Temperatures of serpentinization of ultramafic rocks based on O18/O16 fractionation between coexisting serpentine and magnetite
Year: 1971
Type: article
DOI: 10.1007/bf00643332
Authors: David B. Wenner, Hugh P. Taylor
Institutions: California Institute of Technology, University of Georgia
Language: English
Subfield: Geochemistry and Petrology
Field: Earth and Planetary Sciences
Domain: Physical Sciences
Open Access status: closed
OpenAlex ID: W1988978036