Neoarchean crustal growth by accretionary processes: Evidence from combined zircon–titanite U–Pb isotope studies on granitoid rocks around the Hutti greenstone belt, eastern Dharwar Craton, India.


Autoria(s): Anand, R; Balakrishnan, S; Kooijman, E; Mezger, Klaus
Data(s)

2014

Formato

application/pdf

Identificador

http://boris.unibe.ch/46186/1/mezger_anand.pdf

Anand, R; Balakrishnan, S; Kooijman, E; Mezger, Klaus (2014). Neoarchean crustal growth by accretionary processes: Evidence from combined zircon–titanite U–Pb isotope studies on granitoid rocks around the Hutti greenstone belt, eastern Dharwar Craton, India. Journal of Asian earth sciences, 79, pp. 72-85. Elsevier 10.1016/j.jseaes.2013.09.017 <http://dx.doi.org/10.1016/j.jseaes.2013.09.017>

doi:10.7892/boris.46186

info:doi:10.1016/j.jseaes.2013.09.017

urn:issn:1367-9120

Idioma(s)

eng

Publicador

Elsevier

Relação

http://boris.unibe.ch/46186/

Direitos

info:eu-repo/semantics/restrictedAccess

Fonte

Anand, R; Balakrishnan, S; Kooijman, E; Mezger, Klaus (2014). Neoarchean crustal growth by accretionary processes: Evidence from combined zircon–titanite U–Pb isotope studies on granitoid rocks around the Hutti greenstone belt, eastern Dharwar Craton, India. Journal of Asian earth sciences, 79, pp. 72-85. Elsevier 10.1016/j.jseaes.2013.09.017 <http://dx.doi.org/10.1016/j.jseaes.2013.09.017>

Palavras-Chave #550 Earth sciences & geology
Tipo

info:eu-repo/semantics/article

info:eu-repo/semantics/publishedVersion

PeerReviewed