Results 111 to 120 of about 2,562 (192)
Miocene arc volcanism is manifested widely in the Valle del Cura-El Indio belt region (29°30´–30° South latitude), in the southern Central Andes of Argentina and Chile.
V.D. LITVAK, S. POMA
doaj
Archean eclogite-facies oceanic crust indicates modern-style plate tectonics. [PDF]
Ning W, Kusky T, Wang L, Huang B.
europepmc +1 more source
Pyroxenite xenoliths from Marsabit (Northern Kenya): evidence for different magmatic events in the lithospheric mantle and interaction between peridotite and pyroxenite [PDF]
Garnet-bearing and garnet-free pyroxenite xenoliths from Quaternary basanites of Marsabit, northern Kenya, were analysed for microstructures and mineral compositions (major and trace elements) to constrain the thermal and compositional evolution of the ...
Altherr, Rainer +4 more
core
Amphibolites in the Shuixiakou area of the southern Dunhuang Orogenic Belt, southernmost Central Asian Orogenic Belt (CAOB), occur as lenses within hornblende-biotite-plagioclase gneiss or pelitic schist, exhibiting block-in-matrix feature of tectonic ...
Hao Y. C. Wang +7 more
doaj +1 more source
The origin and role of fluid associated with lower crustal metamorphism [PDF]
科学研究費助成事業(科学研究費補助金)研究成果報告書:基盤研究(B)2008-2011課題番号 ...
Tsunogae Toshiaki, 角替 敏昭
core
Pristine microstructures in pseudotachylytes formed in dry lower crust, Lofoten, Norway. [PDF]
Dunkel KG, Morales LFG, Jamtveit B.
europepmc +1 more source
Introduction The area studied is located north of Azna (Lorestan Province) in a small portion of the Sanandaj – Sirjan structural zone (Mohajjel et al., 2003).This area is part of the Zagros orogenic belt, formed by the opening and closure of Neotethyan
Karim Abdollahi Silabi +2 more
doaj
Precambrian crustal evolution and Cretaceous–Palaeogene faulting in West Greenland: Origin and evolution of the Kangâmiut mafic dyke swarm, West Greenland [PDF]
The Kangâmiut dyke swarm in West Greenland intruded Archaean terrains at 2.04 Ga, and its northern portion was subsequently metamorphosed to granulite facies during the Nagssugtoqidian orogeny(c. 1.8 Ga).
Lesher, Charkes E., Mayborn, Kyle R.
doaj
Massive methane fluxing from magma-sediment interaction in the end-Triassic Central Atlantic Magmatic Province. [PDF]
Capriolo M +11 more
europepmc +1 more source
Petrological and major-trace element mineral chemistry studies have been carried out on pyroxenites from the Pakkanadu alkaline-ultramafic complex from the southern India to understand their origin and nature of magma responsible for ultramafic magmatism
Jiten Pattnaik +6 more
doaj +1 more source

