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论太古宙含金剪切带的成矿机制 被引量:11

ON THE MECHANISM OF MINERALIZATION IN ARCHAEAN GOLD-BEARING SHEAR ZONE
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摘要 含金剪切带是长期发展演化着的宏大动力学体系。其成矿过程是个动态过程,受时间、空间和动力学、热力学等因素综合控制。含金剪切带发生于强变质变形高峰期或稍晚,含金石英脉是它发展演化的中晚期产物。含金剪切带不仅具有导矿、容矿作用,而且也是重要的造矿因素,在金的成矿作用链中导致矿化发生、促进矿化向成矿转化和控制就位起极重要的作用。绿岩的含金性、变质变形及伴随的重熔岩浆活动是金成矿必要条件,而含金剪切带及伴随的钾质花岗岩和碱交代、酸交代作用是金成矿的充要条件。 The gold-bearing shear zone is a great dynamic system which is develo- ped for a long time. The process of mineralization is controlled comprehensively by dynamics, thermodynamics, time and space. The gold-bearing shear zone was developed duriag or after the peak of major metamophism developed during or after the pfeak of major metamophism and deformation, the gold bearing quartz vein was accurred in late stage of evolution of shear zone. The shear zone played an important role in the gold deposits forming process.Gold bearing greenstone, metamorphism, deformation and associated magma activity are neccessary to gold mineralization. Shear zone, alkaline metasomatism and acid metasomatism are also sufficient and necessary to the gold mineralization.
作者 刘劲鸿
出处 《长春地质学院学报》 CSCD 1991年第2期156-166,共11页
关键词 剪切带 含金 成矿 太古宙 gold-bearing shear zone,mineralization, sufficient and necessary condition, Archaean
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参考文献5

  • 1刘劲鸿.吉林省夹皮沟—金城洞花岗绿岩带中金矿床的形成时代[J].吉林地质,1989(4):58-70. 被引量:7
  • 2J.V.Hamilton,C.Jay Hodgson,李上森.印度科拉尔金矿田的矿化和构造[J]国外前寒武纪地质,1988(04).
  • 3R. Mason,N. Melnik,田书文.加拿大安大略省提敏斯麦克因蒂尔—霍林格尔杂岩的太古宙含金矿系剖析[J]国外前寒武纪地质,1988(02).
  • 4於崇文.成矿作用与耗散结构[J]地质学报,1987(04).
  • 5G.J.Hinse,张立生.据安大略和魁北克的拉尔德莱克“破裂”论太古代脉型金矿床的成因[J]地质地球化学,1987(12).

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