Geomorfología del Complejo de Bushveld [PDF]
, 1997 [Abstract] This paper deals wich che differenc relacion becween scruccure and lichology in che geomorphology of che Bushveld Complexo The final resules demonscrace chac, even so differenc scale ofsize, wider for che epirogenic-cecconic movements and ...
Lageat, Y.
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Unusual nickel and copper to noble-metal ratios from the Råna Layered Intrusion, northern Norway [PDF]
, 1987 Rocks from the Rana Layered Intrusion usually have low concentrations of noble metals but have normal Ni and Cu concentrations. Consequently the rocks have higher Cu/Ir, Ni/Ir, Cu/Pb and Ni/Pd ratios than extrusive rocks from the literature.
Barnes, Sarah-Jane
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Formation and evolution of the chromitites of the Stillwater Complex : a trace element study [PDF]
, 2011 Large layered intrusions, such as the Stillwater Complex, contain cyclic units of chromite-rich layers (cm to m thick) having kilometre-scale lateral extension.
Barnes, Sarah-Jane +2 more
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Chromitite in a Tibetan Ophiolite Records Deep Upper-Mantle Circulation and Episodic Subduction [PDF]
, 2020 Suzanne Y. O’Reilly +5 more
openalex +1 more source
86th Annual Meeting of the Meteoritical Society (2024)
Meteoritics &Planetary Science, Volume 59, Issue S1, Page A1-A468, August 2024.
wiley +1 more source
Monomineralic anorthosites in layered intrusions are indicators of the magma chamber replenishment by plagioclase-only-saturated melts. [PDF]
Sci Rep, 2020 Latypov R +5 more
europepmc +1 more source
Ophiolitic Chromitites Originated from Ancient SCLM [PDF]
Acta Geologica Sinica - English Edition, 2015 R. D. SHI +8 more
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Anthropogenic Sources Dominate Foliar Chromium Dust Deposition in a Mining-Based Urban Region of South Africa. [PDF]
Int J Environ Res Public Health, 2022 Adhikari S +3 more
europepmc +1 more source
High pressure metamorphic conditions in garnet amphibolite from a collisional shear zone related to the Tapo ultramafic body, Eastern Cordillera of Central Peru [PDF]
, 2010 A discontinuos belt of elongated ultramafic rock bodies (mostly serpentinites) occurs in the Eastern Cordillera of the central Peruvian Andes. One of the main occurrences is the Tapo Massif, a lense-shaped serpentinite body, ~2 km x 5 km, comprising ...
Acosta, Jorge +4 more
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