Melted Rocks under the Microscope: Microstructures and Their Interpretation
Melted Rocks under the Microscope: Microstructures and Their Interpretation
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DOI：
10.2113/gselements.7.4.247
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发表时间：
2011-08
期刊：
影响因子：
4.5
通讯作者：
M. Holness;B. Cesare;E. Sawyer
中科院分区：
文献类型：
--
作者：
M. Holness;B. Cesare;E. Sawyer
在区域变质作用后经历了数百万年的冷却和折返的岩石中，认识到以前存在的熔体通常依赖于对只有在显微镜下才能看到的颗粒尺度结构的正确解释。这些结构的演变过程中的反熔，后来，逆行冷却可以理解使用的概念来自实验模拟和材料科学。
Recognising the former presence of melt in rocks which have undergone cooling and exhumation over millions of years following regional metamorphism commonly relies on the correct interpretation of grain-scale structures visible only under the microscope. The evolution of these structures during prograde melting and, later, retrograde cooling can be understood using concepts derived from experimental simulation and materials science.