Geochemical constraints on CO2-rich mantle source for the Kocebu Seamount, Magellan Seamount chain in the western Pacific
Author:
Publisher
Springer Science and Business Media LLC
Subject
Water Science and Technology,Oceanography
Link
https://link.springer.com/content/pdf/10.1007/s00343-020-0013-x.pdf
Reference55 articles.
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3. Chazot G, Menzies M A, Harte B. 1996. Determination of partition coefficients between apatite, clinopyroxene, amphibole, and melt in natural spinel lherzolites from Yemen: implications for wet melting of the lithospheric mantle. Geochimica et Cosmochimica Acta, 60(3): 423–437, https://doi.org/10.1016/0016-7037(95)00412-2.
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5. Dasgupta R, Hirschmann M M, Smith N D, 2007b. Water follows carbon: CO2 incites deep silicate melting and dehydration beneath mid-ocean ridges. Geology, 35(2): 135–138, https://doi.org/10.1130/G22856A.1.
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