首页> 外文会议>Joint Sixth Biennial Sga-Seg Meeting, 6th, Aug 26-29, 2001, Krakow/Poland >Phosphorus and rubidium in alkali feldspars -tools for better understanding of the late- to post-magmatic evolution of fractionated granites
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Phosphorus and rubidium in alkali feldspars -tools for better understanding of the late- to post-magmatic evolution of fractionated granites

机译:碱性长石中的磷和id-用于更好地了解分馏花岗岩从后期到岩浆演化的工具

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摘要

Absolute contents and distribution patterns of phosphorus and rubidium in alkali feldspars were studied in detail in two peraluminous granite systems being quite different in intensity of influence of the late-to post-magmatic fluids - Podlesi (Bohemia) and Beauvoir (France). Rubidium is firmly bound in the Kfs-lattice and preserves well its magmatic signature during post-magmatic processes. In contrast, phosphorus can be easily released from the feldspar lattice and P-content serves as a sensitive indicator of the late- and/or post-magmatic fluid-related reactions.
机译:在两个晚辉岩后流体影响强度差异很大的两个高铝花岗岩系统中详细研究了碱性长石中磷和id的绝对含量和分布模式-波德西(Bohemia)和波伏娃(法国)。 post牢固地结合在Kfs晶格中,并在后岩浆作用过程中很好地保留了其岩浆特征。相反,磷很容易从长石晶格中释放出来,P含量可作为岩浆后期和/或岩浆后流体相关反应的敏感指标。

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