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Heterogeneity in mid-ocean ridge sources

Asimow, Paul D. (2006) Heterogeneity in mid-ocean ridge sources. Geochimica et Cosmochimica Acta, 70 (18). A23. ISSN 0016-7037. https://resolver.caltech.edu/CaltechAUTHORS:20120830-140449069

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Abstract

Understanding of decompression melting of homogeneous peridotite sources beneath mid-ocean ridges has reached a reasonably mature state. One can construct apparently adequate models that relate source composition, including volatile contents, and potential temperature to major and trace element chemistry of the aggregate primary liquid and to correlations with physical variables like melt flux and axial depth. Such models are the basis of the consensus view of the average thermal and compositional state of the upper mantle and the range of their variability.


Item Type:Article
Related URLs:
URLURL TypeDescription
http://dx.doi.org/10.1016/j.gca.2006.06.060 DOIUNSPECIFIED
http://www.sciencedirect.com/science/article/pii/S0016703706003383PublisherUNSPECIFIED
http://goldschmidt.info/OrganizationUNSPECIFIED
ORCID:
AuthorORCID
Asimow, Paul D.0000-0001-6025-8925
Additional Information:© 2006 Pergamon-Elsevier Science Ltd.
Issue or Number:18
Record Number:CaltechAUTHORS:20120830-140449069
Persistent URL:https://resolver.caltech.edu/CaltechAUTHORS:20120830-140449069
Official Citation:P.D. Asimow, Heterogeneity in mid-ocean ridge sources, Geochimica et Cosmochimica Acta, Volume 70, Issue 18, Supplement, August–September 2006, Page A23, ISSN 0016-7037, 10.1016/j.gca.2006.06.060.
Usage Policy:No commercial reproduction, distribution, display or performance rights in this work are provided.
ID Code:33718
Collection:CaltechAUTHORS
Deposited By: Tony Diaz
Deposited On:30 Aug 2012 22:35
Last Modified:03 Oct 2019 04:12

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