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机译:橄榄石宿主溶液的挥发性浓度来自西伯利亚陷阱的梅梅科矿石和甜瓜泥炭液:助势相关的高TI,高镁岩岩
Russian Acad Sci Siberian Branch Inst Earths Crust 128 Lermontov St Irkutsk 664033 Russia;
Univ Minnesota Dept Earth Sci 116 Church St SE Minneapolis MN 55455 USA;
Univ Tasmania Sch Phys Sci Hobart Tas 7001 Australia;
Carnegie Inst Sci Geophys Lab 5251 Broad Branch Rd NW Washington DC 20015 USA;
Russian Acad Sci Siberian Branch Inst Earths Crust 128 Lermontov St Irkutsk 664033 Russia;
Russian Acad Sci Geol Inst 7 Pyzhevsky Lane Moscow 119017 Russia;
Russian Acad Sci Siberian Branch AP Vinogradov Inst Geochem 1A Favorkogo St Irkutsk 664033 Russia;
Russian Acad Sci Siberian Branch Sobolev Inst Geol &
Mineral Koptyuga Av. 3 Novosibirsk 630090 Russia;
Russian Acad Sci Siberian Branch Sobolev Inst Geol &
Mineral Koptyuga Av. 3 Novosibirsk 630090 Russia;
Russian Acad Sci Siberian Branch Sobolev Inst Geol &
Mineral Koptyuga Av. 3 Novosibirsk 630090 Russia;
Siberian Traps; Meimechite; Melanephelinite; Olivine; Melt inclusion;
机译:橄榄石宿主溶液的挥发性浓度来自西伯利亚陷阱的梅梅科矿石和甜瓜泥炭液:助势相关的高TI,高镁岩岩
机译:哥伦比亚河洪水玄武岩和俄勒冈高原相关熔岩中橄榄石包裹的熔体包裹物中的挥发性浓度:对岩浆成因的启示
机译:大火众省的高TI和低TI岩浆的起源,来自熔融包容性散布元素和SR-PB同位素的emeishan大火省的见解
机译:低TI从东南部的西伯利亚陷阱大火省融化:富含水的地幔源的证据吗?