Remelting of cumulates as a process for producing chemical zoning in silicic tuffs: A comparison of cool, wet and hot, dry rhyolitic magma systems

Lithos

Volumn 236-237, Issue , 2015, Pages 275-286

  Wolff, J A ^a   Ellis, B S ^b   Ramos, F C ^c   Starkel, W A ^a   Boroughs, S ^a   Olin, P H ^d   Bachmann, O ^b  

^a WASHINGTON STATE UNIVERSITY   (United States)

^b ETH ZURICH   (Switzerland)

^c NEW MEXICO STATE UNIVERSITY   (United States)

^d UNIVERSITY OF TASMANIA   (Australia)

Author keywords

Compositional zoning; Cumulate melting; Recharge; Silicic magma; Trace elements

Indexed keywords

CALDERA; CUMULATE; IGNEOUS GEOCHEMISTRY; MAGMA CHEMISTRY; MELTING; SILICICLASTIC DEPOSIT; TRACE ELEMENT; TUFF;

EID: 84942613255     PISSN: 00244937     EISSN: 18726143     Source Type: Journal    
DOI: 10.1016/j.lithos.2015.09.002     Document Type: Review

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