1) Tonghualing intermediate-acid intrusive rocks
铜华岭岩体
1.
Tonghualing intermediate-acid intrusive rocks is located in Yemaquan arc between Armantai fault and Kelameili fault,Eastern Junggar,North Xinjiang.
6 Ma,说明铜华岭岩体是早古生代岩浆活动的产物,为东准噶尔早古生代造山带演化提供了花岗岩证据。
2) Tongshanling granite body
铜山岭岩体
3) Siling pluton
泗岭岩体
4) Fuling mass
伏岭岩体
1.
Petrology and geochemistry of the Fuling mass in Jixi, southern Anhui;
皖南绩溪伏岭岩体岩石地球化学特征
5) Wangxianling pluton
王仙岭岩体
1.
Important significance of regional tectonic regime to metallogenic capacity of Indosinian and Early Yanshanian granites in southeastern Hunan:A case study of Qianlishan and Wangxianling plutons;
区域构造体制对湘东南印支期与燕山早期花岗岩成矿能力的重要意义——以千里山岩体和王仙岭岩体为例
6) 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。
补充资料:铜华
1.见"铜花"。
说明:补充资料仅用于学习参考,请勿用于其它任何用途。
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