Results 131 to 140 of about 200 (171)
Some of the next articles are maybe not open access.
A review of the tectonic evolution of the Sunsás belt, SW Amazonian Craton
Journal of South American Earth Sciences, 2010Abstract The Sunsas–Aguapei province (1.20–0.95 Ga), SW Amazonian Craton, is a key area to study the heterogeneous effects of collisional events with Laurentia, which shows evidence of the Grenvillian and Sunsas orogens. The Sunsas orogen, characterized by an allochthonous collisional-type belt (1.11–1.00 Ga), is the youngest and southwesternmost of ...
Wilson Teixeira +5 more
openaire +1 more source
The Rondonian-San Ignacio Province in the SW Amazonian Craton: An overview
Journal of South American Earth Sciences, 2010Abstract The Rondonian-San Ignacio Province (1.56–1.30 Ga) is a composite orogen created through successive accretion of arcs, ocean basin closure and final oblique microcontinent–continent collision. The effects of the collision are well preserved mostly in the Paragua Terrane (Bolivia and Mato Grosso regions) and in the Alto Guapore Belt and the ...
Bettencourt, Jorge Silva +5 more
openaire +2 more sources
Geochronology of the Archean Tumucumaque Complex, Amapá Terrane, Amazonian Craton, Brazil
Journal of South American Earth Sciences, 2018Abstract U-Pb and Lu-Hf isotopic studies were performed in igneous zircon crystals from orthogneisses, metagranodiorites and a gabbro of the Tumucumaque Complex, in Vila Nova region, south of Amapa state, Brazil. The complex is located in the southeastern region of the Guyana Shield, northeastern portion of the Amazonian Craton.
Cristiano Borghetti +3 more
openaire +1 more source
Organic matter in the Neoproterozoic cap carbonate from the Amazonian Craton, Brazil
Journal of South American Earth Sciences, 2016Abstract Bitumen found in Neoproterozoic carbonates from the southern Amazonian Craton, Brazil, represents a great challenge for its geochemical characterization (origin, thermal maturity and the degree of preservation) within a context of petroleum system.
Gustavo R. Sousa Júnior +5 more
openaire +1 more source
Lithos, 2019
Abstract The central portion of the Canaa dos Carajas domain (Ouro Verde area) exhibits a peculiar scenario involving two units of orthopyroxene-bearing sodic rocks: (i) the Mesoarchean Ouro Verde felsic granulite with protolith crystallization and metamorphism ages of 3.05–2.93 Ga and 2.89–2.84 Ga, respectively, and (ii) the Neoarchean Cafe ...
Bhrenno Marangoanha +2 more
openaire +1 more source
Abstract The central portion of the Canaa dos Carajas domain (Ouro Verde area) exhibits a peculiar scenario involving two units of orthopyroxene-bearing sodic rocks: (i) the Mesoarchean Ouro Verde felsic granulite with protolith crystallization and metamorphism ages of 3.05–2.93 Ga and 2.89–2.84 Ga, respectively, and (ii) the Neoarchean Cafe ...
Bhrenno Marangoanha +2 more
openaire +1 more source
From Mesoarchean drips to modern–style tectonics in the Carajás Province, Amazonian Craton
Journal of South American Earth Sciences, 2020Abstract The beginning of modern–style plate tectonics on Earth is not a consensus, but many authors suggest that it happened transitionally, from 3.2 to 2.5 Ga. In the Amazonian Craton, Brazil, the contrasting crustal architecture of the Rio Maria and the Carajas domains is marked by dome–and–keel and linear belt, respectively, which may represent a
Felipe Grandjean da Costa +4 more
openaire +1 more source
The Canadian Mineralogist, 2009
The Mesoproterozoic Mucajai anorthosite – mangerite – rapakivi granite (AMG) complex, in northern Brazil, comprises rapakivi granites, fayalite–pyroxene quartz mangerite and syenite, and a massif-type anorthosite forming an asymmetrically zoned igneous complex without counterpart in the Amazonian craton.
L. M. B. Fraga +3 more
openaire +1 more source
The Mesoproterozoic Mucajai anorthosite – mangerite – rapakivi granite (AMG) complex, in northern Brazil, comprises rapakivi granites, fayalite–pyroxene quartz mangerite and syenite, and a massif-type anorthosite forming an asymmetrically zoned igneous complex without counterpart in the Amazonian craton.
L. M. B. Fraga +3 more
openaire +1 more source
Fissural mafic magmatism on southwestern Amazonian Craton: Petrogenesis and 40Ar-39Ar geochronology
Journal of South American Earth Sciences, 2019Abstract Expressive occurrences of sills and mafic dyke swarms as a result of tafrogenetic processes that led to break-up or attempted break-up of continental crust are found on the south and southwestern Amazonian Craton. This work focus on the magmatic-tectonic processes that formed the Salto do Ceu, Huanchaca, and Rancho de Prata suites. The Salto
Gabrielle Aparecida Lima +4 more
openaire +1 more source
The Roraima Alkaline Province: A cretaceous alkaline province in the Amazonian Craton
Geochemistry, 2022Raisa Fagundes de Figueiredo +2 more
openaire +1 more source
LOMAGUNDI CARBON-ISOTOPE EXCURSION ON THE AMAZONIAN CRATON
Geological Society of America Abstracts with Programs, 2017Andrey Bekker +4 more
openaire +1 more source

