Premium
The Curves of Seven REE and Their Geological Significances of Porphyry Mo (Cu) Deposit of Chengba, Tibet
Author(s) -
SONG Xuebing,
SHI Zeming,
ZHANG Kailiang,
ZHANG Junji,
ZHU Feilin
Publication year - 2014
Publication title -
acta geologica sinica ‐ english edition
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.444
H-Index - 61
eISSN - 1755-6724
pISSN - 1000-9515
DOI - 10.1111/1755-6724.12374_50
Subject(s) - china , zhàng , chinese academy of sciences , library science , geochemistry , geology , geography , history , archaeology , computer science
The Chengba deposit adjacent to the Yarlung Zangbo suture zone is a porphyry deposit occurring at the southern edge of the eastern Gangdese metallogenic belt. The metallogenic element combinations in the Chengba deposit is Mo-Cu (Wang et al., 2014). This district is mainly located in Zedang region of the southeastern margin of the Gandese metallogenic belt, Aitchison based on the development of the area of Cretaceous tholeiitic and basalt andesite, which think the intra oceanic arc of new Tethys ocean subduction, accompanying by subduction of the Tethys ocean and collision between the Indian continental plate and the Asian plate collage in the southern margin of Lhasa block (Zhou et al., 2011).