涟邵煤田金竹山向斜构造应力场探讨  

A DISCUSSION OF THE STRUCTURAL STRESS FIELD INJINZHUSHAN SYNCLINE,LIANSHAO COALFIELD

作　　者：莫时旭[1] 杨荣丰[1] 黄昔容 

机构地区：[1]湘潭工学院

出　　处：《湖南地质》1998年第2期76-80,共5页Hunan Geology

摘　　要：根据共轭剪、张节理和小褶皱发育特征的综合研究，本文恢复了金竹山向斜晚古生代以来的主要４期构造应力场，探讨了该向斜的形成和演化过程。By analyzing various indicators such as conjugated shear joins,tension fissures and small folds,the article reconstructs the main four episodes of structural stress field late Palaeoznic in Jinzhushan syncline,and discusses the process of formation and evolution of the syncline.

关 键 词：煤田 金竹山 向斜构造 应力场 

分 类 号：P618.110.2[天文地球—矿床学]