大别山北缘早白垩世黑石渡组沉积体系研究

李双应; 李任伟; 王道轩; 刘因; 岳书仓; 孟庆任; 金福全

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大别山北缘早白垩世黑石渡组沉积体系研究

李双应, 李任伟, 王道轩, 刘因, 岳书仓, 孟庆任, 金福全

文章导航 > 沉积学报 > 2004 > 22(4): 566-572

李双应, 李任伟, 王道轩, 刘因, 岳书仓, 孟庆任, 金福全. 大别山北缘早白垩世黑石渡组沉积体系研究[J]. 沉积学报, 2004, 22(4): 566-572.

引用本文:

李双应, 李任伟, 王道轩, 刘因, 岳书仓, 孟庆任, 金福全. 大别山北缘早白垩世黑石渡组沉积体系研究[J]. 沉积学报, 2004, 22(4): 566-572.

LI Shuang ying, LI Ren wei, WANG Dao xuan, LIU Yin, YUE Shu cang, MENG Qing ren, JIN Fu quan. Depositional System of Early Cretaceous Heishidu Formation in the North Margin of the Dabie Mountains[J]. Acta Sedimentologica Sinica, 2004, 22(4): 566-572.

Citation:

李双应, 李任伟, 王道轩, 刘因, 岳书仓, 孟庆任, 金福全. 大别山北缘早白垩世黑石渡组沉积体系研究[J]. 沉积学报, 2004, 22(4): 566-572.

引用本文:

李双应, 李任伟, 王道轩, 刘因, 岳书仓, 孟庆任, 金福全. 大别山北缘早白垩世黑石渡组沉积体系研究[J]. 沉积学报, 2004, 22(4): 566-572.

Citation:

大别山北缘早白垩世黑石渡组沉积体系研究

1.
合肥工业大学资源与环境工程学院合肥 230009;
2.
中国科学院地质与地球物理研究所北京 100029

基金项目: 国家重点基础研究发展规划项目(编号:G1999075507)资助.

详细信息

作者简介:
李双应男 1956年出生博士教授(博士生导师) 沉积地质学

中图分类号: P512.2

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文章访问数: 607
HTML全文浏览量: 5
PDF下载量: 406
被引次数: 0

Depositional System of Early Cretaceous Heishidu Formation in the North Margin of the Dabie Mountains

1.
College of Resource and Environment Engineering, Hefei University of Technology, Hefei 230009;
2.
Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029

摘要

摘要: 分布于大别山北缘晓天—磨子潭断裂以北和金寨—响洪甸—西汤池断裂以南呈东西向延伸的早白垩世黑石渡组,厚达千米,岩相主要有角砾岩、砾岩、砂岩、粉砂岩、泥岩等,包括冲积扇、河流、扇三角洲和湖泊沉积体系,其中河流沉积主要由洪泛平原和决口扇组成。黑石渡组属于向上变细层序,早期为冲积扇沉积,中期为洪泛平原、决口扇和扇三角洲沉积,晚期为深湖浊流沉积。冲积扇和湖相浊流沉积主要发育于盆地东段舒城晓天地区,洪泛平原和决口扇沉积主要发育于盆地西段霍山地区,扇三角洲在两地都比较发育。这是一个不对称的断陷盆地,晓天—磨子潭断裂可能对盆地的发育具有控制作用。
- 黑石渡组 /
- 早白垩世 /
- 沉积体系 /
- 大别山北缘
Abstract: The Early Cretaceous Heishidu Formation (HsdF), distributed between the southern Xiaotian Mozitang fault (XMF) and northern Jinzhai Xianghongdian Xitanchi fault in the north margin of the Dabie Mountains, elongates in east westward, and thickness is more than 1 km. The lithofacies are mainly composed of Bcm, Gcg, Gcm, Gm, Sg, Ss, Fc, Fm, Fr, C and so on, and depositional systems include alluvial fan, fluvial, fan delta and lacustrine deposits, and fluvial deposits are mainly composed of sediments of floodplain and crevasse splays. HsdF developed the fining upward sequences, and alluvial fan in the early stage, floodplain and crevasse splay and fan delta in the middle stage, and lacustrine turbidites in the late stage. Alluvial fan and lacustrine turbidites mainly developed in Xiaotian area on the eastern part of the basin, floodplain and crevasse splay in Huoshan area on the western, and fan delta on both parts. The basin might be attributed to an asymmetric down faulted lake, and its evolution might be controlled by XMF.
- Heishidu Formation /
- Early Cretaceous /
- depositional system /
- the north margin of the Dabie Mountains

