Present day serpentinization in New Caledonia, Oman and Yugoslavia

Details Present day serpentinization in New Caledonia, Oman and Yugoslavia Present day serpentinization in New Caledonia, Oman and Yugoslavia

Jan 1978

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1978gecoa..42..144b&link_type=abstract

Geochimica et Cosmochimica Acta, vol. 42, Issue 1, pp.144-145

Physics

13

Scientific paper

Geochemical evidence for modern low-temperature serpentinization has
been found in three new localities. Apparently the low-temperature
reactions are a common mode of formation of the lizardite-chrysotile and
brucite assemblage. Possibly the 18 O content of serpentine formed at
low temperatures is in part inherited from the pyroxene and olivine.

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