石油实验地质2012，Vol.34Issue(4)：362-367,6.
贵州南部印支晚期—燕山期构造变形特征
Tectonic deformation features from Late Indosinian to Yanshanian in southern Guizhou
摘要
Abstract
The tectonic deformations in the southern Guizhou were zoned obviously. To the north of Guiyang-Guiding-Sandu, fault belts distributed in NS direction. The studies of fluid inclusion showed that the present fault belts were active from the late Indosinian to Yanshanian and their tectonic deformation features were in accordance with the general law of progressive ( attenuated) deformation caused by the nappe of Xuefeng Mountain from east to west. The rock samples from the fault belts confirmed that rocks were influenced by the squeeze and twist effect from the upper to the lower disk. The faults were compressive. The fault belts were brittle and some were ductile. To the south of Guiyang-Guiding-Sandu, the thrusting of Xuefeng Mountain from east to west led to medium-weak or weak deformations and a gentle anticlinal tectonic framework in NE direction was formed under the influence of Yaziluo squeeze and strike-slip belt. Big difference of stress field existed between the northeast and the southwest of the study area during tectonic evolution. The Anshun and Changshun Sags in the weak deformation belt might be favorable targets for petroleum migration and accumulation.关键词
包裹体数据/X射线衍射数据/断裂带岩组特性/断裂带/构造形变/贵州南部Key words
fluid inclusion data/ X-ray diffraction data/ characteristics of rock group/ fault belt/ tectonic deformation/ southern Guizhou分类
能源科技引用本文复制引用
王津义,彭金宁,王彦清,刘光祥,高林..贵州南部印支晚期—燕山期构造变形特征[J].石油实验地质,2012,34(4):362-367,6.基金项目
中国石油化工股份有限公司科技项目(P04038)和中国石油化工股份有限公司勘探南方分公司科技攻关项目(G0800-10KK-137)资助. （P04038）
