骑田岭

骑田岭矿&新发现的一种超结构复杂氧化物

Qitianlingite & a newly discovered superstructure complex oxide

芙蓉锡矿田位于湖南省骑田岭花岗岩体的南部，是一个新近发现的超大型锡矿田。

The Furong tin orefield , located in southern Hunan , China , is a newly-discovered super-large tin orefield .

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。

Qitianling pluton was formed by two phases of emplacement , and is mainly composed of early stage granite .

锡矿产于骑田岭复式花岗岩体南部内外接触带，多呈脉状产出。

The tin deposits are occurred as the veins in the southern part of the Qitianling composite granite body and its contact zone .

骑田岭岩体是南岭地区燕山早期具幔源组分贡献的花岗岩典型代表。

The Qitianling pluton is one of the typical granites with the contribution of mantle-derived components in the Nanling region , southern China .

因此本文认为，黄沙坪花岗岩体与千里山、骑田岭等岩体属于同一类型，岩石成因可能与印支造山运动后的岩石圈伸展有关，形成于地壳物质的部分熔融；

They are the same type granitoid . Their lithogenesis was related to the lithospheric extension after the Indosinian Orogenesis , and formed from partial melting of the crust material .

以湖南骑田岭花岗岩复式岩体为实例，进行了芙蓉-菜岭含锡花岗岩和新田岭含钨花岗岩的成矿矿物学对比研究。

Finally , a case study was made in the Qitianling granite complex , which is essentially composed of the Sn granites of Furong and Cailing , and the Xintianling W granite .