Extremely low ^3He/^4He and relatively low ^<40>Ar/^<36>Ar ratios observed in ultramafic mantle xenoliths from far eastern Siberia : Evidence for incorporation of recycled components into the subcontinental mantle.

Extremely low ^3He/^4He and relatively low ^<40>Ar/^<36>Ar ratios observed in ultramafic mantle xenoliths from far eastern Siberia : Evidence for incorporation of recycled components into the subcontinental mantle.
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在西伯利亚远东的超镁铁质地幔捕虏体中观察到极低的^3He/^4He和相对较低的^<40>Ar/^<36>Ar比率:回收成分并入次大陆地幔的证据。

DOI:
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发表时间:
2004
期刊:
Chemical Geology 207
影响因子:
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通讯作者:
Arai S.
Arai S.
中科院分区:
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文献类型:
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作者:
Yamamoto J.;Kaneoka I.;Nakai S.;Kagi H.;Prikhod'ko V.S.;Arai S.

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