中国地质(英文)2020,Vol.3Issue(2):299-313,15.DOI:10.31035/cg2020035
Genesis of pyroxenite veins in supra-subduction zone peridotites: Evidence from petrography and mineral composition of Egiingol massif (Northern Mongolia)
Genesis of pyroxenite veins in supra-subduction zone peridotites: Evidence from petrography and mineral composition of Egiingol massif (Northern Mongolia)
摘要
关键词
Pyroxenite vein/Boninite/Partial melting/Melt-rock interaction/Supra-subduction zone peridotite/Egiingol massif/Dzhida terrain/Central Asian Orogenic Belt/Northern MongoliaKey words
Pyroxenite vein/Boninite/Partial melting/Melt-rock interaction/Supra-subduction zone peridotite/Egiingol massif/Dzhida terrain/Central Asian Orogenic Belt/Northern Mongolia引用本文复制引用
Anas A.Karimov,Marina A.Gornova,Vasiliy A.Belyaev,Aleksander Ya.Medvedev,Nikolay V.Bryanskiy..Genesis of pyroxenite veins in supra-subduction zone peridotites: Evidence from petrography and mineral composition of Egiingol massif (Northern Mongolia)[J].中国地质(英文),2020,3(2):299-313,15.基金项目
The reported study was funded by RFBR according to the research project (18-35-00535) and IGC State Assignment Project (0350-2019-0008). (18-35-00535)