机译:纪伊半岛西部船冈山地区的高压石榴石角闪岩及三叶川川带的榴辉岩相变质程度
Institute of Geology and Geoinformation, National Institute of Advanced Industrial Science and Technology (AIST), Central 7, Tsukuba 305-8567, Japan,Department of Earth and Planetary Sciences, Nagoya University, Chikusa-ku, Nagoya 464-8602, Japan;
Institute of Geological Sciences, Polish Academy of Sciences INGPAN, Podwale 75, 50-449 Wroclaw, Poland,Department of Earth and Planetary Sciences, Nagoya University, Chikusa-ku, Nagoya 464-8602, Japan;
Department of Earth and Planetary Sciences, Nagoya University, Chikusa-ku, Nagoya 464-8602, Japan;
Eclogite facies; Funaokayama unit; Garnet amphibolite; P-Tpath; Sanbagawa belt;
机译:纪伊半岛西部船冈山地区的高压石榴石角闪石及三叶川川带的榴辉岩相变质程度
机译:日本三河川带的榴辉岩相变质作用的实际范围:拉曼显微探针研究石英残余压力的新证据
机译:日本三河川带的榴辉岩相变质作用的实际范围:来自拉曼微探针研究石英残余压力的新证据
机译:巴基斯坦西北喜马拉雅山上卡格汉河谷高地特提斯喜马拉雅的构造:喜马拉雅带早期碰撞,高压(榴辉岩相)变质作用的含义。
机译:来自Funaokayama单位的高压石榴石倒置,西部Kii半岛和Sanbagawa皮带中的eClogite相变质的程度