Results 111 to 120 of about 418,217 (192)

Basaltic magma reservoirs: factors controlling their rupture characteristics and evolution.

open access: yes, 1993
The manner in which magma enters and leaves a magma reservoir is a fundamental aspect of magmatic activity. A quantitative model is developed to evaluate the variation of stress acting on the wall of a magma reservoir as a function of depth.
Wilson, L., Parfitt, E. A., Head, J. W.
core   +1 more source

Magma reservoir dynamics at Toba caldera, Indonesia, recorded by oxygen isotope zoning in quartz. [PDF]

open access: yesSci Rep, 2017
Budd DA   +10 more
europepmc   +1 more source

Deep magma underpressure and connectivity drive large dike intrusions. [PDF]

open access: yesSci Adv
Pagli C   +12 more
europepmc   +1 more source

Hadean bridgmanite in the source of a present-day ocean island. [PDF]

open access: yesNature
Israel C   +5 more
europepmc   +1 more source

Enhanced crystal-melt segregation within dynamic mush systems links silicic cumulates with caldera-forming eruptions. [PDF]

open access: yesNat Commun
Lino LM   +8 more
europepmc   +1 more source

Recurrent evacuation of mantle mush in ocean islands revealed by clinopyroxene from La Palma. [PDF]

open access: yesNat Commun
Caracciolo A   +10 more
europepmc   +1 more source

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