A suit of metamorphic rocks experienced amphibolite and partly granulite facies metamorphism exposed on the Lhasa block,which are recognized as the basement of the Lhasa block named as Nyainqentanglha Group in
The Kuda ophiolite belongs to the early Paleozoic ophiolite belt in Western Kunlun Mountains and is composed of metamorphic peridotites,cumulate peridotites,mafic volcanic rocks and quartzites(Li et al.,
基金funded by grants from the NSF China(No.41572051)the China Geological Survey(No.DD20160022-01)project from Institute of Geology,Chinese Academy of Geological Sciences(J1518)
文摘A suit of metamorphic rocks experienced amphibolite and partly granulite facies metamorphism exposed on the Lhasa block,which are recognized as the basement of the Lhasa block named as Nyainqentanglha Group in
基金supported by National Natural Science Foundation Project(grant number 41302051)Shaanxi Province Science Technology Research Development Plan Project(grant number 2014JM2-4037)National Sci-Tech Support Plan Project(grant number 2011BAB06B05-02)
文摘The Kuda ophiolite belongs to the early Paleozoic ophiolite belt in Western Kunlun Mountains and is composed of metamorphic peridotites,cumulate peridotites,mafic volcanic rocks and quartzites(Li et al.,
