Sedimentary characteristics of the Cambrian slope controlled by synsedimentary faults in northern margin of Yangtze Platform

doi:10.7605/gdlxb.2013.03.033

JOURNAL OF PALAEOGEOGRAPHY ›› 2013, Vol. 15 ›› Issue (3): 401-412. doi: 10.7605/gdlxb.2013.03.033

• LITHOFACIES PALAEOGEOGRAPHY AND SEDIMENTOLOGY • Previous Articles Next Articles

Sedimentary characteristics of the Cambrian slope controlled by synsedimentary faults in northern margin of Yangtze Platform

Yu Kuanhong Jin Zhenkui Dong Xiaodong Su Kui Zhang Wei,Du Hongyu Chen Ying Zhang Weidan

College of Geosciences，China University of Petroleum(Beijing)，Beijing 102249

Received:2012-06-07 Revised:2012-09-05 Online:2013-06-01 Published:2013-06-01
Contact: About the corresponding author:Jin Zhenkui，born in 1963，is a professor in China University of Petroleum(Beijing).His academic interest is focused on sedimentology.E-mail:jinzhenkui@188.com.
About author:Yu Kuanhong，born in 1983，is a Ph.D.candidate in China University of Petroleum(Beijing).His academic interests are focused on sedimentology and reservoir geology.E-mail:yukuanhong1983@126.com.

扬子地台北缘寒武纪同沉积断裂控制的斜坡沉积特征^*

余宽宏金振奎董晓东苏奎张伟
杜宏宇陈英张卫丹

中国石油大学（北京）地球科学学院，北京 102249

通讯作者: 通讯作者简介金振奎，男，1963年生，中国石油大学（北京）教授，博士生导师，主要从事沉积学方面的研究。E-mail:jinzhenkui@188.com。
作者简介:余宽宏，男，1983年生，现为中国石油大学（北京）博士研究生，主要从事沉积学及储层地质学方面的研究。E-mail:yukuanhong1983@126.com
基金资助:
中国石油化工股份有限公司海相油气前瞻性科研项目（合同编号：YPH08015）成果之一

Abstract

Abstract:

Based on summarizing regional data and practical investigation，the sedimentary characteristics of the slope controlled by synsedimentary faults were studied.It is found that rock types include pebble clastic limestone，micrite，cherts，shale and so on，with abundant sedimentary structures，and the thickness of sedimentary rocks in slope is much larger than that in platform and basin.Palaeogeographic division was controlled by bordering fault zone，and locations of platform，slope and basin remained stationary during different phases of the Cambrian.Region of the slope subsided in a tension environment，with a continuous increasing accommodation space and plenty of sediments from platform，which resulted in much thicker strata in slope than that in shallow platform and deep basin.

Key words: northern margin of Yangtze Platform, slope, synsedimentary fault, sedimentary characteristics

摘要：

通过对扬子地台北缘寒武系剖面实测以及前人资料的综合分析，研究了同沉积断裂控制的斜坡沉积特征。斜坡区岩石类型丰富，包括砾屑石灰岩、灰泥石灰岩、硅岩和页岩等，沉积构造丰富，沉积厚度远大于台地区以及深海盆地区。断裂带在宏观上控制了扬子地台北缘寒武纪古地理分区，台地区、斜坡—深海盆地区的古地理位置在寒武纪的不同地质时期基本保持不变。寒武纪持续拉伸的构造环境造成斜坡区持续下降拗陷，从而为沉积物的堆积提供了足够大的可容空间，同时来自台地区的沉积物补给充足，导致了斜坡区相对于台地区以及深海盆地区而言具有巨厚的沉积层。

CLC Number:

P512.2

Yu Kuanhong, Jin Zhenkui, Dong Xiaodong, Su Kui, Zhang Wei,Du Hongyu, Chen Ying, Zhang Weidan. Sedimentary characteristics of the Cambrian slope controlled by synsedimentary faults in northern margin of Yangtze Platform[J]. JOURNAL OF PALAEOGEOGRAPHY, 2013, 15(3): 401-412.

余宽宏, 金振奎, 董晓东, 苏奎, 张伟, 杜宏宇, 陈英, 张卫丹. 扬子地台北缘寒武纪同沉积断裂控制的斜坡沉积特征^*[J]. 古地理学报, 2013, 15(3): 401-412.

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Sedimentary characteristics of the Cambrian slope controlled by synsedimentary faults in northern margin of Yangtze Platform

扬子地台北缘寒武纪同沉积断裂控制的斜坡沉积特征^*

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Sedimentary characteristics of the Cambrian slope controlled by synsedimentary faults in northern margin of Yangtze Platform

扬子地台北缘寒武纪同沉积断裂控制的斜坡沉积特征*

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扬子地台北缘寒武纪同沉积断裂控制的斜坡沉积特征^*