Mineral Geochemical Characteristics and Indication Significance of Biotite-Rutile in the Gabbro Intrusions in the Yinmin Iron-Copper District, Yunnan

<正>1 Introduction After the Dongchuan Orogenic movement(Hudsonian Orogeny,ca.1800 Ma±),the tectonic basement layer of the continental crust on the Yangtze massif could have been formed.And then tectonic-magmatic emplacement

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Bibliographic Details
Published in:Acta geologica Sinica (Beijing) 2017-05, Vol.91 (S1), p.224-226
Main Authors: SUN, Zijian, FANG, Weixuan, Jia, Lu, GUO, Yuqian, SONG, Lihong
Format: Article
Language:English
Subjects:
Biotite
Copper
Gabbro
Geochemistry
Indication
Iron
Rutile
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Summary:<正>1 Introduction After the Dongchuan Orogenic movement(Hudsonian Orogeny,ca.1800 Ma±),the tectonic basement layer of the continental crust on the Yangtze massif could have been formed.And then tectonic-magmatic emplacement
ISSN:1000-9515
1755-6724
DOI:10.1111/1755-6724.13267