淮南煤田二叠系三、四含煤段古水系特征

彭苏萍; 韩德馨; 张鹏飞; 蓝昌益

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淮南煤田二叠系三、四含煤段古水系特征

彭苏萍, 韩德馨, 张鹏飞, 蓝昌益

文章导航 > 沉积学报 > 1991 > 9(3): 1-10

彭苏萍, 韩德馨, 张鹏飞, 蓝昌益. 淮南煤田二叠系三、四含煤段古水系特征[J]. 沉积学报, 1991, 9(3): 1-10.

引用本文:

彭苏萍, 韩德馨, 张鹏飞, 蓝昌益. 淮南煤田二叠系三、四含煤段古水系特征[J]. 沉积学报, 1991, 9(3): 1-10.

Peng Suping, Han Dexin, Zhang Pengfei, Lan Changyi. Paleodrainage Characteristics of the Permian Members C and D in Huainan Coalfield, China[J]. Acta Sedimentologica Sinica, 1991, 9(3): 1-10.

Citation:

Peng Suping, Han Dexin, Zhang Pengfei, Lan Changyi. Paleodrainage Characteristics of the Permian Members C and D in Huainan Coalfield, China[J]. Acta Sedimentologica Sinica, 1991, 9(3): 1-10.

彭苏萍, 韩德馨, 张鹏飞, 蓝昌益. 淮南煤田二叠系三、四含煤段古水系特征[J]. 沉积学报, 1991, 9(3): 1-10.

引用本文:

彭苏萍, 韩德馨, 张鹏飞, 蓝昌益. 淮南煤田二叠系三、四含煤段古水系特征[J]. 沉积学报, 1991, 9(3): 1-10.

Peng Suping, Han Dexin, Zhang Pengfei, Lan Changyi. Paleodrainage Characteristics of the Permian Members C and D in Huainan Coalfield, China[J]. Acta Sedimentologica Sinica, 1991, 9(3): 1-10.

Citation:

Peng Suping, Han Dexin, Zhang Pengfei, Lan Changyi. Paleodrainage Characteristics of the Permian Members C and D in Huainan Coalfield, China[J]. Acta Sedimentologica Sinica, 1991, 9(3): 1-10.

淮南煤田二叠系三、四含煤段古水系特征

1.
中国矿业大学北京研究生部;
2.
淮南矿业学院

基金项目: 国家青年科学基金

详细信息

作者简介:
彭苏萍,男,30岁,博士,煤田地质学及比较沉积学.

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文章访问数: 710
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被引次数: 0

Paleodrainage Characteristics of the Permian Members C and D in Huainan Coalfield, China

1.
Beijing Graduate School, China University of Mining and Technology;
2.
Huainan Mining Institute

摘要

摘要: 本文通过对淮南煤田二叠系三、四含煤段5千余个钻孔资料的系统分析和煤矿开拓巷道中古流向的实际测量,获得大量有关古水系的第-性资料。研究认为可与现代珠江三角洲上的水系进行类比、进而推断三、四含煤段沉积时的环境为-种由多条陆源河流共同作用形成的复合型三角洲。
- 古水系 /
- 复合型三角洲 /
- 树技状河系 /
- 网状河系
Abstract: The Huainan Coalfield, covering an area of more than 8000 km₂. is concealed by the Quaternary system and the main coal-bearing strata are Permian Members C-D. By the investigation of more than 5000 bores and surveying of undergroud tunnels of the coal mines in the research district, many characteristics of the paleodrainage have been acquired as follows: 1. By undergroud surveying of the main channel sandstones of the members C-D, it is shown that during their deposition the paleocurrent direction is southward. 2.The paleodrainage of the Permian members C-D have two forms, the branched channel system (in member C) and the anastomosing channel system (in member D). The channels composed the drainages are very stable and fail to lateral migration. 3. The results of grainsize analysis and the C-M pattern of the same genetic increment demonstrates that the paleostream flown from north to south, and the south side is more near to the sea. 4. The characteristics of sedimentology and sedimentary geochemistry indicate that the t;ne sediments of member C which deposited in the branched channel system contain much more of the tidal sediments, bur- rows, and Lingula sp. etc. The content of the trace element B. B; Ga and Ca (Fe+Ca) are higher than that of member D To sum up the characteristics discussed above and analyze by means of Walther's Law of correlation of fades. and compare with the drainage on the modern Pearl River, the authers propose that the paleodrainage of the members C-D is more similar to that on the modern Pearl River Delta, that is to say, it can be divided into two parts, the anastomosing fluvial system near the continent and the branched fluvial system close to the sea. It is recognized that the paleodrainage discussed m this paper is different from that on the Mississippi River Delta and’or on the Yangtze River Delta. that could he account for which discussed' in this p:ner is a complex delta formed together by several continental streams, the low-medium thal range and the Coriolis Force exist in the history of the Earth.

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参考文献(1)

[1]

1. 黄镇国、李平日等，1982，珠江三角洲形成发育演变，科学普及出版社广州分社.

2. 彭苏萍，1989,科学通报，34卷，17期，1326-1328页.

3. Sorby, H.C., 1859, The Geologist。Vol.2, p.137-147

4. Sorby. H.C., 1879, Quart.J.GeoLSoc., London, Vo1.35, p.56-77.

5. Potter, P. E.&Pettijohn. F. J.，1977. Paleocurrents and basin analysis〔second, corrected and updatededition )，Springer-Verlag.

