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辽宁北地金矿地球化学特征 被引量:2
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作者 朴寿成 于泽新 +2 位作者 李清泉 张博文 师磊 《世界地质》 CAS CSCD 2008年第2期172-177,共6页
北地金矿产于燕山期石英二长岩与太古宙建平群小塔子沟组变质杂岩的内接触带,主成矿阶段的温度为240~360℃,盐度(NaCl)为1%~6%,成矿压力为105.5×106~156×106Pa,矿化深度为3.52~6.24km,属中温中深成脉状热液矿床。从矿石... 北地金矿产于燕山期石英二长岩与太古宙建平群小塔子沟组变质杂岩的内接触带,主成矿阶段的温度为240~360℃,盐度(NaCl)为1%~6%,成矿压力为105.5×106~156×106Pa,矿化深度为3.52~6.24km,属中温中深成脉状热液矿床。从矿石的石英及其包裹体获得的δD分别为-88.44×10-3和-88.96×10-3,δ18O分别为5.08×10-3和5.11×10-3,成矿流体主要来源于岩浆水。燕山期石英二长岩形成过程和区内广泛分布的太古宙变质杂岩都可能提供了部分成矿物质。矿石的石英流体包裹体均一温度和盐度都有双峰现象,均一温度峰值分别为160℃~220℃和280℃~300℃,盐度(NaCl)的峰值分别为3%~4%和7%~8%,矿质的沉淀、富集可能与流体的不混溶有关。 展开更多
关键词 北地金矿 流体包裹体 微量元素 氢、氧同位素 地球化学
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NUMERICAL SIMULATION OF THE STRUCTURAL STRESS FIELD OF BEIYA GOLD DEPOSIT
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作者 MA Deyun and GAO Zhenmin(Open Laboratory of Ore Deposit Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang 550002, China Department of Earth Science, Kunming University of Scienceand Technology, Kunming 650093, China) 《Geotectonica et Metallogenia》 2003年第1期91-103,共13页
Based on the study about the geological background of Beiya Gold Deposit, numerical simulation was conducted about the three-dimensional structural stress field for Beiya Gold Deposit by applying finite element theory... Based on the study about the geological background of Beiya Gold Deposit, numerical simulation was conducted about the three-dimensional structural stress field for Beiya Gold Deposit by applying finite element theory and by employing a linear elasticity model. Results of the simulation indicate that the Beiya syncline is a faulted basin, and a hidden fracture occurs in the west wing of the syncline.Under the action of the EW-trending compressive force, four nearly NS-trending fractures (groups) were generated in the stress stretching areas of the two wings of the syncline, and these fractures constitute favorable tectonic positions for the upward intrusion of porphyry magma and the occurrence of Au-Pb-Zn polymetallic deposits. 展开更多
关键词 Beiya gold deposit structural stress field numerical simulation
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