島根大学教育学部紀要. 自然科学

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島根大学教育学部紀要. 自然科学 22 2
1988-12-26 発行

沸石脈生成に伴う岩石の変質作用 : 特に深成岩類の深層風化と関係して

Formation of zeolite veins and rock alteration, with special reference to deeper seated weathering processes
三浦 清
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内容記述(抄録等)
During the final stages of consolidation of granitic magma the volatile-rich residualsolutions may induce widespread alterations, so that pre-existed minerals are veind or replaced by new ones.
Laumontite and stilbite resulting from these processes occuurs generally in veins cutting plutonic rock masses, and these zeolites are also in association with albite and hydrogrossularite mineralization, especially in granodiorite masses.
The alteration zones along zeolite veins can be a very effective mechanical agent of rock weathering and thus allowing other weathering agencies accese to the interior of the rock is a phenomenon frequently observed.
The significance of these alteration to deeper seated weathering are discussed in this paper.