Association of hydrothermal plagioclase alteration with micropores in a granite: Petrographic indicators to evaluate the extent of hydrothermal alteration
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引用次数: 0
Abstract
This study presents the use of petrographic plagioclase alteration indicators as a new method for quantitatively evaluating the extent of plagioclase alteration within granites, using the Toki granite, central Japan, as an example. The new petrological indicator enables us to discuss the similarities/di ff erences in the extent of alteration within a rock body and between rock bodies. Alteration indicators and areal fractions of microvoids in the plagioclase grains were obtained through the analysis of backscattered electron images. The volume of the micropores in the altered plagioclase was estimated using the areal fraction of microvoids in the grains. The plagioclase alteration indicators were obtained as the ratio between the alteration product domain and the original plagioclase domain. We found positive correlations between the plagioclase alteration and biotite chloritization indicators presented in Yuguchi et al. (2021), indicating that each alteration indicator can be used independently as a representative value for the sample. The positive correlations between the areal fraction of microvoids in the altered plagioclase and the alteration indicator in the samples and petrographic observations indicated the following: 1) the altered plagioclase contains the incipient micropores and the alteration micropores, 2) the incipient micropores, which were caused by the dissolution of plagioclase during the incipient stage of plagioclase alteration, acted as a pathway of hydrothermal fl uid within the plagioclase, resulting in alteration progress, and 3) the hydrothermal alteration resulted in the production of new alteration micropores. In the Toki granite, the progress of plagioclase alteration is essentially dominated by the progress of biotite chloritization. The progress of biotite chloritization essentially in fl uenced the progress of plagioclase
本文以日本中部Toki花岗岩为例,提出了利用岩相斜长石蚀变指标定量评价花岗岩内斜长石蚀变程度的新方法。新的岩石学指标使我们能够讨论一个岩体内和岩体之间蚀变程度的异同。通过背向散射电子图像分析,获得了斜长石颗粒的蚀变指标和微孔的面积分数。蚀变斜长石中微孔的体积是用颗粒中微孔的面积分数来估计的。斜长石蚀变指标为蚀变产物域与原斜长石域之比。我们发现Yuguchi et al.(2021)提出的斜长石蚀变与黑云母绿泥化指标之间存在正相关关系,表明每种蚀变指标都可以独立作为样品的代表性值。蚀变斜长石中微孔的面积分数与样品中的蚀变指标和岩石学观察呈正相关,表明:蚀变斜长石包含有初始微孔和蚀变微孔;2)初始微孔是斜长石蚀变初期溶蚀作用形成的,是热液流体在斜长石内部的通道,导致蚀变进程;3)热液蚀变导致新的蚀变微孔的产生。在东木花岗岩中,斜长石蚀变的过程主要以黑云母绿岩化的过程为主。黑云母绿泥化作用的进展基本上影响了斜长石的进展
期刊介绍:
The Journal of Mineralogical and Petrological Sciences (JMPS) publishes original articles, reviews and letters in the fields of mineralogy, petrology, economic geology, geochemistry, planetary materials science, and related scientific fields. As an international journal, we aim to provide worldwide diffusion for the results of research in Japan, as well as to serve as a medium with high impact factor for the global scientific communication
Given the remarkable rate at which publications have been expanding to include several fields, including planetary and earth sciences, materials science, and instrumental analysis technology, the journal aims to encourage and develop a variety of such new interdisciplinary scientific fields, to encourage the wide scope of such new fields to bloom in the future, and to contribute to the rapidly growing international scientific community.
To cope with this emerging scientific environment, in April 2000 the journal''s two parent societies, MSJ* (The Mineralogical Society of Japan) and JAMPEG* (The Japanese Association of Mineralogists, Petrologists and Economic Geologists), combined their respective journals (the Mineralogical Journal and the Journal of Mineralogy, Petrology and Economic Geology). The result of this merger was the Journal of Mineralogical and Petrological Sciences, which has a greatly expanded and enriched scope compared to its predecessors.