一种特殊瘤状灰岩的成因研究

董兆雄; 朱晓惠; 侯方浩; 方少仙; 吴诒

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一种特殊瘤状灰岩的成因研究

董兆雄, 朱晓惠, 侯方浩, 方少仙, 吴诒

文章导航 > 沉积学报 > 2002 > 20(1): 20-24

董兆雄, 朱晓惠, 侯方浩, 方少仙, 吴诒. 一种特殊瘤状灰岩的成因研究[J]. 沉积学报, 2002, 20(1): 20-24.

引用本文:

董兆雄, 朱晓惠, 侯方浩, 方少仙, 吴诒. 一种特殊瘤状灰岩的成因研究[J]. 沉积学报, 2002, 20(1): 20-24.

DONG Zhao-xiong, ZHU Xiao-hui, FANG Shao-xian, HOU Fang-hao, WU Yi. Study on Origin of Special Nodular Limestone[J]. Acta Sedimentologica Sinica, 2002, 20(1): 20-24.

Citation:

DONG Zhao-xiong, ZHU Xiao-hui, FANG Shao-xian, HOU Fang-hao, WU Yi. Study on Origin of Special Nodular Limestone[J]. Acta Sedimentologica Sinica, 2002, 20(1): 20-24.

董兆雄, 朱晓惠, 侯方浩, 方少仙, 吴诒. 一种特殊瘤状灰岩的成因研究[J]. 沉积学报, 2002, 20(1): 20-24.

引用本文:

董兆雄, 朱晓惠, 侯方浩, 方少仙, 吴诒. 一种特殊瘤状灰岩的成因研究[J]. 沉积学报, 2002, 20(1): 20-24.

DONG Zhao-xiong, ZHU Xiao-hui, FANG Shao-xian, HOU Fang-hao, WU Yi. Study on Origin of Special Nodular Limestone[J]. Acta Sedimentologica Sinica, 2002, 20(1): 20-24.

Citation:

DONG Zhao-xiong, ZHU Xiao-hui, FANG Shao-xian, HOU Fang-hao, WU Yi. Study on Origin of Special Nodular Limestone[J]. Acta Sedimentologica Sinica, 2002, 20(1): 20-24.

一种特殊瘤状灰岩的成因研究

1 西南石油学院,四川南充,637001;
2 四川石油管理局川南矿区,四川泸洲,646001;
3 广西地质研究所,南宁,530023

详细信息

作者简介:
董兆雄男 1954年出生副教授沉积学与储层地质学

中图分类号: P588.24⁺5

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文章访问数: 478
HTML全文浏览量: 1
PDF下载量: 337
被引次数: 0

Study on Origin of Special Nodular Limestone

1 Southwest Petroleum Institute,Nanchong Sichuan 637001;
2 South Sichuan Mining District of Sichuan Petroleum Administration,Luzhou Sichuan 646001;
3 Guangxi Insiti of Geology and Mineral Resources, Nanning 530023

摘要

摘要: 关于瘤状灰岩的成因主要有三种观点,其中一种认为与碳酸盐结核有关,另一种则认为是差异压实所为,再一种则认为是同沉积作用形成。然而,广西德保县都安下泥盆统达莲塘组发育的一种特殊的瘤状灰岩却因其产状貌似通常意义的砾状灰岩而使得人们将其误认为砾状灰岩。作者通过对这套“砾状灰岩”的沉积岩石学、生物化石、古构造等特征的研究,发现该“砾状灰岩”既不是沉积作用形成,也非同沉积构造作用形成,而是首先在闭塞的台内洼槽环境中形成同生和成岩碳酸盐结核,然后差异压实作用导致地层表面强烈地凹凸不平或地层整体的不均匀性 (致使强度降低 ),最后在印支期的穹隆形成过程中由于翼部的剪切、弯滑、弯流作用,致使结核发生转动、移动而形成今天所见的“砾状灰岩”。因此都安“砾状灰岩”实为瘤状灰岩,它代表的是闭塞、贫氧的 (台内洼槽 )沉积—成岩环境,是沉积成岩和构造等多种因素共同作用的产物。
- 瘤状灰岩 /
- 砾状灰岩 /
- 成因 /
- 碳酸盐结核 /
- 差异压实 /
- 褶皱作用 /
- 广西德保都安
Abstract: There are three interpretations for the cause of formation of nodular limestones.The first interpretation is that they are the beds of carbonate concretions, the second is that they are the result of the differential compaction,and the third is that they are formed by the sedimentation or the synsedimentary faulting.However, in the Da Liang Tang Formating of lower Devenian Series in Du-an,Debao county,Guangxi,a special nodular limestone is mistaken as a rudstone by some people,because the nodular limstone similar to the normal rudstones in its figure and mode of occurrence. The study on its petrology,paleontology,paleostructurs,etc., shows that the rudstone is not simply the beds of carbonate concretions, it was formed neither by the differential compaction nor by the sedimentation and synsedimentary faulting,and the fact is that lot of carbonate nodules were first formed in the poor-oxygen,closed flute facies of shelf platform;then,the differential compaction led to the extremely concave-convex of the bedding surface or the heterogeneity of the beds; finally,the nodules were turned and also transferred by the shearing,flexural slip,flexural flow, process of the limb during forming the dome in the Indo-Chinese epoch, the "rudstone" we see today was produced. Hence,the "rudstone" in Du-an was realy the nodular limstone,and it was the result of sedimentationg,diagenesis and tectonism,etc,and it also shows a kind of sedimentary-diagenetic environment which was the poor-oxygen and closed flute of shelf platform.
- nodular limestone /
- rudstone carbonate concretion /
- differential compaction /
- Du-an /
- Debao County /
- Guangxi /

