摘要
通过推覆剪切热估算和花岗岩岩石学特征的研究，作者认为达拉布特地区的花岗岩岩体是由推覆剪切重熔形成的。
Through thrust-shearing thermal calculations and studies on petrological characteristcs of granites near Qiqiu No.1 gold deposit,the authors stated that the granites were formed from thrust-shearing anatexis, which was directly in fluences on the forming of the deposit.
出处
《矿物岩石》
CAS
CSCD
1996年第2期77-81,共5页
Mineralogy and Petrology
关键词
花岗岩
金矿床
构造重熔
成因
Thearing,Qiqiu No.1 gold deposit,granite rock mass
