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吐哈盆地鄯善弧形带三间房组二段重矿物物源分析
引用本文:张景琦,;韩小锋,;杨占龙.吐哈盆地鄯善弧形带三间房组二段重矿物物源分析[J].岩性油气藏,2014(6):34-39.
作者姓名:张景琦  ;韩小锋  ;杨占龙
作者单位:[1]中国石油大学(北京)地球科学学院,北京102249; [2]中国石油勘探开发研究院西北分院,兰州730020; [3]中国地质调查局西安地质调查中心,西安710054
基金项目:国家油气重大专项“岩性地层油气藏成藏规律、关键技术及目标评价”(编号:2011ZX05001)资助
摘    要:利用重矿物的相关性分析、因子分析、Q型聚类分析、稳定系数分析、平面组合特征分析以及古地貌地形分析等,对吐哈盆地鄯善弧形带三间房组二段的重矿物组分进行了统计研究,认为该区母岩类型主要为沉积岩和变质岩,分别对应南部塔克泉凸起主要物源区和东南部了墩隆起次要物源区,其中塔克泉凸起物源区主要控制弧形带丘陵地区辫状河三角洲扇体展布形态,了墩隆起物源区主要控制温吉桑地区辫状河三角洲扇体展布形态,丘陵东部地区则为两大物源交汇区.

关 键 词:重矿物  物源分析  鄯善弧形带  吐哈盆地

Provenance analysis of heavy minerals of the second member of Sanjianfang Formation in Shanshan arcuate belt,Tuha Basin
Affiliation:ZHANG Jingqi, HAN Xiaofeng, YANG Zhanlong (1. College of Geoseienees, China University of Petroleum, Beijing 102249, China; 2. PetroChina Research Institute of Petroleum Exploration & Development-Northwest, Lanzhou 730020, China ; 3. Xi' an Center of Geologieal Survey, China Geologieal Survey, Xi'an 710054, China)
Abstract:Based on the analyses of correlation, factor, Q type cluster, stability coefficient, plane assemblage features and paleogeomorphology, this paper studied the heavy mineral components of the second member of Sanjianfang Formation in Shanshan arcuate belt. The result shows that the source rock types are mainly sedimentary rock and metamorphic rock, which respectively responds to the primary provenance in Takequan uplift in the north and the secondary provenance in Liaodun uplift in the southeast. The provenance in Takequan uplift controls the sedimentation of braided delta fan in hill country, and the provenance in Liaodun uplift controls the sedimentation of braided delta fan in Wenjisang area. The eastern hill country is the intersection of Takequan uplift provenance and Liaodun uplift provenance.
Keywords:heavy mineral  provenance analysis  Shanshan areuate belt  Tuha Basin
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