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Graciete Tavares Dias
AuthID:
R-000-5N1
Publications
Confirmed
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Document Type:
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Article (5)
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Order:
Year Dsc
Year Asc
Cit. WOS Dsc
IF WOS Dsc
Cit. Scopus Dsc
IF Scopus Dsc
Title Asc
Title Dsc
Results:
10
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Confirmed Publications: 5
1
TITLE:
Mantle-like Sr-Nd isotope composition of Fe-K subalkaline granites: the Peneda-Geres Variscan massif (NW Iberian Peninsula). Mantle-like composition of subalkaline granites
Full Text
AUTHORS:
Mendes, AC
;
Dias, G
;
PUBLISHED:
2004
,
SOURCE:
TERRA NOVA,
VOLUME:
16,
ISSUE:
3
INDEXED IN:
Scopus
WOS
CrossRef
IN MY:
ORCID
2
TITLE:
Mantle and crustal sources in the genesis of late-Hercynian granitoids (NW Portugal): Geochemical and Sr-Nd isotopic constraints
Full Text
AUTHORS:
Dias, G
;
Simoes, PP
; Ferreira, N;
Leterrier, J
;
PUBLISHED:
2002
,
SOURCE:
31st International Geological Congress
in
GONDWANA RESEARCH,
VOLUME:
5,
ISSUE:
2
INDEXED IN:
Scopus
WOS
CrossRef
IN MY:
ORCID
3
TITLE:
U-Pb zircon and monazite geochronology of post-collisional Hercynian granitoids from the Central Iberian Zone (Northern Portugal)
Full Text
AUTHORS:
Dias, G
;
Leterrier, J
;
Mendes, A
;
Simoes, PP
; Bertrand, JM;
PUBLISHED:
1998
,
SOURCE:
Symposium 55 on Post-Collisional Magmatism
in
LITHOS,
VOLUME:
45,
ISSUE:
1-4
INDEXED IN:
Scopus
WOS
CrossRef
IN MY:
ORCID
4
TITLE:
Petrology and geochemistry of late-Hercynian subalkaline plutonism in the Central Iberian Zone; the Peneda-Gerês granitic massif [Pétrologie et géochimie du plutonisme subalcalin tardi-hercynien de la Zone Centro-Ibérique: Le massif granitique de Peneda-Gerês]
Full Text
AUTHORS:
Mendes, A;
Dias, G
;
PUBLISHED:
1996
,
SOURCE:
Comptes Rendus de l'Academie de Sciences - Serie IIa: Sciences de la Terre et des Planetes,
VOLUME:
323,
ISSUE:
8
INDEXED IN:
Scopus
IN MY:
ORCID
5
TITLE:
THE GENESIS OF FELSIC-MAFIC PLUTONIC ASSOCIATIONS - A SR AND ND ISOTOPIC STUDY OF THE HERCYNIAN BRAGA GRANITOID MASSIF (NORTHERN PORTUGAL)
Full Text
AUTHORS:
DIAS, G
;
LETERRIER, J
;
PUBLISHED:
1994
,
SOURCE:
LITHOS,
VOLUME:
32,
ISSUE:
3-4
INDEXED IN:
Scopus
WOS
IN MY:
ORCID
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