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花岗岩成因机制研究综述
引用本文:宋子新 钱祥麟. 花岗岩成因机制研究综述[J]. 地质科技情报, 1996, 15(3): 19-25
作者姓名:宋子新 钱祥麟
作者单位:北京大学地质学系
摘    要:花岗岩的形成与原岩成分及热源有关,且受流体的影响。形成机制主要有俯冲作用、大陆地壳的增厚、板底垫托、拆沉作用、板块破碎、地幔柱、减压熔融作用、助熔作用等。在变形、浮力、重力等作用下,熔体从母岩中分离,分离受粘度、流体、变形、渗透性等因素的影响。花岗质岩浆的侵位机制虽然较多,但主要是剪切带及断裂为其提供了上升、侵位的通道和空间。

关 键 词:花岗岩 熔融作用 形成机制 俯冲作用 上升机制 侵位机制

ON THE FORMATION MECHANISM OF GRANITE:A REVIEW
Song Zixin Qian Xianglin. ON THE FORMATION MECHANISM OF GRANITE:A REVIEW[J]. Geological Science and Technology Information, 1996, 15(3): 19-25
Authors:Song Zixin Qian Xianglin
Abstract:The generation of granite is related to the source compositions and heat sources,and influenced by the fluid.The mechanisms of granitic melting include subduction,crustal thickening followed by erosional exhumation or extensional thinning,mafic magma underplating delamination,slab break off, mantle plume,decompression melting,fluxing, etc. Under the deviatoric stresses and the effect of a few factors,such as viscosity,fluid,deformation,percolation,the melt segregates from the source region, and ascends and emplaces along the shear zones and fractures.
Keywords:granite  generation  melting  segregation and aggregation  ascent and emplacement  
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