BONGIOLO MARQUES , E.

Last name: BONGIOLO MARQUES

First name: E.

March 2016 (v1)

Journal article

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Structural and lithological controls of gold–bearing veins associated with the Brasiliano–Pan African Orogeny: An example from the Buracão Area, Araí Group (Brasília Fold Belt, Brazil),

Campos Pires, G. Bongiolo Marques, E. Renac, Ch.

The Buracão area, Central Brazil, comprises a group of structurally–controlled vein–type gold prospects, hosted in the metasedimentary Traíras Fm. of the Araí Group. This group records all tectonic stages of the Statherian taphrogenesis in Central Brazil and represents part of the Brasília Fold Belt (BFB) developed during the Neoproterozoic...

Uploaded on: February 28, 2023
November 2011 (v1)

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Evidence of Ediacaran glaciation in southernmost Brazil through magmatic to meteoric fluid circulation in the porphyry-epithermal Au-Cu deposits of Lavras do Sul

Bongiolo Marques, E. Renac, Christophe Mexias Sampaio, A.

The Lavras do Sul Au-Cu mining district, southern Brazil, hosts an Ediacaran plutonic-volcanic association with hydrothermal alteration. This association is interpreted as a ca. 600-580 Ma tilted porphyry-epithermal system, where the main ore occurs in phyllic and intermediate argillic halos around quartz veins. In this paper we used detailed...

Uploaded on: December 3, 2022
January 2016 (v1)

Journal article

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Origin of pegmatites and fluids at Ponta Negra (RJ, Brazil) during late- to post-collisional stages of the Gondwana Assembly,

Bongiolo Marques, E. Renac, Ch. de Toledo Piza, P.

The Ponta Negra Pegmatites (PNP), part of a pegmatitic province in Rio de Janeiro State, Brazil, crop out along an intensely deformed, medium- to high-grade metamorphic area that is proximal to a crustal-scale thrust zone developed during the Brasiliano/Pan–African Orogeny. Fieldwork shows that the pegmatites formed in two distinct stages: (i)...

Uploaded on: February 28, 2023

BONGIOLO MARQUES , E.

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