Diagenetic fractionation of Ge and Si in reducing sediments: the missing Ge sink and a possible mechanism to cause glacial/interglacial variations in oceanic Ge/Si

Details Diagenetic fractionation of Ge and Si in reducing sediments: the missing Ge sink and a possible mechanism to cause glacial/interglacial variations in oceanic Ge/Si Diagenetic fractionation of Ge and Si in reducing sediments: the missing Ge sink and a possible mechanism to cause glacial/interglacial variations in oceanic Ge/Si

Jul 2000

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2000gecoa..64.2453h&link_type=ejournal

Geochimica et Cosmochimica Acta, v. 64, iss. 14, p. 2453-2465.

Physics

13

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