Results 41 to 50 of about 128,965 (257)
Morphostructure Control Towards the Development of Mahawu Volcanic Complex, North Sulawesi
Indonesian Journal on Geoscience, 2014 DOI: 10.17014/ijog.v7i1.134The studied area, situated in northeastern part of North Sulawesi Arm, is dominantly occupied by the Mahawu, Linau, Tompusu, and Kasurutan volcanic rocks.
S. Poedjoprajitno
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Modeling Viscosity of Volcanic Melts With Artificial Neural Networks
Geochemistry, Geophysics, Geosystems, 2022 Viscosity is of great importance in governing the dynamics of volcanoes, including their eruptive style. The viscosity of a volcanic melt is dominated by temperature and chemical composition, both oxides and water content.
D. Langhammer +2 more
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Pre-eruptive CO2 budget of lower Cenozoic Neo-Tethyan magmas [PDF]
, 2023 Léa Ostorero +3 more
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Philosophical Transactions of the Royal Society A, 2018 The thermal and therefore physical state of magma bodies within the crust controls the processes and time scales required to mobilize magmas before eruptions, which in turn are critical to hazard assessment.
K. Cooper
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Revista Eureka sobre Enseñanza y Divulgación de las Ciencias, 2013 Los programas de Biología y Geología establecen la utilización de modelos físicos analógicos para promover el aprendizaje de fenómenos geológicos.
Paula Cristina de Almeida Maria Castelhano +2 more
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Emplacement of magma pulses and growth of magma bodies [PDF]
Tectonophysics, 2011 Magmatism is responsible for the formation of continental and oceanic crusts. It is the main agent of mass and heat transfers from the mantle towards the crust, the hydrosphere (oceanic and continental hydrothermalism) and the atmosphere (emissions of volcanic gas and ashes).
Menand, Thierry +2 more
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Boulder of orbicular rapakivi in Taivassalo, southwestern Finland [PDF]
Bulletin of the Geological Society of Finland, 1983 A boulder of an orbicular rapakivi was found in Taivassalo, close to the southern contact of the Vehmaa rapakivi area in southwestern Finland. Many features, e.g.
N. Edelman
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Feeding of a magma chamber by an ascending magma bubble
Geophysical Journal International, 2021 SUMMARY There is evidence that magma chambers are not fed by a continuous flow, but in the form of discrete magma batches. The possibility is considered that the chamber is fed by a magma bubble ascending through the region underneath, driven by buoyancy force.
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Magma chamber formation by magma intrusion into the Earth’s crust
Computational Continuum Mechanics, 2018 <p>The main mechanism of transport of magma in the Earth&#8217;s crust is the formation of cracks, or dikes, through which the melt moves towards the surface under the action of buoyancy forces and tectonic stresses.
Ivan Utkin, Oleg Melnik
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Magma evolution of the Emeishan mantle plume: insights from the Hongge diabase in the Panxi region, SW China [PDF]
, 2023 Kun Wang
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