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Baker, L.; Franchi, Ian; Wright, Ian and Pillinger, Colin
(2001).
URL: http://www.lpi.usra.edu/meetings/gold2001/pdf/3610...
Abstract
The oxygen isotopic composition of water from carbonaceous chondrites suggests that close to isotopic equilibrium was attained on CI and CM parent bodies. This is more consistent with a closed system than one with fluid flow. Tagish Lake does not display such equilibrium.