Temperatures of serpentinization of ultramafic rocks based on O18/O16 fractionation between coexisting serpentine and magnetite
- 1 September 1971
- journal article
- research article
- Published by Springer Nature in Contributions to Mineralogy and Petrology
- Vol. 32 (3) , 165-185
- https://doi.org/10.1007/bf00643332
Abstract
No abstract availableKeywords
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