Olivine xenocryst diffusion reveals rapid monogenetic basaltic magma ascent following complex storage at Pupuke Maar, Auckland Volcanic Field, New Zealand
Basalt
; Olivine
; Silicate minerals
; Trace elements
; Volcanoes
; Diffusion profiles
; Elemental diffusion
; Magma ascents
; Major and minor elements
; Major and trace elements
; Monogenetic volcanoes
; Volcanic field
; Water diffusion
; Diffusion
; alkaline rock
; basalt
; crystallography
; degassing
; diffusion
; magma
; mantle structure
; olivine
; seismic method
; tuff
; Auckland Volcanic Field
; Auckland [North Island]
; Lake Pupuke
; New Zealand
; North Island
Geology Department, University of Otago, Dunedin, New Zealand; School of Environment, University of Auckland, Auckland, New Zealand; Research School of Earth Sciences, The Australian National University, Canberra, Australia; Australian Synchrotron, Clayton, Australia; Department of Earth and Environmental Sciences, University of Iowa, Iowa City, United States; Institut für Geologie, Universität Bern, Bern, Switzerland
Recommended Citation:
Brenna M.,Cronin S.J.,Smith I.E.M.,et al. Olivine xenocryst diffusion reveals rapid monogenetic basaltic magma ascent following complex storage at Pupuke Maar, Auckland Volcanic Field, New Zealand[J]. Earth and Planetary Science Letters,2018-01-01,499