湘中地区锑矿区域成矿模式
Mineral Resources and Geology（2017）
Abstract
从物理化学条件中反映研究区内锑矿成矿物质主要来源于重熔型岩浆岩,次为地层本身锑元素;成矿热液沿构造裂隙在多期构造作用下向上运移,并经历碱性-酸性-碱性演化、古水热循环萃取作用,在隆起带中部、边部以及拗陷盆地中的次级隆起区富集成矿.
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Key words
New Huaxia structure,remelting magmatic rock,ore-forming elements,paleo-hydrothermal cy-cle,metallogenic model
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