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地质科学  2001, Vol. Issue (3): 380-384    DOI:
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从成矿构造动力学探讨脉状金矿床成矿深度
陈柏林
中国地质科学院地质力学研究所, 北京, 100081
CALCULATION OF METALLOGENIC DEPTH OF LODE GOLD DEPOSITS FROM MINERALIZATION STRUCTURE-DYNAMICS
Chen Bailin
Institute of Geomechanics, Chinese Academy of Geological Scineces, Beijing 100081
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摘要 在综述国内外与韧性剪切带有关的脉状金矿床成矿动力学的新近研究成果后,根据成矿控矿构造动力学特征及其与成矿流体运移机制、矿物结晶特点的关系认为矿物结晶发生于地震微破裂导致成矿流体压力骤降后的低压力阶段,由矿物包裹体压力并按静岩压力梯度推算的成矿深度要明显小于矿床的实际成矿深度.本文提出一种新的成矿深度估算方法,其估算的成矿深度与目前大多数脉状金矿床中石英具有明显的韧性变形的特点相吻合.
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陈柏林
关键词脉状金矿床   成矿构造动力学   成矿深度   成矿流体运移机制   矿物包裹体压力     
Abstract: The recent research achievement of mineralization structure-dynamics about lode gold deposits related to ductile shear zone is first summarized in the paper. According to the relation between the structural pulsation of ore-forming and ore-controlling structures and the migratory mechanism of ore-forming fluid and the characteristics of mineral crystallization, the author considers that mineral only crystals at lower ore-forming fluid pressure that appears only just after the happening of a micro seismic fracturing. So the metallogenic depth calculated by means of mineral inclusion pressure divided by lithostatic pressure gradient is smaller than the actual depth. Then, the author puts forward a new calculating way, by which the calculated metallogenic depths are more-identical with the fact that the evident ductile deformation has been occurred in quartz of most lode gold deposits.
Key wordsLode gold deposits   Mineralization structure dynamics   Metallogenic depth   Migratory mechanism of ore-forming fluid   Mineral inclusion pressure   
收稿日期: 2000-04-12;
引用本文:   
陈柏林. 2001, 从成矿构造动力学探讨脉状金矿床成矿深度. 地质科学, (3): 380-384.
Chen Bailin. CALCULATION OF METALLOGENIC DEPTH OF LODE GOLD DEPOSITS FROM MINERALIZATION STRUCTURE-DYNAMICS[J]. Chinese Journal of Geology, 2001, (3): 380-384.
 
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[1] 吕古贤, 刘瑞珣, 王方正, 郭涛, 舒斌, 夏林, 刘杜娟. 关于成岩成矿深度构造校正测算的理论基础、方法和实例[J]. 地质科学, 2003, (4): 546-563.
[2] 陶琰, 高振敏, 金景福, 曾令交. 湘中锡矿山式锑矿成矿地质条件分析[J]. 地质科学, 2002, (2): 184-195.
 
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