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特提斯喜马拉雅多重基性岩浆事件:追溯新特提斯洋的生存时限(英文) 被引量:3
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作者 zeng ling-sen1),gao li-e1),HE ke-jun2),tang suo-han1),guo chun-li2) 1).state key laboratory of continental tectonics and dynamics,institute of geology,chinese academy of geological sciences,beijing 100037,china 《地球学报》 EI CAS CSCD 北大核心 2012年第S1期72-73,共2页
Processes accompanied the breakup of continents spreading of ocean floor and continent-ocean transition could trigger large scale melting of the mantle beneath the continent as well as the ocean,and produce mafic magm... Processes accompanied the breakup of continents spreading of ocean floor and continent-ocean transition could trigger large scale melting of the mantle beneath the continent as well as the ocean,and produce mafic magmas with distinct 展开更多
关键词 TETHYAN Himalaya NEO-TETHYS India-Eurasia collision MAFIC MAGMATISM
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