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华北克拉通南部周口坳陷谭庄-沈丘凹陷早白垩世沉积、构造特征与原型盆地性质

旷红伟 穆朋飞 顾兴明 柳永清 彭晓波 杨飞 陈铭培 岑超 彭楠 李家华 王晓光

地质论评2009,Vol.55Issue(6):804-815,12.
地质论评2009,Vol.55Issue(6):804-815,12.

华北克拉通南部周口坳陷谭庄-沈丘凹陷早白垩世沉积、构造特征与原型盆地性质

Sedimentary and Tectonic Features and Proto-basin of Early Cretaceous Tanzhuang-Shenqiu Sag, Zhoukou depression, in southern area of North China Craton

旷红伟 1穆朋飞 2顾兴明 1柳永清 1彭晓波 2杨飞 1陈铭培 1岑超 1彭楠 1李家华 1王晓光1

作者信息

  • 1. 油气资源与勘探技术教育部重点实验室(长江大学)长江大学地球物理与石油资源学院,湖北荆州,434023
  • 2. 中国地质科学院地质研究所,北京,100037
  • 折叠

摘要

Abstract

Located at the sourthern margin of the North China Craton, the Tanzhuang-Shenqiu sag, Zhoukou depression, is filled with Lower Cretaceous sediments in a huge thinckness. Deposits in the sag are characterized by thinner grained clastic rocks with miderteran composition and texture maturations, such as mudstone, siltstone and sandstone, and especially rich in volcanic clastics. Sedimentary structures and depositional facies associations interpreted as fluvial-delta and lacustrine environments were recognized in this research. Present study insisted that sediments supply of the Tanzhuang-Shenqiu sag in Early Cretaceous are from the Dabie orogenic belt to the south. Basin's Formation was initially controlled by the southern marginal stretch fault, I.e.,Yelu fault, which became thrusting toward north at the end of Early Cretaceous. Based upon study of sandstone composition and Q-F-L diagram (Dickinson's diagram), geochemistry of major and REE elements of sediments and the geochonology of volocanic rocks, writers suggest that the Tanzhuang-Shenqiu sag formed in a regional stretch tectonic setting in the Early Cretaceous, was a original fault basin.

关键词

华北/早白垩世/沉积/构造/盆地

Key words

North China/ Early Cretaceous/ deposition/ tectonic/ Zhoukou depression

分类

天文与地球科学

引用本文复制引用

旷红伟,穆朋飞,顾兴明,柳永清,彭晓波,杨飞,陈铭培,岑超,彭楠,李家华,王晓光..华北克拉通南部周口坳陷谭庄-沈丘凹陷早白垩世沉积、构造特征与原型盆地性质[J].地质论评,2009,55(6):804-815,12.

基金项目

本文为国土资源部全国油气资源战略选区调查与评价专项"东秦岭-大别山造山带两侧油气资源战略选区研究"(子课题编号XQ-2007-02-3-4)的成果. (子课题编号XQ-2007-02-3-4)

地质论评

OA北大核心CSCDCSTPCD

0371-5736

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