1.94–1.93 Ga charnockitic magmatism from the central part of the Guyana Shield, Roraima, Brazil: Single-zircon evaporation data and tectonic implications |
| |
Authors: | Lêda Maria Fraga Moacir Jose Buenano Macambira Roberto DallAgnol Joo Batista Sena Costa |
| |
Institution: | aCPRM – Geological Survey of Brazil, Department of Geology, Av. Pasteur, 404, 22290-240 Rio de Janeiro, Rio de Janeiro, Brazil;bIsotope Geology Laboratory, Center of Geosciences, Federal University of Pará, Rua Augusto Corrêa s/n, Guamá 66075-110, Belém, Pará, Brazil |
| |
Abstract: | Age and origin of the charnockitic rocks of the central part of the Guyana Shield have been a matter of discussion. These rocks have been interpreted either as Transamazonian granulites metamorphosed around 2.02 Ga or as 1.56 Ga old igneous charnockites. Recently, most of the Roraima charnockitic rocks have been recognized as igneous rocks and included into the Serra da Prata Suite (SPS). Five Pb–Pb single-zircon evaporation ages were obtained for samples representative of different facies of the SPS and these constrained the age of the charnockitic magmatism between 1943 ± 5 Ma and 1933 ± 2 Ma. This charnockitic magmatism may be related to a post-collisional setting after the evolution of the Cauarane-Coeroeni Belt (~2.00 Ga), or may represent a post-collisional (or intracontinental?) magmatism related to orogenic activities along the plate margins around 1.95–1.94 Ga. |
| |
Keywords: | Geochronology Charnockitic magmatism Paleoproterozoic Guyana shield Amazonian craton |
本文献已被 ScienceDirect 等数据库收录! |
|