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鄂尔多斯盆地镇北地区延长组长7沉积期物源分析
引用本文:周黎霞,王居里,张雷. 鄂尔多斯盆地镇北地区延长组长7沉积期物源分析[J]. 西安文理学院学报, 2011, 0(4): 82-86,94
作者姓名:周黎霞  王居里  张雷
作者单位:[1]低渗透油气田勘探开发国家工程实验室,陕西西安710018 [2]长庆油田分公司勘探开发研究院,陕西西安710018 [3]西北大学地质系,陕西西安710069
摘    要:收集前人研究成果,结合薄片鉴定、重矿物分析、稀土元素及地震等资料,对鄂尔多斯盆地延长组长7沉积期物源进行分析.结果表明:镇北地区延长组长7物源来自盆地西部和西南方向,其中西南物源为主要物源区,主要岩性为变质岩、中酸性岩浆岩;西部方向仅为沉积区提供白云岩等碳酸盐岩碎屑.

关 键 词:碎屑岩成熟度  重矿物  稀土元素  聚类分析  物源方向

An Analysis of Sediment Provenance of the Chang7 Oil-bearing in the Zhenbei Area,Ordos Basin
ZHOU Li-xia,WANG Ju-li,ZHANG Lei. An Analysis of Sediment Provenance of the Chang7 Oil-bearing in the Zhenbei Area,Ordos Basin[J]. Journal of Xi‘an University of Arts & Science:Natural Science Edition Edi Edition, 2011, 0(4): 82-86,94
Authors:ZHOU Li-xia  WANG Ju-li  ZHANG Lei
Affiliation:1.National Engineering Laboratory for Low-permeability Petroleum Exploration and Development,Xi'an 710018,China; 2.Research Institute of Exploration and Development,Changqing Oilfield Company,PetroChina,Xi'an 710018,China; 3.Department of Geology,Northwest University,Xi'an 710069,China)
Abstract:Based on previous research and the references concerning thin section identification,heavy mineral analysis,rare earth elements and seismic data,we give an analysis of Chang 7 sedimentary provenance in Ordos Basin.The result shows that Chang 7 source in Zhenbei area is from the west and southwest of the basin.The main provenance is the southwest area where the major lithology is that of metamorphic rocks and intermediate-acid magmatic rocks.The west area is only the sedimentary provenance where dolomite and other carbonate rock debris are found.
Keywords:clastic rock maturity  heavy minerals  rare earth elements  cluster analysis  source direction
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