Results 31 to 40 of about 3,530 (217)

SHRIMP U-Pb zircon dating of Pedras Grandes Suite, southern Santa Catarina State, Brazil

open access: yesAnais da Academia Brasileira de Ciências, 2005
Two major magmatic pulses of the granitic Florianópolis Batholith in Santa Catarina State, southern Brazil, occurred between 613±5Ma and 595±5 Ma, during the Neoproterozoic Brasiliano Cycle.
Andréa R. Jelinek   +4 more
doaj   +1 more source

Role of Complex Crustal and Basinal Structures in Onset of an Intracratonic Rift System: An Example From the Onshore Potiguar Basin, Brazilian Equatorial Margin

open access: yesBasin Research, Volume 38, Issue 2, March–April 2026.
Schematic evolution model of the Onshore Potiguar Basin, illustrating the role of complex crustal and basinal structures in the onset of this intracratonic rift system in NE Brazilian Equatorial Margin. Red arrows indicate the extensional direction and coloured areas on the surface are the Self‐Organizing Maps populations related to crystalline ...
David L. de Castro   +5 more
wiley   +1 more source

Itinerário da errância: a morte na obra cardosiana

open access: yesRevista Interdisciplinar de Direito, 2012
Nella controversa produzione letteraria dello scrittore brasiliano, Lúcio Cardoso, il tema della morte appare in modalità privilegiata. È su questo tema che questo articolo presenta considerazioni.
Regina Pentagna Petrillo
doaj  

The hidden passive margins from the birth of SW Gondwana [PDF]

open access: yesBrazilian Journal of Geology
The final consolidation of southwestern Gondwana during the Ediacaran–Cambrian resulted in the formation of a large landmass originally surrounded by the newborn Panthalassic Ocean.
Lucas Veríssimo Warren   +10 more
doaj   +1 more source

Tectonic Framework of the Arenópolis and Anicuns‐Itaberaí Segments of the Goiás Magmatic Arc Based on 3D Magnetotelluric Inversion

open access: yesGeochemistry, Geophysics, Geosystems, Volume 26, Issue 12, December 2025.
Abstract The Goiás Magmatic Arc (GMA) is a Neoproterozoic juvenile terrain formed through oceanic‐oceanic and oceanic‐continental subduction. It comprises three main segments: Mara Rosa, Anicuns‐Itaberaí (GMAAI), and Arenópolis (GMAA), whose tectonic evolution and connectivity remain uncertain.
J. G. C. Inacio   +4 more
wiley   +1 more source

Limites subjetivos da coisa julgada no direito brasileiro: uma rápida comparação com o direito italiano

open access: yesIl Diritto degli Affari, 2021
L’Autore si confronta con il tema dei limiti soggettivi del giudicato nel diritto brasiliano, mettendolo a confronto con il sistema italiano, in particolare con riferimento alla necessità del rispetto del principio del contraddittorio, dando altresì ...
Enrico Andrade
doaj  

Il diritto amministrativo brasiliano: aspetti attuali del controllo della pubblica amministrazione

open access: yesRevista Eurolatinoamericana de Derecho Administrativo, 2017
L'articolo mira a descrivere l'attuale diritto amministrativo brasiliano. Inizia con un approccio generale alla situazione contemporanea, in particolare degli ultimi venti anni.
Emerson Gabardo   +2 more
doaj   +1 more source

Confronting Episodic vs. Continuous Heat Sources in Long‐Lived Hot Orogens: Insights From Petrochronological Studies in the Nova Venecia Complex, Araçuaí Orogen (SE Brazil)

open access: yesJournal of Metamorphic Geology, Volume 43, Issue 9, Page 863-890, December 2025.
ABSTRACT Orogenic belts that sustain elevated temperatures at intermediate crustal depths for tens of millions of years are known as hot orogens. The evolution of these hot orogens is largely influenced by thermal maturation, primarily driven by the distribution of heat‐producing elements (HPEs), such as K, Th and U in the overthickened crust.
Lucas R. Schiavetti   +6 more
wiley   +1 more source

A Recipe for Exotic Continental Fragment Formation: Key Constraints From Numerical Rift Models

open access: yesJournal of Geophysical Research: Solid Earth, Volume 130, Issue 10, October 2025.
Abstract The Wilson Cycle describes the opening and closing of oceans, generating new plate boundaries at continental rifts, and extinguishing ancient plate boundaries with continental collisions (creating a continental suture). However, the general view of the Wilson Cycle does not fully explain more complex tectonic scenarios.
Alan J. Yu   +3 more
wiley   +1 more source

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