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参考文献(7)

[1]	王英华,张秀莲等.华北地台早古生代碳酸盐岩岩石学[J].北京:地质出版社,1988.7
[2]	侯方浩等.西南地区上古生界海相碳酸盐岩沉积相模式及其在油气勘探中的应用[M].成都:成都科技大学出版社1991.9
[3]	H J 里丁著,周明鉴等译.沉积环境和相[M].北京:科学出版社,1985.471
[4]	端木合顺.陕西凤县-山阳泥盆系同沉积断裂砾岩[J].古地理学报,2000,3:97
[5]	鲜思远.华南泥盆纪埃姆斯期腕足类、双壳类群落、竹节石生物相及生态地层[J].岩相古地理,1992.3:55
[6]	刘宝王君.沉积岩石学[M].北京:地质出版社,1980,75～76
[7]	Moller,N K,Vingan K K.The genesis of nodular limestones in the Ordovician and Silurian of the Oslo Region (Norway)[J].Sedimentology.1988,35:417

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[14]	夏燕青, 孟仟祥, 王红勇, 王春江, 杜丽. 芴系列化合物的成因 . 沉积学报, 1999, 17(4): 655-658.
[15]	孙玉善, 杨帆. 再论东河砂岩孔隙成因──以塔中地区为例 . 沉积学报, 1999, 17(S1): 699-705.
[16]	金振奎, 冯增昭. 滇东—川西下二叠统白云岩的形成机理——玄武岩淋滤白云化 . 沉积学报, 1999, 17(3): 383-389.
[17]	谢晓安, 王仁德, 李光文, 卢华复. 塔里木盆地满加尔南切割谷的成因探讨与石油地质意义浅析 . 沉积学报, 1996, 14(2): 41-46.
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一种特殊瘤状灰岩的成因研究

1 西南石油学院,四川南充,637001;

2 四川石油管理局川南矿区,四川泸洲,646001;

3 广西地质研究所,南宁,530023

作者简介:
董兆雄男 1954年出生副教授沉积学与储层地质学

收稿日期: 2001-03-28

中图分类号: P588.24⁺5

关键词:

成因 /

摘要: 关于瘤状灰岩的成因主要有三种观点,其中一种认为与碳酸盐结核有关,另一种则认为是差异压实所为,再一种则认为是同沉积作用形成。然而,广西德保县都安下泥盆统达莲塘组发育的一种特殊的瘤状灰岩却因其产状貌似通常意义的砾状灰岩而使得人们将其误认为砾状灰岩。作者通过对这套“砾状灰岩”的沉积岩石学、生物化石、古构造等特征的研究,发现该“砾状灰岩”既不是沉积作用形成,也非同沉积构造作用形成,而是首先在闭塞的台内洼槽环境中形成同生和成岩碳酸盐结核,然后差异压实作用导致地层表面强烈地凹凸不平或地层整体的不均匀性 (致使强度降低 ),最后在印支期的穹隆形成过程中由于翼部的剪切、弯滑、弯流作用,致使结核发生转动、移动而形成今天所见的“砾状灰岩”。因此都安“砾状灰岩”实为瘤状灰岩,它代表的是闭塞、贫氧的 (台内洼槽 )沉积—成岩环境,是沉积成岩和构造等多种因素共同作用的产物。

English Abstract

Study on Origin of Special Nodular Limestone

1 Southwest Petroleum Institute,Nanchong Sichuan 637001;

2 South Sichuan Mining District of Sichuan Petroleum Administration,Luzhou Sichuan 646001;

3 Guangxi Insiti of Geology and Mineral Resources, Nanning 530023

Received Date: 2001-03-28

Keywords:

