Results 131 to 140 of about 3,252 (193)
Author Correction: Numerical modeling the process of deep slab dehydration and magmatism. [PDF]
Sci RepWu H +5 more
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Channelized metasomatism in Archean cratonic roots as a mechanism of lithospheric refertilization. [PDF]
Nat CommunRoots EA +6 more
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Synchronized Mascarene volcanism reveals 400 kyr cycles in melt supply from the Réunion plume. [PDF]
Nat CommunFamin V +3 more
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Contemporaneous mobile- and stagnant-lid tectonics on the Hadean Earth. [PDF]
NatureValley JW +11 more
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Weak mantle wedge causes mantle exhumation punctuated with discrete oceanic crust in the Tyrrhenian basin. [PDF]
Nat CommunSu H, Leng W, Liao J, Brune S.
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Reviews in Mineralogy and Geochemistry, 2004
Epidote was first recognized as a magmatic mineral in the alpine Bergell tonalite by Cornelius (1915). Field observations and microscopic textures let Cornelius to conclude "... the only possibility is, that epidote is a primary mineral in our tonalite, crystallizing early from the magma, i.e., before (in part also contemporaneous with) biotite ...
M. W. Schmidt, S. Poli
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Epidote was first recognized as a magmatic mineral in the alpine Bergell tonalite by Cornelius (1915). Field observations and microscopic textures let Cornelius to conclude "... the only possibility is, that epidote is a primary mineral in our tonalite, crystallizing early from the magma, i.e., before (in part also contemporaneous with) biotite ...
M. W. Schmidt, S. Poli
openaire +5 more sources
The magmatic web beneath Hawai‘i
Science, 2023The deep magmatic architecture of the Hawaiian volcanic system is central to understanding the transport of magma from the upper mantle to the individual volcanoes. We leverage advances in earthquake monitoring with deep learning algorithms to image the structures underlying a major mantle earthquake swarm of nearly 200,000 events that rapidly ...
John D. Wilding +3 more
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The Terminology of Late-Magmatic and Post-Magmatic Processes
The Journal of Geology, 1944Too many conflicting terms are used by petrologists and ore geologists in relation to late-magmatic and post-magmatic processes. An attempt is made to evaluate these terms and to show which are worthy of preservation and which might be eliminated.
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Geological Society, London, Memoirs, 1993
AbstractDuring the past 150 years, a wide range of processes have been invoked to explain the mechanism by which magmas differentiate.These may be divided into those which operate essentially in the liquid state, such as liquid immiscibility and thermogravitational diffusion, and those which involve some form of crystal-liquid fractionation.
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AbstractDuring the past 150 years, a wide range of processes have been invoked to explain the mechanism by which magmas differentiate.These may be divided into those which operate essentially in the liquid state, such as liquid immiscibility and thermogravitational diffusion, and those which involve some form of crystal-liquid fractionation.
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Passive magmatism on Earth and Earth-like planets
Geosystems and Geoenvironment, 2022Xi-Yao Li, Sanzhong Li, Yanhui Suo
exaly