Age of the magma chamber and its physicochemical state under Elbrus Greater Caucasus, Russia using zircon petrochronology and modeling insights. [PDF]
Sci Rep, 2023 Bindeman IN +6 more
europepmc +1 more source
Author Correction: Age of the magma chamber and its physicochemical state under Elbrus Greater Caucasus, Russia using zircon petrochronology and modeling insights. [PDF]
Sci Rep, 2023 Bindeman IN +6 more
europepmc +1 more source
Catastrophic volcanism as a cause of shocked features found at the K/T boundary and in cryptoexplosion structures [PDF]
The presence of quartz grains containing shock lamellae at the Cretaceous/Tertiary (K/T) boundary is viewed by many as the single most compelling evidence of meteoritic or cometary impact because there is no known endogenous mechanism for producing these
Loper, D. E., Mccartney, K.
core +1 more source
Geophysical Research Letters, 2016 The Wudalianchi Volcano Field (WDF) is a typical intraplate volcano in northeast China with generation mechanism not yet well understood. As its last eruption was around 300 years ago, the present risk for volcano eruption is of particular public ...
Zhiwei Li +6 more
doaj +1 more source
P‐SV conversions at a shallow boundary beneath Campi Flegrei Caldera (Italy): Evidence for the magma chamber [PDF]
, 1992 F. Ferrucci +4 more
openalex +1 more source
The Origin of Co-Magmatic Andesite Enclaves in the Rabor Miocene Pyroxene Andesites, SE Kerman, Iran: Insights from Textural and Mineralogical Composition [PDF]
Journal of Sciences, Islamic Republic of Iran, 2012 The Miocene pyroxene andesite lava flows are exposed in southeastern edge of Urumieh Dokhtar Magmatic assemblage in Iran. The hypocrystalline andesite in parts contain conspicuous co-magmatic igneous enclaves which are dark grey and occur mostly as ...
S. S. Dargahi
doaj
Thermodynamic Model for Energy-Constrained Open-System Evolution of Crustal Magma Bodies Undergoing Simultaneous Recharge, Assimilation and Crystallization: the Magma Chamber Simulator [PDF]
, 2014 Wendy A. Bohrson +5 more
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Timescale of open-reservoir evolution beneath the south Cleft segment, Juan de Fuca ridge
, 2011 International audienceLavas erupted at the southern end of the intermediate Juan de Fuca ridge (Cleft segment) are mostly cogenetic and their chemical diversity results from melt evolution in an open magma system.
Caroff, Martial +2 more
core +3 more sources
The theoretical basis for textural indices of eruption dynamics: review and new conceptual models
Earth, Planets and SpaceThe textural indices of eruption products (pumice, scoria and lavas), number density of crystals or bubbles, or characteristics of their size distributions, have been proposed to estimate dynamic properties such as magma ascent rates, on the basis of ...
Atsushi Toramaru
doaj +1 more source
Crystallization Sequence and Magma Chamber Processes in the Ferrobasaltic Sept Iles Layered Intrusion, Canada [PDF]
, 2010 Olivier Namur +5 more
openalex +1 more source