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参考文献(11)

[1]	李双应,王道轩,刘因,等.大别造山带北缘中生代冲积沉积体系对源区构造的沉积响.地质通报,2002,21(8～9):541～546[Li Shuangying, Yue Shucang, Wang Daoxuan, et al.Sedimentological response of Mesozoic alluvial depositional systems to tectonism in the source area on the northern margin of the Dabie orogenic belt. Geological Bulletin of China, 2002,21(8～9):541～546]
[2]	杨为民,杨有根.北淮阳地区的中生界.安徽地质, 1995.5(4):11～17[Yang Weimin, Yang Yougen. Mesozoic Erathem of the north Huaiyang area. Geology of Anhui, 1995, 5(4): 11～17]
[3]	韩树芬.安徽北部中新生代沉积盆地分析.北京:地质出版社,1996.16～40[Hang Shufen. Analysis of Mesozoic and Cenozoic Sedimentary Basins in North Anhui. Beijing: Geological Publishing House, 1996.117～121]
[4]	李双应,岳书仓,王道轩,等.大别造山带北缘中生代地层格架厘定.地层学杂志,2002,22(3):178～186[Li Shuangying, Yue Shucang, Wang Daoxuan, et al. Age determining of Mesozoic strata in the north of Dabie Orogenic Belt. Journal of Stratigraphy, 2002, 26(3): 178～186]
[5]	Miall A D. The Geology of Fluvial Deposits. Berlin:Springer-Verlag, 1996.343～419
[6]	Sohn Y K, Rhee C W, Kim B C. Debris flow and hyperconcentrated flood-flow deposits in an alluvial fan, northwestern part of the Cretaceous Yongdong Basin, central Korea. The Journal of Geology, 1999, 107: 111～132
[7]	Nemec W, Steel R J. What is a fan delta and how do we recognize it? In: Nemec W, Steel R J, eds. Fan delta: Sedimentology and tectonic settings. Blackie and Son, Glasgow, 1988.3～13
[8]	黄杏珍,何明喜,李振西,等.中国河南省白湾盆地的白垩系特征.沉积学报,1996,14(增刊):38～47 [Huang Xingzhen, He Mingxi, Li Zhenxi, et al.The characteristics of Cretaceous system in Baiwan basin of Henan Province, China. Acta Sediemntaologica Sinica, 1996,14 (Supp.): 38～47]
[9]	晋慧娟,李育慈.西秦岭造山带中三叠统复理石相研究.沉积学报,2001,19(3):321～326 [Jin Huijuan, Li Yuci. A study on Middle Triassic flysch facies in west Qinling orogenic belt. Acta Sedimentological Sinica, 2001, 19(3):321～326]
[10]	刘招君.湖泊水下扇沉积特征及影响因素.沉积学报,2003,21(1):148～154 [Liu Zhaojun. Lacustrine subaqueous fan sedimentary characteristics and influence factors. Acta Sedimentologica Sinica, 2003, 21(1): 148～154]
[11]	Bridge J S, Mackey S D. Averised alluvial stratigraphy model. In: Marzo M, Puigdefabregas C,eds. Alluvial sedimentation. Special publication number 17 of the International Association of Sedimentologists. London: lackwell scientific publications, Oxford,1993.319～336

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文章访问数: 607
HTML全文浏览量: 5
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大别山北缘早白垩世黑石渡组沉积体系研究

1. 合肥工业大学资源与环境工程学院合肥 230009;

2. 中国科学院地质与地球物理研究所北京 100029

基金项目: 国家重点基础研究发展规划项目(编号:G1999075507)资助.

作者简介:
李双应男 1956年出生博士教授(博士生导师) 沉积地质学

收稿日期: 2003-10-28
修回日期: 2004-01-07
刊出日期: 2004-12-10

中图分类号: P512.2

关键词:

摘要: 分布于大别山北缘晓天—磨子潭断裂以北和金寨—响洪甸—西汤池断裂以南呈东西向延伸的早白垩世黑石渡组,厚达千米,岩相主要有角砾岩、砾岩、砂岩、粉砂岩、泥岩等,包括冲积扇、河流、扇三角洲和湖泊沉积体系,其中河流沉积主要由洪泛平原和决口扇组成。黑石渡组属于向上变细层序,早期为冲积扇沉积,中期为洪泛平原、决口扇和扇三角洲沉积,晚期为深湖浊流沉积。冲积扇和湖相浊流沉积主要发育于盆地东段舒城晓天地区,洪泛平原和决口扇沉积主要发育于盆地西段霍山地区,扇三角洲在两地都比较发育。这是一个不对称的断陷盆地,晓天—磨子潭断裂可能对盆地的发育具有控制作用。

