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鄂尔多斯盆地东南部二叠系物源分析
引用本文:屈红军,马强,高胜利,梅志超,苗建宇.鄂尔多斯盆地东南部二叠系物源分析[J].地质学报,2011,85(6):979-986.
作者姓名:屈红军  马强  高胜利  梅志超  苗建宇
作者单位:1. 西北大学大陆动力学国家重点实验室/地质学系,西安,710069
2. 中石油吐哈油田分公司勘探开发研究院,新疆哈密,839000
3. 西北大学大陆动力学国家重点实验室/地质学系,西安,710069;陕西延长石油(集团)有限公司研究院,西安,710000
基金项目:国家重点基础研究发展计划(973计划)
摘    要:近几年鄂尔多斯盆地东南部上古生界陆续发现新的天然气区带,显示出巨大的勘探潜力,因此对盆地东南部二叠系物源的研究对于确定储集砂体展布规律具有重要价值。以钻测井、岩心及周边露头资料为基础,通过露头剖面古流向测定、重矿物分析、边缘相分析、相带分析的方法,确定了研究区二叠系的物源方向;研究认为鄂尔多斯盆地东南部二叠系山西组与石盒子组物源可分为北北东、北北西及南部三个方向,以延安为中心区域属于汇水区;山2段南部物源影响范围较大,影响到延安以北区域;盒8段北部物源范围较大,越过了延安,相应的南部物源范围后撤。

关 键 词:鄂尔多斯盆地  古流向  重矿物  物源  边缘相
收稿时间:2010/7/26 0:00:00
修稿时间:12/1/2010 2:42:53 PM

Study on Provenance of the Permian in southeast Ordos basin
Qu Hongjun,ma qiang,gao shengli,mei zhichao and miao jianyu.Study on Provenance of the Permian in southeast Ordos basin[J].Acta Geologica Sinica,2011,85(6):979-986.
Authors:Qu Hongjun  ma qiang  gao shengli  mei zhichao and miao jianyu
Institution:Northwest University,Institute of Petroleum Exploration and Development, Tuha Oil Corporation, CNPC,Research institute of Shaanxi Yanchang Petroleum Corporation,Northwest University,Northwest University
Abstract:Recent years lots of new gas plays are found continuously in the Upper Paleozoic in southeast Ordos basin, which displays great exploration prospects. Therefore, the study on Provenance of the Permian in southeast Ordos basin is of great importance to confine reservoir distribution rules. Based on data of well drilling, logging and core as long with outcrop sections of surroundings, the provenance directions of the Permian are confined by means of paleo-current direction measuring in outcrop sections, heavy mineral analyzing, and marginal facies diagnosing as well as facies belt construing. The study shows that the provenance of Shanxi and Shehezi Formation of the Permian in southeast Ordos basin can be divided into three directions which are NNE, NNE, and south, while Yanan region being the center of water catchment; The influence area of southern provenance is bigger in Shan-2 member which influenced areas of north of Yanan; The influence area of northern provenance is bigger in He-8 member which overreached areas of south of Yanan while the southern provenance receded simultaneously.
Keywords:Ordos basin  paleo-current directions  heavy minerals  Provenance  marginal facies
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