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Metamorphism of thought about igneous rock textures

机译:火成岩质地思想的变质

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摘要

The standard interpretation of textures in igneous rocks was largely set over a century ago, when pioneering petrographers such as H.C. Sorby (1858) and L.V. Pirsson (1909) systematized the study of rocks in thin section and hand sample. Numerous classic works since then have built on this foundation (e.g. Johannsen 1931–1939; Williams et al. 1954), producing the framework used in classroom and practice alike. This issue contains a set of articles that challenge some of the fundamental assumptions and interpretations of this framework. As igneous petrologists, we wish to emphasize the similarities of processes between plutonic rocks and high-grade metamorphic rocks in the development of texture and the formation of features such as igneous modal layering and metamorphic layering.
机译:火成岩岩石纹理的标准解释很大程度上是在一个世纪前,当时H.C.索比(1858)和L.V. Pirsson(1909)系统地研究了薄片和手部样品中的岩石。从那时起,许多经典作品都建立在这个基础上(例如Johannsen 1931-1939; Williams等人1954),产生了课堂和实践中使用的框架。本期包含一组文章,这些文章挑战了该框架的一些基本假设和解释。作为火成岩岩石学家,我们希望强调深成岩与高级变质岩在构造发展和形成特征如火成岩模态层和变质层方面的相似之处。

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