千里山
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红旗岭锡多金属矿床位于东坡矿田北东角,是千里山花岗岩岩体北侧的一个重要的矿床。
The Hongqiling Sn-polymetallic deposit is located at the northeastern corner of the Dongpo minefield and is an important deposit on the northern side of the Qianlishan granite mass .
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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 .