YAO Peng1, 2, WANG Quan-hai3, LI Jin-gao4. Ore and ore resource prospects of the Jiama-Qulong ore concentration area, Tibet[J]. Geology in China, 2002, (2): 197-202.
Citation: |
YAO Peng1, 2, WANG Quan-hai3, LI Jin-gao4. Ore and ore resource prospects of the Jiama-Qulong ore concentration area, Tibet[J]. Geology in China, 2002, (2): 197-202.
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Ore and ore resource prospects of the Jiama-Qulong ore concentration area, Tibet
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1.Institute of Geology and Mineral Resources, Chengdu 610082, Sichaun, China; 2.Chengdu University of Technology, Chengdu 610059, Sichuan, China; 3.Southwestern China Division of Project Management, China Geological Survey, Chengdu 610082, Sichuan, China ; 4.Tibet Bureau of Geology and Geological Exploration and Development, Lhasa 850000, Tibet, China
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Abstract
Abstract: The Jiama-Qulong ore concentration area, Tibet, 124km long and 69 km wide, is located in the east-central part of the Mid-Late Jurassic-Paleogene Gangdise continental-margin volcanic-magma arc. Through recent geological survey, mineral exploration and ore deposit study, the authors found several ore concentration areas in the Gangdise continental-margin volcanic-magma arc, of which the Jiama-Qulong ore concentration area is one of the important copper polymetallic ore concentration areas in the arc. The deposits of this area are represented by the large Jiama-Qulong copper polymetallic ore deposit which is being exploited. In addition, they also found a number of very promising deposits and mineralization occurrences such as Oulong South, Oulong North, Dirima, Songduoxiong, Lakang'e and Xiangbeishan. They are characterized by unique mineralization types and a variety of genetic types, suggesting that they are products of different stages of evolution of the Gangdise continental-margin volcanic-magma arc. These different types of deposit are concentrated in a certain areal extent and have primarily shown and formed an important ore concentration area with great ore potential and a certain ore prospect in the Gangdise continental-margin volcanic-magma arc. The authors believe that through further work this area is expected to become another nonferrous mineral resource base in western China.
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