English Abstract

Depositional System of Early Cretaceous Heishidu Formation in the North Margin of the Dabie Mountains

1. College of Resource and Environment Engineering, Hefei University of Technology, Hefei 230009;

2. Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029

Received Date: 2003-10-28
Rev Recd Date: 2004-01-07
Publish Date: 2004-12-10

Keywords:

Abstract: The Early Cretaceous Heishidu Formation (HsdF), distributed between the southern Xiaotian Mozitang fault (XMF) and northern Jinzhai Xianghongdian Xitanchi fault in the north margin of the Dabie Mountains, elongates in east westward, and thickness is more than 1 km. The lithofacies are mainly composed of Bcm, Gcg, Gcm, Gm, Sg, Ss, Fc, Fm, Fr, C and so on, and depositional systems include alluvial fan, fluvial, fan delta and lacustrine deposits, and fluvial deposits are mainly composed of sediments of floodplain and crevasse splays. HsdF developed the fining upward sequences, and alluvial fan in the early stage, floodplain and crevasse splay and fan delta in the middle stage, and lacustrine turbidites in the late stage. Alluvial fan and lacustrine turbidites mainly developed in Xiaotian area on the eastern part of the basin, floodplain and crevasse splay in Huoshan area on the western, and fan delta on both parts. The basin might be attributed to an asymmetric down faulted lake, and its evolution might be controlled by XMF.

李双应, 李任伟, 王道轩, 刘因, 岳书仓, 孟庆任, 金福全. 大别山北缘早白垩世黑石渡组沉积体系研究[J]. 沉积学报, 2004, 22(4): 566-572.

引用本文:

李双应, 李任伟, 王道轩, 刘因, 岳书仓, 孟庆任, 金福全. 大别山北缘早白垩世黑石渡组沉积体系研究[J]. 沉积学报, 2004, 22(4): 566-572.

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大别山北缘早白垩世黑石渡组沉积体系研究

作者简介:
李双应男 1956年出生博士教授(博士生导师) 沉积地质学

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Depositional System of Early Cretaceous Heishidu Formation in the North Margin of the Dabie Mountains

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大别山北缘早白垩世黑石渡组沉积体系研究

1. 合肥工业大学资源与环境工程学院合肥 230009;

2. 中国科学院地质与地球物理研究所北京 100029

作者简介:
李双应男 1956年出生博士教授(博士生导师) 沉积地质学

English Abstract

Depositional System of Early Cretaceous Heishidu Formation in the North Margin of the Dabie Mountains

1. College of Resource and Environment Engineering, Hefei University of Technology, Hefei 230009;

2. Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029

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[1]	李忠. “从最高到最深”—从第17届国际沉积学大会看沉积学研究前沿 . 沉积学报, 2006, (6): 928-933.
[2]	李忠. “从最高到最深”—从第17届国际沉积学大会看沉积学研究前沿 . 沉积学报, 2006, 24(06): 928-933.

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大别山北缘早白垩世黑石渡组沉积体系研究

作者简介: 李双应 男 1956年出生 博士 教授(博士生导师) 沉积地质学

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Depositional System of Early Cretaceous Heishidu Formation in the North Margin of the Dabie Mountains

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出版历程

目录

大别山北缘早白垩世黑石渡组沉积体系研究

1. 合肥工业大学资源与环境工程学院 合肥 230009; 2. 中国科学院地质与地球物理研究所 北京 100029

作者简介: 李双应 男 1956年出生 博士 教授(博士生导师) 沉积地质学

English Abstract

Depositional System of Early Cretaceous Heishidu Formation in the North Margin of the Dabie Mountains

1. College of Resource and Environment Engineering, Hefei University of Technology, Hefei 230009; 2. Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029

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期刊在线

联系我们

作者简介:
李双应男 1956年出生博士教授(博士生导师) 沉积地质学

1. 合肥工业大学资源与环境工程学院合肥 230009;

2. 中国科学院地质与地球物理研究所北京 100029

作者简介:
李双应男 1956年出生博士教授(博士生导师) 沉积地质学

1. College of Resource and Environment Engineering, Hefei University of Technology, Hefei 230009;

2. Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029