Results 1 to 10 of about 6,694 (263)

Constraints from rocks in the Taiwan orogen on crustal stress levels and rheology [PDF]

open access: yes, 2012
Taiwan's Hsüehshan range experienced penetrative coaxial deformation within and near the brittle-plastic transition between ∼6.5 and 3 Ma. This recent and short-lasting deformation in an active, well-studied orogen makes it an ideal natural laboratory ...
Avouac, Jean-Philippe   +2 more
core   +1 more source

A changing thermal regime revealed from shallow to deep basalt source melting in the Moon. [PDF]

open access: yesNat Commun, 2022
Srivastava Y   +4 more
europepmc   +1 more source

Evolution of the Lithospheric Mantle beneath the Marsabit Volcanic Field (Northern Kenya): Constraints from Textural, P-T and Geochemical Studies on Xenoliths [PDF]

open access: yes, 2017
Xenoliths hosted by Quaternary basanites and alkali basalts from Marsabit (northern Kenya) represent fragments of Proterozoic lithospheric mantle thinned and chemically modified during rifting in the Mesozoic (Anza Graben) and in the Tertiary-Quaternary (
KAESER, BENJAMIN   +2 more
core  

Compositional zoning of garnet porphyroblasts from the polymetamorphic Wölz Complex, Eastern Alps [PDF]

open access: yes, 2018
We employ garnet isopleth thermobarometry to derive the P-T conditions of Permian and Cretaceous metamorphism in the Wölz crystalline Complex of the Eastern Alps.
Abart, Rainer   +3 more
core  

Pyroxenite xenoliths from Marsabit (Northern Kenya): evidence for different magmatic events in the lithospheric mantle and interaction between peridotite and pyroxenite [PDF]

open access: yes, 2018
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  

Mineral Chemistry and Pressure and Temperature Estimates of Metasedimentary Rocks of the Araxá Group in the Region of Morrinhos, South of Goiás State [PDF]

open access: yesGeologia USP. Série Científica, 2011
In the Morrinhos region, Goiás state, Brazil, the rocks of the Araxá Group have mineral assemblages related to themetamorphic peak which occurred in this region and is typical of the amphibolite facies (kyanite zone).
Guillermo Rafael Beltran Navarro   +4 more
doaj  

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