Results 61 to 70 of about 1,193 (219)
Résumé. - Alors qu'en régions continentales le granite à biotite et/ou muscovite est une roche résistante, il fait figure de roche moins résistante en conditions littorales (Bretagne, Irlande).
openaire +2 more sources
Abstract The Altai Accretionary Wedge in the Mongolian Altai records a polyphase geodynamic evolution involving two extensional–compressional tectonic cycles, constrained by petrostructural analysis and zircon, monazite U–Pb, and Ar–Ar geochronology. The studied section includes a southwestern high‐grade and a northeastern low‐grade domain, previously ...
O. Lexa +7 more
wiley +1 more source
Abstract The Kosi River watershed captures the major lithotectonic units, structures, and characteristic climatic conditions found along the Himalaya. Therefore, this setting provides a useful location to investigate the respective influences of tectonics and climate in eroding bedrock and driving landscape evolution.
J. N. Zehner +7 more
wiley +1 more source
Daraban leucogranite occurs as cactus-like dykes hosted in serpentinized harzburgite in the mantle section of the Mawat ophiolite, Kurdistan region, northeastern Iraq.
Mohammad, Y O,, Qaradaghi, J. H.
core +1 more source
Detailed geochronology from two compositionally distinct generations of dikes and sills intruded into the Alta metamorphic aureole, north‐central Utah, complement previous geochronologic studies from the Alta stock, providing information on the timing of
C. J. Beno +5 more
doaj +1 more source
Himalayan Leucogranites: An Experimental Petrology Perspective
The High Himalayan leucogranites (HHL) are produced by muscovite breakdown of a metapelitic source, at temperatures below 800 °C, with initial melt water contents of ~5–7 wt.%. The tourmaline-rich HHL variety is colder, possibly a fractionation product of the hotter two-mica HHL.
Scaillet, Bruno, Pichavant, Michel
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ABSTRACT Orogenic belts that sustain elevated temperatures at intermediate crustal depths for tens of millions of years are known as hot orogens. The evolution of these hot orogens is largely influenced by thermal maturation, primarily driven by the distribution of heat‐producing elements (HPEs), such as K, Th and U in the overthickened crust.
Lucas R. Schiavetti +6 more
wiley +1 more source
Zircon morphology as a petrogenetic indicators in the tonalite-leucogranite association; Zarza la Mayor pluton case (Cáceres, Spain) [PDF]
Zarza la Mayor pluton is a good example of the tonalite-leucogranite association. A new survey has been carried out and some additional study of zircon morphologies has been performed.
Corretgé Castañón, Luis Guillermo +2 more
core
In the Wadi Nugrus area, south Eastern Desert of Egypt, A-type granite is highly deformed in a prominent NW-SE trending shear zone, likely related to the Najd shear system.
Adel A. Surour +2 more
doaj +1 more source
The Yanshanian Orogeny consists of Jurassic to Cretaceous compressional-extensional cycles related to the subduction of the Paleo-Pacific Ocean beneath East Asia. Numerous granitic plutons were emplaced across southeast China at distinct intervals over a
J. Gregory Shellnutt +3 more
doaj +1 more source

