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Fluid Inclusions Studies And Geological Significance In The Xuebaoding W‐Sn‐Be Deposit, Sichuan
Author(s) -
WU Dawei,
LI Baohua,
DU Xiaofei
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 - 10.1111/1755-6724.12379_55
Subject(s) - chinese academy of sciences , library science , theology , history , philosophy , china , computer science , archaeology
The Xuebaoding deposit is located at Songpan-Garze orogenic belt of the northwest margins of Yangtze plate. It is controlled by the secondary Ziboshan dome structure which is located in the core of Moziping-Nacai overturned synclinorium. The exposure strata was Triassic Zhuwo Formation (T3zh). It is the main orebearing strata of Xuebaoding mining area which is made up slate, schist and marble. The granite body was intruded in the Triassic system at Late Indosinian as stock and dike, the lithology is muscovite monzogranite and muscovite granodiorite.