引用本文:吴小斌, 孙卫, 王进军.鄂尔多斯盆地陇东地区延长组的物源分析[J].沉积与特提斯地质,2008,(4):57-61.[点击复制]
[点击复制]
【打印本页】 【在线阅读全文】【下载PDF全文】 查看/发表评论下载PDF阅读器关闭

←前一篇|后一篇→

过刊浏览    高级检索

本文已被:浏览 221次   下载 151 本文二维码信息
码上扫一扫!
鄂尔多斯盆地陇东地区延长组的物源分析
吴小斌,孙卫,王进军
0
(1. 成都地质矿产研究所;
2. 西北大学地质学系)
摘要:
笔者从区域沉积背景入手,对鄂尔多斯盆地陇东地区长3油层组泥岩稀土元素、碳酸盐岩岩屑、轻重矿物、砂岩粒度等进行综合分析研究,认为研究区内存在混合物源,物源方向主要有北东向和西南向,并初步判断,北东物源的边界大致在南梁-华池地区,西南物源的边界大约在悦乐地区。
关键词:  延长组  稀土元素  碳酸盐岩岩屑  轻重矿物  物源分析  鄂尔多斯盆地
DOI:
附件
基金项目:国家“973”重点科技攻关项目(2003CB214606)资助
Provenance analysis of the Yanchang Formation in eastern Gansu,Ordos Basin
WU Xiao-bin, SUN Wei, WANG Jin-jun
(1. Chengdu Institute of Geology and Mineral Resources, Chengdu 610082, Sichuan, China;
2. Department of Geology, Northwest University, Xi'an 710069, Shaanxi, China)
Abstract:
The synthetic analysis of REEs in mudstone,carbonate debris contents,light and heavy minerals and grain sizes of sandstone in the Chang-3 oil reservoirs shows that the sediments dominantly come from the northeast and southwest in eastern Gansu,Ordos Basin.The provenance boundaries are approximately arranged in the Nanliang-Huachi region in the northeast,and in the Yuele region in the southwest.
Key words:  Yanchang Formation  REE  carbonate debris  light and heavy mineral  provenance analysis  Ordos Basin

用微信扫一扫

用微信扫一扫