Abstract: There are three interpretations for the cause of formation of nodular limestones.The first interpretation is that they are the beds of carbonate concretions, the second is that they are the result of the differential compaction,and the third is that they are formed by the sedimentation or the synsedimentary faulting.However, in the Da Liang Tang Formating of lower Devenian Series in Du-an,Debao county,Guangxi,a special nodular limestone is mistaken as a rudstone by some people,because the nodular limstone similar to the normal rudstones in its figure and mode of occurrence. The study on its petrology,paleontology,paleostructurs,etc., shows that the rudstone is not simply the beds of carbonate concretions, it was formed neither by the differential compaction nor by the sedimentation and synsedimentary faulting,and the fact is that lot of carbonate nodules were first formed in the poor-oxygen,closed flute facies of shelf platform;then,the differential compaction led to the extremely concave-convex of the bedding surface or the heterogeneity of the beds; finally,the nodules were turned and also transferred by the shearing,flexural slip,flexural flow, process of the limb during forming the dome in the Indo-Chinese epoch, the "rudstone" we see today was produced. Hence,the "rudstone" in Du-an was realy the nodular limstone,and it was the result of sedimentationg,diagenesis and tectonism,etc,and it also shows a kind of sedimentary-diagenetic environment which was the poor-oxygen and closed flute of shelf platform.

董兆雄, 朱晓惠, 侯方浩, 方少仙, 吴诒. 一种特殊瘤状灰岩的成因研究[J]. 沉积学报, 2002, 20(1): 20-24.

引用本文:

董兆雄, 朱晓惠, 侯方浩, 方少仙, 吴诒. 一种特殊瘤状灰岩的成因研究[J]. 沉积学报, 2002, 20(1): 20-24.

DONG Zhao-xiong, ZHU Xiao-hui, FANG Shao-xian, HOU Fang-hao, WU Yi. Study on Origin of Special Nodular Limestone[J]. Acta Sedimentologica Sinica, 2002, 20(1): 20-24.

Citation:

DONG Zhao-xiong, ZHU Xiao-hui, FANG Shao-xian, HOU Fang-hao, WU Yi. Study on Origin of Special Nodular Limestone[J]. Acta Sedimentologica Sinica, 2002, 20(1): 20-24.

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一种特殊瘤状灰岩的成因研究

作者简介:
董兆雄男 1954年出生副教授沉积学与储层地质学

计量

Study on Origin of Special Nodular Limestone

计量

目录

一种特殊瘤状灰岩的成因研究

1 西南石油学院,四川南充,637001;

2 四川石油管理局川南矿区,四川泸洲,646001;

3 广西地质研究所,南宁,530023

作者简介:
董兆雄男 1954年出生副教授沉积学与储层地质学

English Abstract

Study on Origin of Special Nodular Limestone

1 Southwest Petroleum Institute,Nanchong Sichuan 637001;

2 South Sichuan Mining District of Sichuan Petroleum Administration,Luzhou Sichuan 646001;

3 Guangxi Insiti of Geology and Mineral Resources, Nanning 530023

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一种特殊瘤状灰岩的成因研究

作者简介: 董兆雄 男 1954年出生 副教授 沉积学与储层地质学

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Study on Origin of Special Nodular Limestone

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出版历程

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一种特殊瘤状灰岩的成因研究

1 西南石油学院,四川南充,637001; 2 四川石油管理局川南矿区,四川泸洲,646001; 3 广西地质研究所,南宁,530023

作者简介: 董兆雄 男 1954年出生 副教授 沉积学与储层地质学

English Abstract

Study on Origin of Special Nodular Limestone

1 Southwest Petroleum Institute,Nanchong Sichuan 637001; 2 South Sichuan Mining District of Sichuan Petroleum Administration,Luzhou Sichuan 646001; 3 Guangxi Insiti of Geology and Mineral Resources, Nanning 530023

全文HTML

目录

友情链接

期刊在线

联系我们

作者简介:
董兆雄男 1954年出生副教授沉积学与储层地质学

1 西南石油学院,四川南充,637001;

2 四川石油管理局川南矿区,四川泸洲,646001;

3 广西地质研究所,南宁,530023

作者简介:
董兆雄男 1954年出生副教授沉积学与储层地质学

1 Southwest Petroleum Institute,Nanchong Sichuan 637001;

2 South Sichuan Mining District of Sichuan Petroleum Administration,Luzhou Sichuan 646001;

3 Guangxi Insiti of Geology and Mineral Resources, Nanning 530023