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Discussion of recent papers on carbonated peridotite, bearing on mantle metasomatism and magmatism: response

Wyllie, Peter J. (1987) Discussion of recent papers on carbonated peridotite, bearing on mantle metasomatism and magmatism: response. Earth and Planetary Science Letters, 82 (3-4). pp. 401-402. ISSN 0012-821X. https://resolver.caltech.edu/CaltechAUTHORS:20160111-155022574

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Abstract

I agree with Eggler [1] that there is no discrepancy in the "10-kbar difference in pressure between the pseudoinvariant point H_2 of Olafsson and Eggler [2] and an invariant point I_6 in CaO- MgO-SiO_2-CO_2" if the topology shown in his Fig. 1 is established. My discussion [3], however, was more concerned with the difference of about 8 kbar between the points H_2, related to the range of amphibole stability, in the only two experimental studies reported on the solidus for dolomite-amphibole- peridotite [2,4], which are reproduced in my Fig. 1A and 1B [3].


Item Type:Article
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http://dx.doi.org/10.1016/0012-821X(87)90215-9DOIArticle
http://www.sciencedirect.com/science/article/pii/0012821X87902159PublisherArticle
Additional Information:© 1987 Elsevier Science Publishers B.V. Received December 8, 1986.
Issue or Number:3-4
Record Number:CaltechAUTHORS:20160111-155022574
Persistent URL:https://resolver.caltech.edu/CaltechAUTHORS:20160111-155022574
Official Citation:Peter J. Wyllie, Discussion of recent papers on carbonated peridotite, bearing on mantle metasomatism and magmatism: response, Earth and Planetary Science Letters, Volume 82, Issue 3, 1987, Pages 401-402, ISSN 0012-821X, http://dx.doi.org/10.1016/0012-821X(87)90215-9. (http://www.sciencedirect.com/science/article/pii/0012821X87902159)
Usage Policy:No commercial reproduction, distribution, display or performance rights in this work are provided.
ID Code:63557
Collection:CaltechAUTHORS
Deposited By: Tony Diaz
Deposited On:12 Jan 2016 19:14
Last Modified:03 Oct 2019 09:29

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