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Chemical Variations in the 1998, 2011, and 2015 Lava Flows From Axial Seamount, Juan de Fuca Ridge: Cooling During Ascent, Lateral Transport, and Flow

Abstract Lava flows erupted at Axial Seamount in 1998, 2011, and 2015 are chemically heterogeneous and display decreases in MgO content in their glass rinds with increasing distance from the summit. The trends are consistent with eruption temperature decreases down the rift zones of ~0.5 °C/km withi...

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Hlavní autoři: David A. Clague, Jennifer B. Paduan, Brian M. Dreyer, William W. Chadwick Jr, Kenna H. Rubin, Michael R. Perfit, Allison T. Fundis
Médium: Artigo
Jazyk:Inglês
Vydáno: Wiley 2018-09-01
Edice:Geochemistry, Geophysics, Geosystems
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On-line přístup:https://doi.org/10.1029/2018GC007708
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