Geomorphological changes in young soils with sparse vegetation: Mathematical modeling and numerical simulation. [PDF]
This article presents an improved mathematical model and numerical simulation for weathering of large areas with complex topography. It uses the equations of momentum, temperature, and humidity in turbulent air and for heat and water infiltration into ...
Zambra C +3 more
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In the Late Paleozoic and Early Mesozoic, during about 100 m.y., the world’s three largest batholiths (Angara-Vitim, Khangai, and Khentei, each up to 1 000 000 km3 in volume) had formed within the limits of the Central Asian orogenic belt. Considering the case of the Khangai batholith, the problem of how, when, and why such an extensive granite ...
V. V. Yarmolyuk +9 more
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Magmatic surge requires two-stage model for the Laramide orogeny. [PDF]
Schwartz JJ +6 more
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The age of the Marulan batholith
(Uploaded by Plazi from the Biodiversity Heritage Library) No abstract provided.
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Carbon dioxide emissions mitigation strategy through enhanced geothermal systems: western Anatolia, Turkey. [PDF]
Chandrasekharam D, Baba A.
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The search for plausible economic mineral deposits in the central parts of Tanzania; insight from stream sediment geochemistry, multivariate statistics and geostatistics. [PDF]
Nunoo S, Mvile BN, Abu M, Kelimenze JD.
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Alkaline magmas in shallow arc plutonic roots: a field and experimental investigation of hydrous cumulate melting in the southern Adamello batholith. [PDF]
Pimenta Silva M +5 more
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Paradoxically lowered oxygen isotopes of hydrothermally altered minerals by an evolved magmatic water. [PDF]
Wei CS, Zhao ZF.
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Long-lived Paleoproterozoic eclogitic lower crust. [PDF]
Buntin S +7 more
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Non invasive subsurface imaging to investigate the site evolution of Machu Picchu. [PDF]
Masini N +11 more
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