Basaltic magma reservoirs: factors controlling their rupture characteristics and evolution.
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.
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Magma reservoir dynamics at Toba caldera, Indonesia, recorded by oxygen isotope zoning in quartz. [PDF]
Budd DA +10 more
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Cascading magmatic unrest and aseismic faulting in the Aegean Sea enabled by elastic stress relay. [PDF]
Wilding JD, Wang TA, Liu YK, Ross ZE.
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Deep magma underpressure and connectivity drive large dike intrusions. [PDF]
Pagli C +12 more
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Hadean bridgmanite in the source of a present-day ocean island. [PDF]
Israel C +5 more
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Experimental constraints on pre-eruptive conditions at Nabro volcano, Eritrea, 2011, and implications for sulphur emissions. [PDF]
Donovan A +4 more
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Enhanced crystal-melt segregation within dynamic mush systems links silicic cumulates with caldera-forming eruptions. [PDF]
Lino LM +8 more
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Felsic hydrothermal deposit formation by chalcophile metal concentration through mafic recharge and fluid-mediated sulfide dissolution. [PDF]
Liu Y +6 more
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Quantitative Characterization and Differential Evolution of Pore-Fracture Systems in Volcanic Reservoirs of the Changling Fault Depression, Songliao Basin. [PDF]
Zhu H +8 more
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Recurrent evacuation of mantle mush in ocean islands revealed by clinopyroxene from La Palma. [PDF]
Caracciolo A +10 more
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