晚期为脆性破裂构造，与早期变形组构具继承、叠加关系。
In the late period, brittle rupture structures inherited and were superimposed on the early deformation fabrics.
洪日豪(1994)台湾西部三义逆冲断块及出磺坑背斜的变形组构分析。台湾石油地质，第29号，第105 - 126页。
Hong, R. H. (1994) Analysis of deformation fabrics in the Sani thrust sheet and the Chuhuangkeng anticline of western Taiwan. Petroleum Geology of Taiwan, 29, 105-126.
而且含金构造中岩石的组构特征、糜棱岩类型、应变幅度、石英变形机制与金矿富集程度都有密切的关系。
The gold abundance is also related to the type of mylonite, the feature of micro-fabric, the mechanism of quartz deformation and the size of strain.
本文详细研究了台湾澎湖列岛上地幔幔源包体的变形结构、组构和橄榄石位错构造。
This paper deals with deformation textures, petrofabrics and dislocation microstructures of olivine from the mantle-derived xenoliths in the Penghu Islands, Taiwan.
岩石的应变组构型式与岩石成分、变形环境和应变过程有着密切关系。
The styles of strain fabrics in rocks are closely associated with the components of rocks, the environment of deformation and the history of straining.
本文介绍了利用变形椭球体理论，对花岗岩组构(叶理、线理)进行应变分析的方法。
This paper introduces the method for a strain analysis of the fabric (foliation and lineation) of granite by using the theory of the strain ellipsoid.
矿区的磁线理、磁面理等磁组构研究表明，磁组构能与岩组研究一样，解决岩石变形的应力场问题。
The magnetic lineation and magnetic foliation study of the ore area show that the magnetic fabric study can proclaim the stress field of rock deformation as the petrofabric analysis.
对橄榄岩中单斜辉石和斜方辉石的组构分析表明，碧溪岭地区超基性岩经历了塑性变形，形成了LPO组构；
The fabric analysis of Cpx and Opx in peridotite indicates that the Bixiling ultra_basic rocks has experienced the ductile deformation, resulting in the LPO fabric.
焦家断裂带晚期表现为强烈的脆性变形，但其早期则表现以糜棱岩组合、对称组构等为特征的韧性变形。
The Jiaojia fault zone is characterized by ductile deformation in the early stage and brittle fracturing in late stage.
岩石磁组构分析可用来研究岩石的组构特征及构造变形。
An analysis of the rock magnetic fabric can be used to study the fabric characteristics of the rocks and structural deformation.
本文研究了典型韧性变形断裂和弱变形区的岩石磁组构特征。
The paper studies magnetic fabric characteristic of faults developed in the typical ductility and weak deformation areas.
本文研究了典型韧性变形断裂和弱变形区的岩石磁组构特征。
The paper studies magnetic fabric characteristic of faults developed in the typical ductility and weak deformation areas.
应用推荐