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      Initial impingement of the Yellowstone plume located by widespread silicic volcanism contemporaneous with Columbia River flood basalts

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      Geology
      Geological Society of America

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          Stirring and structure in mantle starting plumes

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            Effects of repetitive emplacement of basaltic intrusions on thermal evolution and melt generation in the crust

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              Isotopic and Chemical Evidence Concerning the Genesis and Contamination of Basaltic and Rhyolitic Magma Beneath the Yellowstone Plateau Volcanic Field

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                Author and article information

                Journal
                Geology
                Geological Society of America
                1943-2682
                0091-7613
                July 01 2012
                July 01 2012
                : 40
                : 7
                : 655-658
                Article
                10.1130/G32692.1
                4be9b012-dc84-487d-a664-66f544bff3cb
                © 2012
                History

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