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Detalhes Referência

Tipo
Artigos em Revista

Tipo de Documento
Artigo Completo

Título
Magmatic evolution in the N-Gondwana margin related to the opening of the Rheic Ocean - Evidence from the Upper Parautochthon of the Galicia-Trás-os-Montes Zone and from the Central Iberian Zone (NW Iberian Massif)

Participantes na publicação
Dias da Silva I (Author)
Dep. Geologia
 IDL
 IDL
 Díez Fernández R (Author)
Díez Montes A (Author)
González Clavijo E (Author)
Foster DA (Author)

Data de Publicação
2015

Suporte
INTERNATIONAL JOURNAL OF EARTH SCIENCES

Identificadores da Publicação
ISSN - 1437-3254

Identificadores do Documento
DOI - https://doi.org/10.1007/s00531-015-1232-9

Identificadores de Qualidade
Web Of Science Q2 (2018) - 2.295 - GEOSCIENCES, MULTIDISCIPLINARY - SCIE
SCIMAGO Q1 (2018) - 1.164 - Earth and Planetary Sciences (miscellaneous)
SCOPUS Q1 (2017) - 1.125 - General Earth and Planetary Sciences
Web Of Science Q2 (2019) - 2.278 - GEOSCIENCES, MULTIDISCIPLINARY - SCIE
SCOPUS Q1 (2019) - 4.1 - General Earth and Planetary Sciences
SCIMAGO Q1 (2019) - 1.048 - Earth and Planetary Sciences (miscellaneous)


Exportar referência

APA
Dias da Silva I, Díez Fernández R, Díez Montes A, González Clavijo E, Foster DA, (2015). Magmatic evolution in the N-Gondwana margin related to the opening of the Rheic Ocean - Evidence from the Upper Parautochthon of the Galicia-Trás-os-Montes Zone and from the Central Iberian Zone (NW Iberian Massif). INTERNATIONAL JOURNAL OF EARTH SCIENCES, ISSN 1437-3254. eISSN .

IEEE
Dias da Silva I, Díez Fernández R, Díez Montes A, González Clavijo E, Foster DA, "Magmatic evolution in the N-Gondwana margin related to the opening of the Rheic Ocean - Evidence from the Upper Parautochthon of the Galicia-Trás-os-Montes Zone and from the Central Iberian Zone (NW Iberian Massif)" in INTERNATIONAL JOURNAL OF EARTH SCIENCES, 2015. 10.1007/s00531-015-1232-9

BIBTEX
@article{31284, author = {Dias da Silva I and Díez Fernández R and Díez Montes A and González Clavijo E and Foster DA}, title = {Magmatic evolution in the N-Gondwana margin related to the opening of the Rheic Ocean - Evidence from the Upper Parautochthon of the Galicia-Trás-os-Montes Zone and from the Central Iberian Zone (NW Iberian Massif)}, journal = {INTERNATIONAL JOURNAL OF EARTH SCIENCES}, year = 2015, }