江西修水下古生界岩层中的水力破裂现象及其意义  

Hydraulic Fracturing in Lower Paleozoic Strata in Xiushui, Jiangxi and Its Implications

作　　者：祁向雷[1] 印纯清[1] 索书田[1] 

机构地区：[1]中国地质大学

出　　处：《江西地质科技》1997年第1期29-32,共4页

摘　　要：本文简要阐述了水力破裂的基本原理和工作方法。通过对江西修水下古生界岩层中的水力破裂现象描述和分类,分析其形成条件和构造环境。指出水力破裂作用在修水地区对多级滑脱构造的研究具有重要意义。This paper describes briefly the fundamental principles and working procedures of hydraulicfracturing. Based on a description and clasification of the hydraulic fracturing in the Lower Paleozoic strata in Xiushui,Jiangxi,and on an. analysis on its formative conditions and tectonic setting,the author points out taht hydraulic fracturing has a great significance in the study of multiple decollement structures in the Xiushui area.

关 键 词：水力破裂 下古生界 多级滑脱构造 岩层 滑脱构造 

分 类 号：P542.3[天文地球—构造地质学]