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《Chinese Geology》 2004-02
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Ore-controlling structure and its control over gold mineralization in the Baolun gold deposit, Hainan

CHEN Bai-lin1, LI Zhong-jian1, DONG Cheng1, DING Shi-jiang2, SU Bin1, LIAO Xiang-jun2, DONG Fa-xian1, FU Yang-rong2 (1. Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing 100081, China; 2. Hainan Institute of Geology and Exploitation, Haikou 570001, Hainan, China)  
The Baolun gold deposit, as one of the large gold deposits found in Hainan Province recently, is a structurally controlled, magmatic-hydrothermal gold deposit formed in the Indosinian. In the gold district there outcrop the Lower Silurian Tuolie Formation low-grade metamorphic series and Indosinian red clastic rocks, and in addition Indosinian granite is distributed on its northwest side. The NNE-trending Haogangling fault and the NNW-trending fracture zone in the hanging wall of the fault form the basic structural framework of the ore district. Magnetic fabric analysis indicates that: flattening deformation predominates in phyllite of the district; the principal compressive stress is oriented in a nearly E-W direction; the structural deformation was stronger before the mineralization thermal event and weaker after mineralization. The structural stress field in the mineralization stage is featured by E-W extension (the principal compressive stress was oriented in a N-S direction). The NNW-trending fracture zone is the main ore-hosting (ore-bearing) structure, which exerts an important controlling effect on the shape, attitude, scale and special distribution of the gold orebodies.
【Fund】: 原地质矿产部定向研究基金项目(地科定97-16)资助。
【CateGory Index】: P618.51
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