Diagenesis-Mineralization and Ore Prospecting of the Yangla Copper Deposit, Yunnan Province, Southwest China

The large-scale Yangla copper deposit, located in the central part of the Sanjiang Tethys polymetallic belt, is structurally controlled by the Jinsha River Fault and Yangla Fault. This deposit consists of seven ore blocks, including the Beiwu, Nilv, Jiangbian, Linong, Lunong, Tongjige and Jiaren. Th...

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Published inActa geologica Sinica (Beijing) Vol. 89; no. 5; p. 1766
Main Authors Bo, LI, Zhilong, HUANG, Jiaxi, ZHOU, Guofu, ZOU, Guo, TANG, Yuedong, LIU
Format Journal Article
LanguageEnglish
Published Richmond Blackwell Publishing Ltd 01.10.2015
Wiley Subscription Services, Inc
Faculty of Land Resource Engineering, Kunming University of Science and Technology, Kunming 650093,Yunnan, China%State Key Laboratory of Ore Deposit Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang 550081, Guizhou, China%Kunming Prospecting Design Institute of China Nonferrous Metals Industry, Yunnan Copper Industry (Group) Co.Ltd., Kunming 650051, Yunnan, China%Yunnan Diqing Mining Co.Ltd., Shangrila 674400, Yunnan, China
Kunming Prospecting Design Institute of China Nonferrous Metals Industry, Yunnan Copper Industry (Group) Co.Ltd., Kunming 650051, Yunnan, China
State Key Laboratory of Ore Deposit Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang 550081, Guizhou, China
EditionEnglish ed.
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Summary:The large-scale Yangla copper deposit, located in the central part of the Sanjiang Tethys polymetallic belt, is structurally controlled by the Jinsha River Fault and Yangla Fault. This deposit consists of seven ore blocks, including the Beiwu, Nilv, Jiangbian, Linong, Lunong, Tongjige and Jiaren. The Cu metal prospective reserves of the Yangla deposit are above 1 million tons. There are widely distributed Indosinian granodiorite and also many gabbro-diabase dikes and few quartz porphyries exposed in the Yangla ore district. The ore-hosting rocks are diopsode-garnet skarn, sericitie sandy slate and metamorphic quartz sandstone of the first member of the Devonian Linong Formation. Ore bodies occur as layered, stratoid, lenticular and veined shapes, and are strictly controlled by rocks, strata and structures.
Bibliography:11-2001/P
The large-scale Yangla copper deposit, located in the central part of the Sanjiang Tethys polymetallic belt, is structurally controlled by the Jinsha River Fault and Yangla Fault. This deposit consists of seven ore blocks, including the Beiwu, Nilv, Jiangbian, Linong, Lunong, Tongjige and Jiaren. The Cu metal prospective reserves of the Yangla deposit are above 1 million tons. There are widely distributed Indosinian granodiorite and also many gabbro-diabase dikes and few quartz porphyries exposed in the Yangla ore district. The ore-hosting rocks are diopsode-garnet skarn, sericitie sandy slate and metamorphic quartz sandstone of the first member of the Devonian Linong Formation. Ore bodies occur as layered, stratoid, lenticular and veined shapes, and are strictly controlled by rocks, strata and structures.
ark:/67375/WNG-4RLPXM0B-Q
ArticleID:ACGS12579
istex:0DEE66F1491D5F37280822DF65C21811F56FB822
ISSN:1000-9515
1755-6724
DOI:10.1111/1755-6724.12579