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- W3140436405 abstract "Nd 比率(0.51271-0.51295 ) 。从地点 794 罐头的暗岩根据他们的 stratigraphic 水平被划分成上面、中间、更低的暴烈的岩石(UVR， MVR，和 LVR ) 。MVR geochemically 从弄空的披风被导出，而 UVR 和 LVR 从 nondepleted 发源并且相对从 subducted 太平洋板液体和沉积与贡献充实披风来源。geothermobarometers 的使用显示为 UVR 和 LVR (6.25-11.19 kbar ) 的结晶化压力比 MVR (3.48-5.84 kbar ) 的显著地高。UVR 和 LVR 可能被导出从低度(5%-10%) 尖晶石 lherzolite 的部分融化，当 MVR 与部分融化的高度(10%-20%) 从更浅的披风来源发源时。另外，样品的 geochemical 特征与更年轻的年龄(13-17 妈) 一致， MVR 和老年(17-23 妈) 并且稍微的弄空的作文充实 UVR 和 LVR 的作文。因此，在披风的时间的变化采购原料从对幼仔旧、充实、弄空并且随后到旧并且 nondepleted 可能与进步 lithospheric 扩展被联系了并且变瘦，以及多样的 asthenospheric upwelling 和拉开的至少二个事件在大和民" @default.
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- W3140436405 date "2015-01-01" @default.
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- W3140436405 title "Geochemical Characteristics of Volcanic Rocks from ODP Site 794,Yamato Basin： Implications for Deep Mantle Processes of the Japan Sea" @default.
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