Go to:
Logótipo
Você está em: Start > Publications > View > Discussion on the Rb-Sr age determination of Porto granite: Implications of the 87Rb decay constant [Discussão sobre a determinação da idade do granito do Porto pelo sistema Rb-Sr: Implicações do valor da constante de decaimento do 87Rb]
Map of Premises
Principal
Publication

Discussion on the Rb-Sr age determination of Porto granite: Implications of the 87Rb decay constant [Discussão sobre a determinação da idade do granito do Porto pelo sistema Rb-Sr: Implicações do valor da constante de decaimento do 87Rb]

Title
Discussion on the Rb-Sr age determination of Porto granite: Implications of the 87Rb decay constant [Discussão sobre a determinação da idade do granito do Porto pelo sistema Rb-Sr: Implicações do valor da constante de decaimento do 87Rb]
Type
Article in International Scientific Journal
Year
2015
Authors
Maria Ângela Almeida
(Author)
FCUP
View Personal Page You do not have permissions to view the institutional email. Search for Participant Publications View Authenticus page View ORCID page
Santos, JF
(Author)
Other
The person does not belong to the institution. The person does not belong to the institution. The person does not belong to the institution. Without AUTHENTICUS Without ORCID
Noronha, F
(Author)
Other
The person does not belong to the institution. The person does not belong to the institution. The person does not belong to the institution. Without AUTHENTICUS Without ORCID
Journal
Vol. 102
Pages: 143-145
ISSN: 0873-948X
Indexing
Other information
Authenticus ID: P-00M-WVC
Abstract (EN): The determination of absolute ages by isotopic systematics is an indispensable datum to constrain the petrogenesis and evolution conditions of a rock, being a contribution to a better characterization of the geological and tectonic settings. The granitic rocks of Porto region have been the object of several isotopic and geochronological studies that have allowed a comparative approach by different methods, namely U-Pb, Rb-Sr and Sm-Nd. The age determination of the Porto peraluminous two-mica granite by the Rb-Sr systematics based on recent estimates of the 87Rb decay constant, assumed as more accurate than the constant usually recommended, suggests the age of 311±7 Ma for the emplacement of the Porto granite. This age is in agreement with the affiliation of Porto granite to the group of syn-tectonic granites related with the third Hercynian deformation phase. The present results are more concordant with the U-Pb ages reported in previous works for zircon and monazite of the same granite. © 2015 LNEG - Laboratório Nacional de Geologia e Energia IP.
Language: Portuguese
Type (Professor's evaluation): Scientific
Documents
We could not find any documents associated to the publication.
Related Publications
Recommend this page Top
Copyright 1996-2025 © Faculdade de Medicina Dentária da Universidade do Porto  I Terms and Conditions  I Acessibility  I Index A-Z
Page created on: 2025-08-08 at 23:54:25 | Privacy Policy | Personal Data Protection Policy | Whistleblowing | Electronic Yellow Book