摘要
花岗岩体的侵位机制,是受岩区特定的大型区域构造控制或者由其在发育演化过程中所产生的局部构造应力场控制的结果,受诸多因素的控制和影响,但起主导作用的是区域断裂构造,讨论汤湖岩体的构造特点及其侵位机制。
The Granite Emplacement Mechanism, is the local tectonic rock zone specific large regional tectonic control or generated by the evolution of stress field in the control results, controlled and affected by many factors but, played a leading role in the regional faults, this paper mainly discusses the structure and characteristics of Tang Lake pluton emplacement mechanism.
出处
《云南化工》
CAS
2017年第8期115-116,共2页
Yunnan Chemical Technology
关键词
黄坳断裂
汤湖断裂
汤湖岩体
侵位机制
Huangao fracture
Tanghu fracture
Tanghu granite
emplacement mechanism
