Origin of 13C-depleted Kerogen in ca. 3.5 Ga hydrothermal silica dikes from Western Australia

Details Origin of 13C-depleted Kerogen in ca. 3.5 Ga hydrothermal silica dikes from Western Australia Origin of 13C-depleted Kerogen in ca. 3.5 Ga hydrothermal silica dikes from Western Australia

Sep 2003

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2003gecas..67q.501u&link_type=openurl

Geochimica et Cosmochimica Acta Supplement, Vol. 67, Issue 18, p.501

Physics

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