Mesoproterozoic high Fe-Ti mafic magmatism in western Shandong, North China Craton: Petrogenesis and implications for the final breakup of the Columbia supercontinent

	Mesoproterozoic high Fe-Ti mafic magmatism in western Shandong, North China Craton: Petrogenesis and implications for the final breakup of the Columbia supercontinent
	Peng, Touping ; Wilde, Simon A. ; Fan, Weiming ; Peng, Bingxia ; Mao, Yongsheng
刊名	Precambrian Research
	2013
卷号	235 页码:190-207
ISSN号	0301-9268
收录类别	SCI
语种	英语
公开日期	2014-10-14
内容类型	期刊论文
源URL	[http://ir.gig.ac.cn:8080/handle/344008/19151]
专题	中国科学院广州地球化学研究所
推荐引用方式 GB/T 7714	Peng, Touping,Wilde, Simon A.,Fan, Weiming,et al. Mesoproterozoic high Fe-Ti mafic magmatism in western Shandong, North China Craton: Petrogenesis and implications for the final breakup of the Columbia supercontinent[J]. Precambrian Research,2013,235:190-207.
APA	Peng, Touping,Wilde, Simon A.,Fan, Weiming,Peng, Bingxia,&Mao, Yongsheng.(2013).Mesoproterozoic high Fe-Ti mafic magmatism in western Shandong, North China Craton: Petrogenesis and implications for the final breakup of the Columbia supercontinent.Precambrian Research,235,190-207.
MLA	Peng, Touping,et al."Mesoproterozoic high Fe-Ti mafic magmatism in western Shandong, North China Craton: Petrogenesis and implications for the final breakup of the Columbia supercontinent".Precambrian Research 235(2013):190-207.