Results 121 to 130 of about 3,793 (208)
Late orogenic carboniferous extensions in the Variscan French Massif Central
International audienceThe Variscan French Massif Central experienced two successive stages of extension from Middle Carboniferous to Early Permian. In the northern Massif Central, the first stage began in the late Visean, immediately after nappe stacking,
Alabouvette +114 more
core +3 more sources
The Borborema Pegmatite Province, NE-Brazil revisited [PDF]
Considering the internal structure, mineralogical distribution and geochemical data on K-feldspar, white micas, Nb-Taoxides, tourmalines, garnet and spinel, it becomes clear that the pegmatites classified as "heterogeneous" (Johnston 1945) include ...
Barreto, S. +5 more
core
Mineralogical characterisation of tantalum ores for the optimization of their processing [PDF]
Peer ReviewedPostprint (published ...
Alfonso Abella, María Pura +7 more
core +1 more source
The pegmatites of Nasarawa area occur in the central part of Nigeria. They are mainly hosted by phyllonites in a NNE-SSW trending shear zone lying east of some foliated Pan-African and West of Jurassic Afu Complex Younger Granites.
O.F. Akintola, J.I.D Adekeye
doaj
Institute of Geology and Geophysics, Chinese Academy of Sciences-The time-space exploration from Earth core to galaxies. [PDF]
Zhang W, Zhao W, Zhao L.
europepmc +1 more source
Isotopic systematics of zircon indicate an African affinity for the rocks of southernmost India. [PDF]
Clark C, Collins AS, Taylor RJM, Hand M.
europepmc +1 more source
The present continental crust is characterized by a felsic upper crust and a mafic lower crust, resulting from significant geochemical differentiation over geological time.
Long Tian +7 more
doaj +1 more source
Microcontinent subduction and S-type volcanism prior to India-Asia collision. [PDF]
Yang Z +7 more
europepmc +1 more source
Ptarmigan Fiord basement-cover thrust imbricates, Baffin Island, Nunavut [PDF]
The rocks at Ptarmigan Fiord on the Hall Peninsula of Baffin Island underwent midcrustal deformation during the formation of the Paleoproterozoic Trans-Hudson Orogen.
Carr, S D +4 more
core
Coexisting divergent and convergent plate boundary assemblages indicate plate tectonics in the Neoarchean. [PDF]
Huang B +5 more
europepmc +1 more source

