冀中坳陷蠡县斜坡古近系沙一下亚段沉积物源分析<sup>&#x0002A;</sup>

doi:10.7605/gdlxb.2016.05.061

古地理学报 ›› 2016, Vol. 18 ›› Issue (5): 809-818. doi: 10.7605/gdlxb.2016.05.061

• 岩相古地理学及沉积学 • 上一篇下一篇

冀中坳陷蠡县斜坡古近系沙一下亚段沉积物源分析^*

刘金龙¹, 李胜利¹, 梁星如², 黄杰², 梁官忠², 于仁江², 曹斌², 吕俊平²

1 中国地质大学(北京)能源学院,北京 100083;
2 中国石油华北油田分公司,河北任丘 062552

收稿日期:2016-03-21 修回日期:2016-06-17 出版日期:2016-10-01 发布日期:2016-10-01
通讯作者: 李胜利,男,1971年生,博士,副教授,主要从事储层沉积学方面的教学和科研工作。E-mail: slli@cugb.edu.cn。
作者简介:刘金龙,男,1992年生,中国地质大学(北京)硕士研究生,研究方向为沉积学。通讯地址:北京市海淀区学院路29号中国地质大学能源学院。E-mail: 442993143@qq.com。
基金资助:
*国家自然科学基金项目(编号: 41572080.41272132)与中石油华北油田重大科技专项(编号: HBYT-YJY-2015-JS)联合资助

Provenance analysis of the lower part of Member 1 of Paleogene Shahejie Formation in Lixian Slope,Central Hebei Depression

Liu Jinlong¹, Li Shengli¹, Liang Xingru², Huang Jie², Liang Guanzhong², Yu Renjiang², Cao Bin², Lü Junping²

1 School of Energy Resources,China University of Geosciences(Beijing),Beijing 100083;
2 Huabei Oilfield Company,PetroChina,Renqiu 062552,Hebei

Received:2016-03-21 Revised:2016-06-17 Online:2016-10-01 Published:2016-10-01
Contact: Liu Jinlong,born in 1992,is a M.S. degree candidate in China University of Geosciences(Beijing). His research field is sedimentology E-mail: 442993143@qq.com.About the corresponding author Li Shengli,born in 1971,doctor,is an associate professor in China University of Geosciences(Beijing). He is mainly engaged in the study of reservoir and sedimentology.E-mail: slli@cugb.edu.cn.
Supported by:
; [Co-funded by the National Natural Science Foundation of China(No.41572080.41272132)and Major Science and Technology Research Program of Huabei Oilfield Company,PetroChina(No; HBYT-YJY-2015-JS)]

摘要/Abstract

摘要： 基于对冀中坳陷饶阳凹陷蠡县斜坡碎屑岩分析化验资料,结合该区古水系与古地貌特征,从岩样的碎屑组分、岩屑类型、重矿物组合与ZTR指数及地震剖面反射特征等方面,对古近系沙河街组一段下亚段(沙一下亚段)沉积的物源方向进行综合研究。结果表明:蠡县斜坡古近系沙一下亚段的沉积物主要来自于斜坡西南部和北部,其中西南部物源区主要位于太行山隆起,沉积物分别由古大沙河经由斜坡南部及古唐河越过高阳低凸起运移进入斜坡,是主要物源;北部物源主要来自牛驼镇低凸起,是次要物源。西南部物源与北部物源交汇于蠡县斜坡东部西柳地区。

关键词: 蠡县斜坡, 古近系沙河街组, 古水系与古地貌, 重矿物组合, 沉积物源分析

Abstract: Based on the testing data,the provenance was determined according to the palaeodrainage pattern and palaeomorphology,clastic components,lithic fragment types,heavy mineral assemblages and ZTR index and seismic profile features. The results show that the sediments of the lower part of Member 1 of Paleogene Shahejie Formation in Lixian Slope mainly derived from the southwestern and northern provenances. The southwestern provenance mainly located in the Taihangshan uplift,whose sediments were carried by the ancient Dashahe river through the southern slope,and the ancient Tanghe river cross Gaoyang low uplift. The northern provenance mainly located in the Niutuozhen low uplift. The southwestern provenance was dominant while the northern one was minor. Xiliu area was a convergence region of both procenances.

Key words: Lixian Slope, Paleogene Shahejie Formation, palaeodrainage and palaeomorphology, heavy mineral assemblages, provenance analysis

中图分类号:

P512.2

刘金龙, 李胜利, 梁星如, 黄杰, 梁官忠, 于仁江, 曹斌, 吕俊平. 冀中坳陷蠡县斜坡古近系沙一下亚段沉积物源分析^*[J]. 古地理学报, 2016, 18(5): 809-818.

Liu Jinlong, Li Shengli, Liang Xingru, Huang Jie, Liang Guanzhong, Yu Renjiang, Cao Bin, Lü Junping. Provenance analysis of the lower part of Member 1 of Paleogene Shahejie Formation in Lixian Slope,Central Hebei Depression[J]. JOPC, 2016, 18(5): 809-818.

http://www.gdlxb.cn/CN/Y2016/V18/I5/809

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