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鄂尔多斯盆地镇原-泾川地区三叠系延长组构造裂缝分布定量预测
引用本文:张林炎,范昆,刘进东,周新桂,王春宇,袁杨森.鄂尔多斯盆地镇原-泾川地区三叠系延长组构造裂缝分布定量预测[J].地质力学学报,2006,12(4):476-484.
作者姓名:张林炎  范昆  刘进东  周新桂  王春宇  袁杨森
作者单位:1. 中国地质科学院地质力学研究所, 北京 100081;
基金项目:中国石油化工集团公司资助项目
摘    要:根据露头地层、钻井岩心、岩石薄片等对构造裂缝进行了详细观测统计,分析了镇原-泾川地区三叠系延长组储层构造裂缝的基本特征、力学构成和成因。以研究区目的层构造裂缝的实际情况为依据,以有限元数值模拟方法为基础,应用岩石破裂法,对延长组构造裂缝分布和发育程度进行了初步定量预测研究,为鄂尔多斯盆地镇原-泾川地区石油勘探提供了有利区评价依据。 

关 键 词:构造裂缝系统    定量预测    三叠系延长组    镇原-泾川地区    鄂尔多斯盆地
文章编号:1006-6616(2006)04-0476-09
收稿时间:2006-04-05
修稿时间:2006年4月5日

QUANTITATIVE PREDICTION OF DISTRIBUTION OF TECTONIC FRACTURES IN THE YANCHANG FORMATION IN THE ZHENYUAN-JINGCHUAN AREA, ORDOS BASIN
ZHANG Lin-yan,FAN Kun,LIU Jin-dong,ZHOU Xin-gui,WANG Chun-yu,YUAN Yang-sen.QUANTITATIVE PREDICTION OF DISTRIBUTION OF TECTONIC FRACTURES IN THE YANCHANG FORMATION IN THE ZHENYUAN-JINGCHUAN AREA, ORDOS BASIN[J].Journal of Geomechanics,2006,12(4):476-484.
Authors:ZHANG Lin-yan  FAN Kun  LIU Jin-dong  ZHOU Xin-gui  WANG Chun-yu  YUAN Yang-sen
Institution:1. Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing 100081, China;2. Liaohe Jinma Oilfield Company limited, Panjin 124100, Liaoning, China;3. China University of Geosciences, Belting 100083, China
Abstract:Detailed observations and statistics of tectonic fractures in outcrops, drilling cores and thin sections have been made and the basic characteristics, mechanics and origin of tectonic fractures in reservoirs of the Triassic Yanchang Formation in the Zhenyuan-Jingchuan area have been analyzed. According to the actual conditions of tectonic fractures in the target strata in the Zhenyuan-Jingchuan area and on the basis of finite element simulation, the authors have quantitatively predicted and evaluated the distribution and development degree of the tectonic fractures by using the rock breaking method, which may be used as a reference for evaluation of a favorable target area in petroleum exploration in the Zhenyuan-Jingchuan area.
Keywords:fracture system  quantitative prediction  Yanchang Formation  Zhenyuan-Jingchuan area  Ordos basin
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