Results 71 to 80 of about 14,875 (109)
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The 2.26 to 2.18 Ga Arc-Related Magmatism of the Almas-Conceição do Tocantins Domain: An Early Stage of the São Francisco Paleocontinent Assembly in Central Brazil

, 2020
Paleoproterozoic (Rhyacian) rocks dominate within the basement of the Neoproterozoic Brasilia Belt and their genesis has been attributed to the orogenic amalgamation event that assembled the Sao Francisco-Congo paleocontinent from 2.18 to 2.07 Ga ...
A. Saboia   +6 more
semanticscholar   +1 more source

Retrieving geological units with unsupervised clustering of gamma-ray spectrometry data

, 2021
Airborne gamma-ray spectrometry (AGRS) provides valuable insights for geological mapping, mineral exploration, geomorphological studies, and lithological differentiation.
J. Weihermann   +4 more
semanticscholar   +1 more source

Tonian Intra-Oceanic Magmatism as the source of the Goiás Porphyry Copper-Gold System in the Brasília Orogenic belt: Petrogenesis and Metallogenetic Implications

Journal of the Geological Society
In the Goiás Intra-Oceanic Arc System (Goiás IOAS), Brasília Orogen, Brazil, occurrences of porphyry-type mineral deposits have been identified. The most significant of these is the Chapada Cu-Au deposit (1056 Mt Cu @ 0.24% Au @ 0.12 g/t).
A. Ferreira   +2 more
semanticscholar   +1 more source

Petrogenesis of the Córrego das Campinas Gabbro-Anorthosite Suite: Characterization of a Neoproterozoic massif-type anorthosite in the Goiás Magmatic Arc and its significance in the evolution of the Brasília belt, Brazil

Journal of South American Earth Sciences, 2022
Fernando Santos Diener   +7 more
semanticscholar   +1 more source

Metamorphism overprint in mafic-ultramafic cumulates in the Mangabal and Americano do Brasil Complexes, Brasilia Belt, Brazil

Journal of the Geological Society
The Americano do Brasil and Mangabal Complexes belong to a cluster of Neoproterozoic mafic-ultramafic intrusions in the southern Goiás Magmatic Arc in Brazil.
C. Augustin   +3 more
semanticscholar   +1 more source

The mantle and crust record of convergent margin deposits – Preliminary results of the MT Brazil Project

Proceedings
The Goiás Magmatic Arc (GMA) evolved between ~900–600 Ma during the Brasiliano Orogeny, involving arc magmatism, craton collisions, and post-collisional processes. Despite insights from airborne geophysics, uncertainties remain about mantle/lower crustal
R. Vidotti   +11 more
semanticscholar   +1 more source

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