Hydrothermal alteration and melting of the crust during the Columbia River Basalt–Snake River Plain transition and the origin of low-δ 18 O rhyolites of the central Snake River Plain-Reference-Cited by-同舟云学术

Hydrothermal alteration and melting of the crust during the Columbia River Basalt–Snake River Plain transition and the origin of low-δ 18 O rhyolites of the central Snake River Plain

Published:2015-05 Issue: Volume:224-225 Page:310-323
ISSN:0024-4937
Container-title:Lithos
language:en
Short-container-title:Lithos

Author:

Colón Dylan P.,Bindeman Ilya N.,Ellis Ben S.,Schmitt Axel K.,Fisher Christopher M.

Funder

NSF

National Science Foundation

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference81 articles.

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5. Pre-Cougar Point Tuff Volcanic Rocks Near the Idaho-Nevada Border, Owyhee County, Idaho;Bernt,1982

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