摘要
在系统的野外地质调查基础上,通过对元宝山花岗岩体地质特征的分析,运用岩石有限应变测量、应变分析等方法,着重分析了元宝山花岗岩体中电英岩包体的应变特征,确定了电英岩包体的变形时代和原因。系统地开展了元宝山花岗岩体中电英岩包体的三维有限应变测量和应变分析。结果表明:电英岩包体的应变型式可分为3种:平面型应变(K=1)、压扁型应变(0<K<1)和收缩型应变(1<K<∞),且以平面型应变为主,有少量的压扁型应变和收缩型应变。
On the basis of the achievements obtained in geological systemic investigation and analyzing geological characteristics,the authors mainly studied the strain characteristics,genesis and the age of deformation of tourmalite-quartz enclaves.Three-dimensional finite strain measurement and strain analysis of tourmalite-quartz enclaves in Yuanbaoshan pluton were carried out successively.The results show that the three strain patterns of tourmalite-quartz enclaves are plane strain(K=1),flattening strain(0K1) and contraction strain(1K∞).The pattern of strain of tourmalite-quartz enclaves in Yuanbaoshan pluton is mainly plane strain,with minor flattening strain and contraction strain.
出处
《中国地质》
CAS
CSCD
北大核心
2012年第5期1236-1246,共11页
Geology in China
基金
广西自然科学基金项目“桂北元古代九万大山地体叠加伸展构造及其与锡多金属成矿关系”[桂财教(2006)40-180]
广西隐伏金属矿产勘查重点实验室(桂林理工大学)共同资助
关键词
应变测量
应变分析
电英岩包体
花岗岩
元宝山
桂北
strain measurement
strain analysis
tourmalite-quartz enclaves
granite
Yuanbaoshan pluton
Guibei