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地质论评  2005 

碳酸岩与铂族元素地球化学

Keywords: 碳酸岩铂族元素地球化学PGE源区特征

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Abstract:

碳酸岩(carbonatite)被视为一种研究大陆地幔地球化学的“探针岩石”,通过对这类岩石的研究,在探讨地幔组成与演化、地幔交代作用与不均一性以及岩浆形成的动力学背景、岩浆来源及演化和有关矿产的成矿作用等方面,具有重要的理论意义和实际价值。铂族元素(Platinum―groupelements,简称PGE)在研究核-幔分异、地幔组成与演化以及幔源岩石(主要为基性-超基性岩)形成的大地构造背景、岩浆起源及演化,以及探讨K/T界线与陨石撞击事件等方面具有重要意义。本文在概述国内外碳酸岩和PGE地球化学研究现状的基础上,结合地质事实和地球化学研究成果,认为碳酸岩熔体具有一定携带PGE的能力,可利用PGE地球化学来探讨碳酸岩的源区特征和岩浆形成与演化过程;同时指出,碳酸岩PGE地球化学研究过程中还存在许多悬而未决的科学问题。

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