有机相研究及其在盆地分析中的应用

郝芳; 陈建渝; 孙永传; 解习农

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有机相研究及其在盆地分析中的应用

郝芳, 陈建渝, 孙永传, 解习农

文章导航 > 沉积学报 > 1994 > 12(4): 77-86

郝芳, 陈建渝, 孙永传, 解习农. 有机相研究及其在盆地分析中的应用[J]. 沉积学报, 1994, 12(4): 77-86.

引用本文:

郝芳, 陈建渝, 孙永传, 解习农. 有机相研究及其在盆地分析中的应用[J]. 沉积学报, 1994, 12(4): 77-86.

Hao Fang, Chen Jianyu, Sun Yongchuan, Xie Xinong. Organic Facies Studies and Their Use in Sedimentary Basin Analysis[J]. Acta Sedimentologica Sinica, 1994, 12(4): 77-86.

Citation:

Hao Fang, Chen Jianyu, Sun Yongchuan, Xie Xinong. Organic Facies Studies and Their Use in Sedimentary Basin Analysis[J]. Acta Sedimentologica Sinica, 1994, 12(4): 77-86.

郝芳, 陈建渝, 孙永传, 解习农. 有机相研究及其在盆地分析中的应用[J]. 沉积学报, 1994, 12(4): 77-86.

引用本文:

郝芳, 陈建渝, 孙永传, 解习农. 有机相研究及其在盆地分析中的应用[J]. 沉积学报, 1994, 12(4): 77-86.

Hao Fang, Chen Jianyu, Sun Yongchuan, Xie Xinong. Organic Facies Studies and Their Use in Sedimentary Basin Analysis[J]. Acta Sedimentologica Sinica, 1994, 12(4): 77-86.

Citation:

Hao Fang, Chen Jianyu, Sun Yongchuan, Xie Xinong. Organic Facies Studies and Their Use in Sedimentary Basin Analysis[J]. Acta Sedimentologica Sinica, 1994, 12(4): 77-86.

有机相研究及其在盆地分析中的应用

中国地质大学

详细信息

作者简介:
郝芳男 28岁讲师有机地球化学和沉积学

中图分类号: P618.130.2

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文章访问数: 583
HTML全文浏览量: 10
PDF下载量: 515
被引次数: 0

Organic Facies Studies and Their Use in Sedimentary Basin Analysis

China University of Geosciences, Wuhan 430074

摘要

摘要: 有机相是具有一定丰度和特定成因类型的有机质的地层单元，决定有机相类型的最重要参数是干酪根的成因类型。为了反映沉积盆地中有机相的时空分布，我们提出了有机相组合和盆地有机充填序列等新概念。有机相及有机相层序、有机充填序列和有机相组合不仅是预测和在三维空间确定生油岩的分布、预测主力生油岩的排烃期和排出产物的组成的有效工具，而且可以弥补以骨架砂岩体为主要研究对象的沉积学分析的不足，在确定层序界线或不整合面的位且、研究盆地的构造沉降和沉积充填史等方面发挥重要作用。
- 有机相 /
- 有机相层序和有机相组合 /
- 盆地有机充填序列 /
- 盆地分析
Abstract: An organic facies is defined as a mappable stratigraphic unit containing organic matter (OM)of a particular genetic type in cartaain abundance. A new organic facies classification，which is based on indicative genetic kerogen(OM)type。is proposed. The improved definition and classification makes organic facies capable of reflecting the origin，diagenetic alternation of organic matter comprehensively, and，the organic facies thus defined and classified，which must be identified on the basis of synthetical parameters other than by atomic H/C ratios and/or Rock-Eval Hydrogen Index values merely. Several new concepts concerning organic facies such as Vertical Organic Facies Sequence ( VOFS )，Organic Facies Association ( OFA ) and Organic Basin-fill Sequence ( OBFS ) are advanced, and their significance in basin analysis is discussed in detail.Several cases are presented in this paper which confirm that organic facies, especially VOFS，OFA and OBFS analysis can not only become a very usefull tool for prediction and three-dimensional mapping of petroleum source rocks, but also make up for some shortcomings of sedimentological studies that put the stress on coarse rocks, and therefore may play a distinctive role in identifying and accurately locating unconformities or sequence/ systems tract boundaries as well as in reconstructing the tectonic subsidence and sedimentary fill histories of sedimentary basins.
- Organic facies /
- Organic facies sequence and association /
- Organic basin-fill sequence /
- Basin analysis

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参考文献(12)

