Results 81 to 90 of about 8,065 (232)
Global Cooling Driving the Increase in Erosion Rates Across the Himalaya Since the Quaternary
Geophysical Research Letters, Volume 53, Issue 13, 16 July 2026.Abstract Late Cenozoic global cooling is well documented, yet its impact on erosion rates in active mountain belts, particularly after the onset of Quaternary glaciation, remain contentious. This ambiguity partially stems from the potential methodological biases in erosion rate quantification, particularly in the Himalaya, where recent studies report ...
Dongxu Cai +9 more
wiley +1 more source
The contorted New England Orogen (eastern Australia): New evidence from U-Pb geochronology of early Permian granitoids [PDF]
, 2012 A series of sharp bends (oroclines) are recognized in the Paleozoic to early Mesozoic New England Orogen of eastern Australia. The exact geometry and origin of these bends is obscured by voluminous magmatism and is still debated. Here we present zircon U-
Rosenbaum, Gideon +7 more
core +1 more source
Геохімія техногенезу, 2020 The article discusses the results of comprehensive studies of the integral and differential geodynamics of the Early Proterozoic Novoukrain-skyi granite gneiss dome, which does not have its own petrological, parametric and specialized analogue on the ...
Semenyuk N. +4 more
doaj +1 more source
Earth and Space Science, Volume 13, Issue 7, July 2026.Abstract Southern Thailand hosts numerous low‐ to medium‐enthalpy geothermal manifestations in a non‐volcanic setting. This study investigates the geothermal potential of the region through the integration of satellite‐derived gravity data and geological observations.
T. Phiranram +3 more
wiley +1 more source
Sumatran granitoids and their relationship to southeast Asian terranes [PDF]
, 1995 Three subparallel, N-S-trending granitoid provinces occur in Southeast Asia: the Eastern Granitoid Province of peninsular Malaysia; the Central Granitoid Province, extending from northwestern Thailand to the western part of peninsular Malaysia and to the
Gasparon, M (15476894) +1 more
core
Geochemistry, Geophysics, Geosystems, Volume 27, Issue 7, July 2026.Abstract The interaction between the Tethyan and Paleo‐Pacific subduction systems in Southeast Asia since the Paleozoic is still poorly understood. Hainan Island and Borneo, located near the junction of the Tethyan and Paleo‐Pacific domains, provide the critical regions for understanding the dynamic processes and interaction between the two tectonic ...
Yang Zhou +14 more
wiley +1 more source
The petrochemical characteristics of the Hercynian granitoids in Tianshan and its geodynamic implications [PDF]
, 2003 Four genectic types of granitoids, i. e. mantle-derived type (M-type), syntexis type (SY-type), trasformation type [T-type, including migmatic (MT), peraluminous (PT) and K-rich (KT) subtypes], and A-type were classified in the Hercynian granitoids in ...
Bao, JX +4 more
core
Types and genesis of the enclaves in Central Anatolian granitoids [PDF]
, 1999 Central Anatolian granitoids range from tonalite-monzonite, through granodiorite, to alkali feldspar granite in composition, and typically have angular to oval-shaped mafic magmatic and metamorphic enclaves.
Güleç, Nilgün Türkan +2 more
core +1 more source
Geochemistry, Geophysics, Geosystems, Volume 27, Issue 7, July 2026.Abstract Eocene magmatism in southern Tibet records deep geodynamic processes associated with the India‐Asia collision. The Quxu batholith, a representative segment of the Gangdese magmatic belt, hosts widespread mafic microgranular enclaves (MMEs) indicating magma mixing.
Yuanku Meng +5 more
wiley +1 more source