Relict Majoritic Garnet Microstructures from Ultra-Deep Orogenic Peridotites in Western Norway
Relict Majoritic Garnet Microstructures from Ultra-Deep Orogenic Peridotites in Western Norway
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DOI：
10.1093/petrology/42.1.117
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发表时间：
2001
影响因子：
3.9
通讯作者：
H. Roermund;M. Drury;A. Barnhoorn;A. D. Ronde
中科院分区：
文献类型：
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作者：
H. Roermund;M. Drury;A. Barnhoorn;A. D. Ronde
使用肉眼、光学、电子光学和共焦激光（荧光）显微镜技术对来自挪威西部片麻岩地区奥特罗伊的 Mg-Cr 型造山石榴石橄榄岩的原粒状和（或等聚多键）石榴石进行了研究。原粒状和碎斑石榴石包含前者的微观结构证据，包括单个原粒状或碎斑石榴石中最大辉石总体积百分比
Protogranular, and (or equant-poly-KEY gonal) garnet from Mg–Cr type orogenic garnet peridotites, Otrøy, Western Gneiss Region, Norway, have been studied using naked eye, light-optical, electron-optical and confocal laser (fluorescence) microscopy techniques. Protogranular and porphyroclastic garnets contain microstructural evidence for the former consists of for maximum pyroxene total volume percentage in one single protogranular or porphyroclastic garnet