Seawater-peridotite interaction at 300°C and 500 bars: implications for the origin of oceanic serpentinites
- 1 February 1980
- journal article
- Published by Elsevier in Geochimica et Cosmochimica Acta
- Vol. 44 (2), 309-321
- https://doi.org/10.1016/0016-7037(80)90139-8
Abstract
No abstract availableKeywords
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