机译:陨石单板逐渐混合到地球早期的深地幔中
Department of Geology, University of Oulu, Linnanmaa, 90014 Oulu, Finland Centre for Exploration Targeting, University of Western Australia, 35 Stirling Highway, Crawiey 6009, Australia;
CSIRO, 26 Dick Perry Avenue, Kensington 6151, Western Australia, Australia;
Research School of Earth Sciences, Australian National University, Canberra 0200, Australian Capital Territory, Australia;
Centre for Exploration Targeting, University of Western Australia, 35 Stirling Highway, Crawiey 6009, Australia;
Geological Survey of Finland, Betonimiehenkuja 4, Espoo 02151, Finland Department of Geology, University of Helsinki, Gustaf Haellstroemin katu 2a, Helsinki 00014, Finland;
Sciences Appliques, Universite du Quebec a Chicoutirni, Chicoutimi G7H 2B1, Quebec, Canada;
Geological Survey of Western Australia, 100 Plain Street, East Perth 6004, Western Australia, Australia;
机译:Os-186 / Os-188在上地幔橄榄岩中的变化:原始上地幔的Pt / Os比值受到约束,并且对后期单板增生和地幔混合时间尺度有影响
机译:保存在古生岩石中的地球上层-中层地幔的钌同位素痕迹
机译:钯和铂的高压分配在地球幔中形成晚软骨状单板的证据
机译:地球通过使用煤灰通过深处混合方法使用纸桩和自支撑的地球挡土墙保持挖掘
机译:地球化学,地震学和混合研究对地幔结构的限制:对地球地幔成分异质性的数值研究。
机译:铁对地球深地幔晶格热导率的影响及其对地幔动力学的影响
机译:铁陨石中的太阳惰性气体表明陆地地幔签名来自地球的核心