新疆可可托海3号伟晶岩脉是阿拉尔花岗岩岩浆演化晚期的产物?

	新疆可可托海3号伟晶岩脉是阿拉尔花岗岩岩浆演化晚期的产物?
	张辉; 刘宏
	2013
Source Publication	矿物学报
Issue	S2
Keyword	伟晶岩脉阿拉尔岩浆演化出露面积主要岩性侵入接触形成时代红山嘴元素比值图定年
Subject Area	地球深部物质与流体作用地球化学
Indexed By	CSCD
Language	中文
Citation statistics
Document Type	期刊论文
Identifier	http://ir.gyig.ac.cn/handle/352002/5483
Collection	地球内部物质高温高压实验室_地球内部物质高温高压实验室_期刊论文
Recommended Citation GB/T 7714	张辉,刘宏. 新疆可可托海3号伟晶岩脉是阿拉尔花岗岩岩浆演化晚期的产物?[J]. 矿物学报,2013(S2).
APA	张辉,&刘宏.(2013).新疆可可托海3号伟晶岩脉是阿拉尔花岗岩岩浆演化晚期的产物?.矿物学报(S2).
MLA	张辉,et al."新疆可可托海3号伟晶岩脉是阿拉尔花岗岩岩浆演化晚期的产物?".矿物学报 .S2(2013).

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