Qitianling area骑田岭
1.Analysis on the tin-polymetallic mineralization characteristics and prospecting potential in northern Qitianling area of Hunan Province;骑田岭北部地区锡多金属矿成矿特征及找矿潜力分析
3)Qitianling pluton骑田岭岩体
1.Qitianling pluton was formed by two phases of emplacement,and is mainly composed of early stage granite.湘南骑田岭岩体主要由两阶段侵位所形成,早阶段侵位花岗岩组成骑田岭岩体的主体。
2.The granitic rocks of the Cailing superunit in the Qitianling pluton are mainly horblende-biotite monzonitic granite.湘南骑田岭岩体菜岭超单元花岗岩以角闪石黑云母二长花岗岩为主,其全岩Rb-Sr等时线年龄为159±1。
4)Furong orefield in Qitianling骑田岭芙蓉矿田
5)Qitianling granites骑田岭花岗岩
1.Tin mineralized bodies mainly occur in the iault zones and alteration zones of the Qitianling granites,which genetically related to chlorite alteration.近年来,在湘南新探明一个超大型锡矿床—芙蓉锡矿床,其中,最重要的锡矿化产在骑田岭花岗岩体西南部的破碎蚀变带内,与绿泥石化密切相关。
6)Qitianling A-type granite骑田岭A型花岗岩
1.Qitianling A-type granite has a close temporal,spatial and genetic relationship with Furong superlarge tin deposit.南岭中段骑田岭A型花岗岩与芙蓉超大型锡矿床具有密切的时间和空间关系。
延伸阅读
骑田岭骑田岭中国南岭之一。位于湖南省东南部宜章县、郴州市之间。古代名称不一：秦名阳山，晋名腊岭；又有桂阳岭、客岭山、黄岑山、折岭等名。主要由花岗岩构成。主峰海拔1510米。为湘江支流耒水和北江西源武水分水岭。附近的折岭关，向为湘、粤通道。京广铁路通过东侧。
