东准噶尔北缘早石炭世构造体制转变:来自碱性花岗岩年代学和地球化学制约

	梁培; 陈华勇; 韩金生; 吴超; 张维峰; 赵联党; 王云峰
	东准噶尔北缘早石炭世构造体制转变:来自碱性花岗岩年代学和地球化学制约
Source Publication	大地构造与成矿学
ISSN	1001-1552
	2017
Volume	41 Issue:1 Pages:202-221
DOI	10.16539/j.ddgzyckx.2017.01.013
Language	中文
EI Accession Number	20171903652814
Indexed By	EI
Citation statistics
Document Type	期刊论文
Identifier	http://ir.gig.ac.cn/handle/344008/34688
Collection	同位素地球化学国家重点实验室
Recommended Citation GB/T 7714	梁培,陈华勇,韩金生,等. 东准噶尔北缘早石炭世构造体制转变:来自碱性花岗岩年代学和地球化学制约[J]. 大地构造与成矿学,2017,41(1):202-221.
APA	梁培.,陈华勇.,韩金生.,吴超.,张维峰.,...&王云峰.(2017).东准噶尔北缘早石炭世构造体制转变:来自碱性花岗岩年代学和地球化学制约.大地构造与成矿学,41(1),202-221.
MLA	梁培,et al."东准噶尔北缘早石炭世构造体制转变:来自碱性花岗岩年代学和地球化学制约".大地构造与成矿学 41.1(2017):202-221.

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