 吐哈盆地侏罗系层序地层学研究 . 沉积学报, 2001, 19(2): 263-270.
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[17]	陈国俊, 史基安, 薛莲花, 王琪, 肖立新. 塔里木西部古生代层序地层特征 . 沉积学报, 1999, 17(4): 560-565.
[18]	陈洪德, 覃建雄, 王成善, 寿建峰, 李祥辉. 中国南方二叠纪层序岩相古地理特征及演化 . 沉积学报, 1999, 17(4): 509-520.
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[20]	张海清, 刘本培, 方念乔. 滇西南古特提斯石炭纪海山碳酸盐台地的层序地层学研究 . 沉积学报, 1997, 15(4): 18-23.

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古水深曲线在测井资料层序地层分析中的应用

石油大学地球科学系北京昌平 102200

作者简介:
康安,男,1972年出生,博士研究生,沉积学、层序地层学和盆地分析

收稿日期: 1998-11-03
修回日期: 1999-03-30
刊出日期: 2000-03-10

中图分类号: P539.2

关键词:

测井 /

古水深曲线 /

层序地层

摘要: 层序地层学的精华就是综合应用露头、钻测井和地震资料进行层序地层分析。因此,在缺乏以陆上暴露不整合面为特征的层序界面的湖相沉积中,如何应用测井资料进行层序划分就成为层序地层学研究中一个重要环节。本文以柴达木盆地金达 1井第四系为例,介绍了一种综合利用岩芯、岩屑和电测曲线等测井资料,通过相对古水深曲线的建立,来进行层序地层分析的快速简便的方法。

English Abstract

Application of Paleobathymetric Curve in the Sequence Stratigraphy of Well-logging Data

Geoscience Department, University of Petroleum, Changping Beijing 102200

Received Date: 1998-11-03
Rev Recd Date: 1999-03-30
Publish Date: 2000-03-10

Keywords:

Abstract: It is well known that integrated use of outcrop, well-logging and seismic data is the key to sequence stratigraphy. Therefore, how to identify the sequence boundary by well-logging in the lacustrine sediments which are lack in the unconformity is critical step to sequence stratigraphic analysis. With an example of sequencestratigraphy of Quaternary in well Jinda1, Qaidam basin, this paper presents the basic procedures of new approach for a stratigraphic subdivision of well logs into sequences by reconstruction of paleobathymetric curve. After the log facies analysis, six kinds of lithofacies have been recognized in Quaternary which are dark-grey shale, brown shale, grey silty shale, carbargillite, shaly siltstone and siltstone. For each Lithofacies association a sedimentologically coherent paleoenvironmental interpretation has to be established. Hence, a distinct paleobathymetric range is assigned to each lithofacies unit. Based on this relative paleo-waterdepth, paleobathymetric curve of Quaternary in well Jinda1 has been established from a vertical succession of lithofacies. This water-depth curve helps to identify stratigraphic sequence of different scales.This approach is based on the identification of bathymetry turnaround trends in the lithofacies succession. The maximum regressive surface is placed at the lowest waterdepth values on the smoothed bathymetry curve. The maximum regressive surface is identical to the sequence boundary. The maximum flooding surface is placed at the deepest bathymetry as the closest approximation. This horizon separates underlying transgressive half cycle from overlying regressive half-cycle. Based on the rules above, four sequences are identified in the Quaternary sediment of Jinda1 Well. Each sequence consists of two systems tracts separated by maximum flooding surface. It is clear that there are two scales of waterdepth cycle in the bathymetry curve. More frequent fluctuation in the bathymetry curve can be considered as the response to the high order stratigraphic sequence. At last, the prospective source rock, favorable reservoir and potential caprock have been predicted.

康安, 朱筱敏, 王贵文, 康强. 古水深曲线在测井资料层序地层分析中的应用[J]. 沉积学报, 2000, 18(1): 63-67.

引用本文:

康安, 朱筱敏, 王贵文, 康强. 古水深曲线在测井资料层序地层分析中的应用[J]. 沉积学报, 2000, 18(1): 63-67.

KANG An, ZHU Xiao min, WANG Gui wen, KANG Qiang. Application of Paleobathymetric Curve in the Sequence Stratigraphy of Well-logging Data[J]. Acta Sedimentologica Sinica, 2000, 18(1): 63-67.

Citation:

KANG An, ZHU Xiao min, WANG Gui wen, KANG Qiang. Application of Paleobathymetric Curve in the Sequence Stratigraphy of Well-logging Data[J]. Acta Sedimentologica Sinica, 2000, 18(1): 63-67.

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古水深曲线在测井资料层序地层分析中的应用

作者简介:
康安,男,1972年出生,博士研究生,沉积学、层序地层学和盆地分析

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Application of Paleobathymetric Curve in the Sequence Stratigraphy of Well-logging Data

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古水深曲线在测井资料层序地层分析中的应用

石油大学地球科学系北京昌平 102200

作者简介:
康安,男,1972年出生,博士研究生,沉积学、层序地层学和盆地分析

English Abstract

Application of Paleobathymetric Curve in the Sequence Stratigraphy of Well-logging Data

Geoscience Department, University of Petroleum, Changping Beijing 102200

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古水深曲线在测井资料层序地层分析中的应用

作者简介: 康安,男,1972年出生,博士研究生,沉积学、层序地层学和盆地分析

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Application of Paleobathymetric Curve in the Sequence Stratigraphy of Well-logging Data

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古水深曲线在测井资料层序地层分析中的应用

石油大学地球科学系 北京昌平 102200

作者简介: 康安,男,1972年出生,博士研究生,沉积学、层序地层学和盆地分析

English Abstract

Application of Paleobathymetric Curve in the Sequence Stratigraphy of Well-logging Data

Geoscience Department, University of Petroleum, Changping Beijing 102200

全文HTML

目录

友情链接

期刊在线

联系我们

作者简介:
康安,男,1972年出生,博士研究生,沉积学、层序地层学和盆地分析

石油大学地球科学系北京昌平 102200

作者简介:
康安,男,1972年出生,博士研究生,沉积学、层序地层学和盆地分析