[1]	黄第落，李晋超,1984.陆相有机质演化和成烃机理，北京:石油工业出版社。
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[4]	郝芳，陈建渝,1993，论有机质生烃潜能与生像的关系及干酪根的成因类型.现代地质，(1):57~65.
[5]	那芳，陈建渝.1994，沉积盆地的有机相研究及其在油气资探评价中的应用，矿物学岩石学论丛(9)，地质出版社，101-109,
[6]	Demaison G. J. et al.，1983, Predictive source bed stratigraphy, a guide to regional petroleum occurtence. In Proc. of Eleventh World Petroleum Congress, 2.17~29.
[7]	DemaL9on G. J. and Moore G.. T.，1980. Anoxic environments and oil source bed genesis. Organic Geochemistry 2. 9~31.
[8]	liao Fang and Chen Jianyu, 1992, The cause and mechanism of vitrinite reflectance anomalies. Journal of Petroleum Geology15(4);419~434.
[9]	Hao Fang. Chen Jianyu, Sun Yongchuan and Liu Yiao2hong, 1993, Application of organic fades studies to sedimentary basin analysis, a case study from the Yitong Graben ,China.Org.Geochem.20(1);27~42.
[10]	Jones R. W.，1989. Comparison of carbonate and shale source racks. In Petroleum Geochemistry and Source Rock Potential of Carbonate Rocks(Fdited by Palaces J. G.),AAPG Studies in Geology 18. 163~180.
[11]	Jones R. W.，1987. Organic Fades, In Advances in Petroleum Geochemistry I (Edited by Brooks J. and Welte D.)，1~90.
[12]	Veil P. R.，1987 , Seismic stratigraphy interpretation using sequence stratigraphy. Part 1; seismic stratigraphy interpretation procedure. In Atlas of Seismic Stratigraphy, Vol. 1(Edited by Belly A. W.)，AAPG Studies in Geology. 27, 1~10.

[1]	肖颖. 陆相富有机质页岩纹层特征及其储集性能 ——以鄂尔多斯盆地东南部延长组长7段为例 . 沉积学报, 2024, (): -. doi: 10.14027/j.issn.1000-0550.2024.071
[2]	于乐丹, 彭军, 许天宇, 韩浩东, 杨一茗. 陆相断陷咸化湖盆细粒沉积地层有机质富集特征及控制因素分析 . 沉积学报, 2024, 42(2): 701-722. doi: 10.14027/j.issn.1000-0550.2022.096
[3]	刘翰林, 邹才能, 邱振, 尹帅, 杨智, 吴松涛, 张国生, 陈艳鹏, 马锋, 李士祥, 张岩. 陆相黑色页岩沉积环境及有机质富集机制 . 沉积学报, 2023, 41(6): 1810-1829. doi: 10.14027/j.issn.1000-0550.2023.118
[4]	徐明慧, 王峰, 田景春, 余威, 王集, 吴静仪, 肖云宵. 湖相富有机质泥页岩岩相划分及沉积环境-以鄂尔多斯盆地长73亚段为例 . 沉积学报, 2023, (): -. doi: 10.14027/j.issn.1000-0550.2023.076
[5]	张慧芳, 吴欣松, 王斌, 段云江, 屈洋, 陈德飞. 陆相湖盆沉积有机质富集机理研究进展 . 沉积学报, 2016, 34(3): 463-477. doi: 10.14027/j.cnki.cjxb.2016.03.004
[6]	. 成熟度对陆相烃源岩可溶有机质Pr/Ph比值的影响 . 沉积学报, 2014, 32(1): 182-188.
[7]	. 合肥盆地烃源岩有机质热演化历史分析 . 沉积学报, 2008, 26(1): 168-177.
[8]	乔海明. 吐哈盆地十红滩铀矿床有机地球化学特征浅析 . 沉积学报, 2007, 25(1): 154-160.
[9]	姚素平, 胡文, 薛春燕, 张景荣, 曹剑. 瓦窑堡煤系有机岩石学特征及煤成烃潜力研究 . 沉积学报, 2004, 22(3): 518-524.
[10]	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.
[11]	杨建业, 任德贻, 邵龙义. 沉积有机相在陆相层序地层格架中的分布特征——以吐哈盆地台北凹陷及准噶尔盆地南缘中侏罗世煤系为例 . 沉积学报, 2000, 18(4): 585-589.
[12]	朱创业. 陕甘宁盆地下奥陶统马家沟组层序沉积有机相特征及其烃源岩分布 . 沉积学报, 2000, 18(1): 57-62.
[13]	杨明慧, 夏文臣, 张兵山, 张宁, 彭晓群. 非海相盆地准层序级别的有机相变化及其地质意义 . 沉积学报, 2000, 18(2): 297-301.
[14]	陈洪德, 王成善, 刘文均, 覃建雄. 华南二叠纪层序地层与盆地演化 . 沉积学报, 1999, 17(4): 528-535.
[15]	夏新宇, 洪峰, 赵林, 张文正. 鄂尔多斯盆地下奥陶统碳酸盐岩有机相类型及生烃潜力 . 沉积学报, 1999, 17(4): 638-643.
[16]	庄汉平, 冉祟英, 何明勤, 卢家烂, 刘金钟. 楚雄盆地有机质、膏盐与砂岩铜矿生成关系的有机地球化学证据与机理 . 沉积学报, 1996, 14(3): 129-138.
[17]	张柏生, 刘文汇, 徐永昌, 王兆云, 吴铁生. 辽河盆地过渡带有机地球化学（Ⅰ）──不同赋存状态的有机质与过渡带气的形成 . 沉积学报, 1994, 12(4): 58-65.
[18]	杨瑞东. 黔中、黔南下、中三叠统沉积相和层序地层 . 沉积学报, 1993, 11(4): 24-29.
[19]	李思田. 论沉积盆地分析领域的追踪与创新 . 沉积学报, 1992, 10(3): 10-15.
[20]	梁仁枝, 李汉瑜, 刘宝珺, 许效松. 湘西黔东下、中寒武统沉积环境 . 沉积学报, 1991, 9(2): 16-24.