6. Martin, R., 1966, AAPG Bull., Vo1.50, IVo.10, p.2277-2311.

7. Daniel A.Busch, 1974, Stratigraphic traps m sandstone-exploration techniques, The American Association of Petroleum Geologists Tulsa. Oklahoma. U.S.A

8. Matthews, R.K., 1984, Dynamic Stratigraphy(second edition) DrenOCe-Hall, Inc，Englewood Cliffs. New Jersey，07632.

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淮南煤田二叠系三、四含煤段古水系特征

1. 中国矿业大学北京研究生部;

2. 淮南矿业学院

基金项目: 国家青年科学基金

作者简介:
彭苏萍,男,30岁,博士,煤田地质学及比较沉积学.

收稿日期: 1989-08-10
刊出日期: 1991-09-10

关键词:

古水系 /

复合型三角洲 /

树技状河系 /

网状河系

摘要: 本文通过对淮南煤田二叠系三、四含煤段5千余个钻孔资料的系统分析和煤矿开拓巷道中古流向的实际测量,获得大量有关古水系的第-性资料。研究认为可与现代珠江三角洲上的水系进行类比、进而推断三、四含煤段沉积时的环境为-种由多条陆源河流共同作用形成的复合型三角洲。

English Abstract

Paleodrainage Characteristics of the Permian Members C and D in Huainan Coalfield, China

1. Beijing Graduate School, China University of Mining and Technology;

2. Huainan Mining Institute

Received Date: 1989-08-10
Publish Date: 1991-09-10

Abstract: The Huainan Coalfield, covering an area of more than 8000 km₂. is concealed by the Quaternary system and the main coal-bearing strata are Permian Members C-D. By the investigation of more than 5000 bores and surveying of undergroud tunnels of the coal mines in the research district, many characteristics of the paleodrainage have been acquired as follows: 1. By undergroud surveying of the main channel sandstones of the members C-D, it is shown that during their deposition the paleocurrent direction is southward. 2.The paleodrainage of the Permian members C-D have two forms, the branched channel system (in member C) and the anastomosing channel system (in member D). The channels composed the drainages are very stable and fail to lateral migration. 3. The results of grainsize analysis and the C-M pattern of the same genetic increment demonstrates that the paleostream flown from north to south, and the south side is more near to the sea. 4. The characteristics of sedimentology and sedimentary geochemistry indicate that the t;ne sediments of member C which deposited in the branched channel system contain much more of the tidal sediments, bur- rows, and Lingula sp. etc. The content of the trace element B. B; Ga and Ca (Fe+Ca) are higher than that of member D To sum up the characteristics discussed above and analyze by means of Walther's Law of correlation of fades. and compare with the drainage on the modern Pearl River, the authers propose that the paleodrainage of the members C-D is more similar to that on the modern Pearl River Delta, that is to say, it can be divided into two parts, the anastomosing fluvial system near the continent and the branched fluvial system close to the sea. It is recognized that the paleodrainage discussed m this paper is different from that on the Mississippi River Delta and’or on the Yangtze River Delta. that could he account for which discussed' in this p:ner is a complex delta formed together by several continental streams, the low-medium thal range and the Coriolis Force exist in the history of the Earth.

彭苏萍, 韩德馨, 张鹏飞, 蓝昌益. 淮南煤田二叠系三、四含煤段古水系特征[J]. 沉积学报, 1991, 9(3): 1-10.

引用本文:

彭苏萍, 韩德馨, 张鹏飞, 蓝昌益. 淮南煤田二叠系三、四含煤段古水系特征[J]. 沉积学报, 1991, 9(3): 1-10.

Peng Suping, Han Dexin, Zhang Pengfei, Lan Changyi. Paleodrainage Characteristics of the Permian Members C and D in Huainan Coalfield, China[J]. Acta Sedimentologica Sinica, 1991, 9(3): 1-10.

Citation:

Peng Suping, Han Dexin, Zhang Pengfei, Lan Changyi. Paleodrainage Characteristics of the Permian Members C and D in Huainan Coalfield, China[J]. Acta Sedimentologica Sinica, 1991, 9(3): 1-10.

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淮南煤田二叠系三、四含煤段古水系特征

作者简介:
彭苏萍,男,30岁,博士,煤田地质学及比较沉积学.

计量

Paleodrainage Characteristics of the Permian Members C and D in Huainan Coalfield, China

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目录

淮南煤田二叠系三、四含煤段古水系特征

1. 中国矿业大学北京研究生部;

2. 淮南矿业学院

作者简介:
彭苏萍,男,30岁,博士,煤田地质学及比较沉积学.

English Abstract

Paleodrainage Characteristics of the Permian Members C and D in Huainan Coalfield, China

1. Beijing Graduate School, China University of Mining and Technology;

2. Huainan Mining Institute

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淮南煤田二叠系三、四含煤段古水系特征

作者简介: 彭苏萍,男,30岁,博士,煤田地质学及比较沉积学.

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Paleodrainage Characteristics of the Permian Members C and D in Huainan Coalfield, China

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淮南煤田二叠系三、四含煤段古水系特征

1. 中国矿业大学北京研究生部; 2. 淮南矿业学院

作者简介: 彭苏萍,男,30岁,博士,煤田地质学及比较沉积学.

English Abstract

Paleodrainage Characteristics of the Permian Members C and D in Huainan Coalfield, China

1. Beijing Graduate School, China University of Mining and Technology; 2. Huainan Mining Institute

全文HTML

目录

友情链接

期刊在线

联系我们

作者简介:
彭苏萍,男,30岁,博士,煤田地质学及比较沉积学.

1. 中国矿业大学北京研究生部;

2. 淮南矿业学院

作者简介:
彭苏萍,男,30岁,博士,煤田地质学及比较沉积学.

1. Beijing Graduate School, China University of Mining and Technology;

2. Huainan Mining Institute