[HTML][HTML] A perspective on potassic and ultrapotassic rocks: Constraints on the Paleoproterozoic late to post-collisional event in the São Francisco paleocontinent
The late-to post-collisional stage in orogenic systems is characterized by the coeval
existence of bimodal potassic to ultrapotassic magmatic activity related to partial melting of …
existence of bimodal potassic to ultrapotassic magmatic activity related to partial melting of …
Stratigraphic and geochronological characterization of the Mato Verde group, Central Espinhaço (Brazil): An Eocalymmian rifting record in the western domain of the …
AF de Oliveira Costa, A Danderfer, C Lana - Journal of South American …, 2018 - Elsevier
Abstract The Mato Verde Group comprises an important volcano-sedimentary record
occurring in the eastern Congo-São Francisco paleocontinent along the western border of …
occurring in the eastern Congo-São Francisco paleocontinent along the western border of …
The atypical Gaoligong orocline: Its geodynamic origin and evolution
YP Chiu, MW Yeh, TY Lee - Frontiers in Earth Science, 2023 - frontiersin.org
Various orocline systems around the India–Eurasia collision zone have long been
recognized and studied. Different portions of the India–Eurasia boundaries represent …
recognized and studied. Different portions of the India–Eurasia boundaries represent …
The Rio Pardo salient, northern Araçuaí orogen: an example of a complex basin-controlled fold-thrust belt curve
The Rio Pardo salient, the large antitaxial curve described by the Araçuaí fold-and-thrust belt
along the southeastern edge of the São Francisco craton, is one of the most prominent and …
along the southeastern edge of the São Francisco craton, is one of the most prominent and …
Geodiversity and abiotic ecosystem services in parks from the far north of Minas Gerais: educational and geotourism potential
LF Pressi, PTA Castro - Revista Cerrados, 2023 - periodicos.unimontes.br
Caracterização microestrutural e geoquímica de granitoides riacianos-orosirianos do embasamento do Orógeno Araçuaí aflorantes no bloco Itacambira-Monte Azul.
INR Guedes - 2019 - monografias.ufop.br
O Bloco Itacambira-Monte Azul (BIMA) é formado por rochas predominantemente graníticas
riacianas-orosirianas e integra parte do embasamento do orógeno Araçuaí. Exposto na …
riacianas-orosirianas e integra parte do embasamento do orógeno Araçuaí. Exposto na …
[引用][C] Arquitetura e evolução tectono-metamórfica da Saliência do Rio Pardo, Orógeno Araçuaí, MG.
EIN Peixoto - 2017