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有机相研究及其在盆地分析中的应用

中国地质大学

作者简介:
郝芳男 28岁讲师有机地球化学和沉积学

收稿日期: 1993-06-20
刊出日期: 1994-12-10

中图分类号: P618.130.2

关键词:

有机相 /

有机相层序和有机相组合 /

盆地有机充填序列 /

盆地分析

摘要: 有机相是具有一定丰度和特定成因类型的有机质的地层单元，决定有机相类型的最重要参数是干酪根的成因类型。为了反映沉积盆地中有机相的时空分布，我们提出了有机相组合和盆地有机充填序列等新概念。有机相及有机相层序、有机充填序列和有机相组合不仅是预测和在三维空间确定生油岩的分布、预测主力生油岩的排烃期和排出产物的组成的有效工具，而且可以弥补以骨架砂岩体为主要研究对象的沉积学分析的不足，在确定层序界线或不整合面的位且、研究盆地的构造沉降和沉积充填史等方面发挥重要作用。

English Abstract

Organic Facies Studies and Their Use in Sedimentary Basin Analysis

China University of Geosciences, Wuhan 430074

Received Date: 1993-06-20
Publish Date: 1994-12-10

Keywords:

Organic facies /
Organic facies sequence and association /
Organic basin-fill sequence /
Basin analysis

Abstract: An organic facies is defined as a mappable stratigraphic unit containing organic matter (OM)of a particular genetic type in cartaain abundance. A new organic facies classification，which is based on indicative genetic kerogen(OM)type。is proposed. The improved definition and classification makes organic facies capable of reflecting the origin，diagenetic alternation of organic matter comprehensively, and，the organic facies thus defined and classified，which must be identified on the basis of synthetical parameters other than by atomic H/C ratios and/or Rock-Eval Hydrogen Index values merely. Several new concepts concerning organic facies such as Vertical Organic Facies Sequence ( VOFS )，Organic Facies Association ( OFA ) and Organic Basin-fill Sequence ( OBFS ) are advanced, and their significance in basin analysis is discussed in detail.Several cases are presented in this paper which confirm that organic facies, especially VOFS，OFA and OBFS analysis can not only become a very usefull tool for prediction and three-dimensional mapping of petroleum source rocks, but also make up for some shortcomings of sedimentological studies that put the stress on coarse rocks, and therefore may play a distinctive role in identifying and accurately locating unconformities or sequence/ systems tract boundaries as well as in reconstructing the tectonic subsidence and sedimentary fill histories of sedimentary basins.

郝芳, 陈建渝, 孙永传, 解习农. 有机相研究及其在盆地分析中的应用[J]. 沉积学报, 1994, 12(4): 77-86.

引用本文:

郝芳, 陈建渝, 孙永传, 解习农. 有机相研究及其在盆地分析中的应用[J]. 沉积学报, 1994, 12(4): 77-86.

Hao Fang, Chen Jianyu, Sun Yongchuan, Xie Xinong. Organic Facies Studies and Their Use in Sedimentary Basin Analysis[J]. Acta Sedimentologica Sinica, 1994, 12(4): 77-86.

Citation:

Hao Fang, Chen Jianyu, Sun Yongchuan, Xie Xinong. Organic Facies Studies and Their Use in Sedimentary Basin Analysis[J]. Acta Sedimentologica Sinica, 1994, 12(4): 77-86.

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有机相研究及其在盆地分析中的应用

作者简介:
郝芳男 28岁讲师有机地球化学和沉积学

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Organic Facies Studies and Their Use in Sedimentary Basin Analysis

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有机相研究及其在盆地分析中的应用

中国地质大学

作者简介:
郝芳男 28岁讲师有机地球化学和沉积学

English Abstract

Organic Facies Studies and Their Use in Sedimentary Basin Analysis

China University of Geosciences, Wuhan 430074

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有机相研究及其在盆地分析中的应用

作者简介: 郝芳 男 28岁 讲师 有机地球化学和沉积学

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Organic Facies Studies and Their Use in Sedimentary Basin Analysis

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出版历程

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有机相研究及其在盆地分析中的应用

中国地质大学

作者简介: 郝芳 男 28岁 讲师 有机地球化学和沉积学

English Abstract

Organic Facies Studies and Their Use in Sedimentary Basin Analysis

China University of Geosciences, Wuhan 430074

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目录

友情链接

期刊在线

联系我们

作者简介:
郝芳男 28岁讲师有机地球化学和沉积学

作者简介:
郝芳男 28岁讲师有机地球化学和沉积学