Zobrazeno 1 - 6
of 6
pro vyhledávání: '"Edith Fuentes-Guzmán"'
Autor:
Edith Fuentes-Guzmán, Antoni Camprubí, Eduardo González-Partida, Geovanny Hernández-Avilés, Pura Alfonso, Edith Cienfuegos-Alvarado, Juan Carlos Mesino-Hernández, Carlos Ortega-Obregón, Francisco J. Otero-Trujano, Juan Tomás Vázquez Ramírez
Publikováno v:
Journal of South American Earth Sciences. 122:104112
This paper stems from the dissertations of E.F.G., G.H.A. and, partly, J.C.M.H., who acknowledge the support of CONACyT through their respective PhD (E.F.G.) and MSc grants (G.H.A. and J.C.M.H.). Funding for this work was provided by CONACyT through
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::f406a9d67bc60206b3f0ac515f60fa94
https://doi.org/10.1016/j.jsames.2022.104112
https://doi.org/10.1016/j.jsames.2022.104112
Autor:
Geovanny Hernández-Avilés, Janet Gabites, Antoni Camprubí, Eduardo González-Partida, Edith Fuentes-Guzmán, Alexander Iriondo, Giovanni Ruggieri, Margarita López-Martínez
Publikováno v:
Boletín de la Sociedad Geológica Mexicana. 72
The Cu- and Au-rich Tatatila–Las Minas IOCG skarn deposits in Veracruz (central-east Mexico) are circumscribed to the earliest stages of the Trans-Mexican Volcanic Belt (TMVB) and stand for a metallogenic province directly linked to its tectonomagm
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b77d0e3d681ae99fa99bd20255ad8524
https://doi.org/10.18268/bsgm2020v72n3a110520
https://doi.org/10.18268/bsgm2020v72n3a110520
Autor:
Eduardo González-Partida, Edith Fuentes-Guzmán, Antoni Camprubí, Janet Gabites, Vanessa Colás
Publikováno v:
Universidad Nacional Autónoma de México
UNAM
Redalyc-UNAM
Boletín de la Sociedad Geológica Mexicana (México) Num.3 Vol.72
UNAM
Redalyc-UNAM
Boletín de la Sociedad Geológica Mexicana (México) Num.3 Vol.72
The Xoconostle prospect in northeastern Michoacán state, south-central Mexico, is constituted by high sulfidation epithermal breccias and stockworks with Au and Hg prospective anomalies. The mineralization is hosted by latest Miocene to Pliocene roc
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::68fbede6c1a5423008c234fd04c693ad
https://www.redalyc.org/articulo.oa?id=94370787019
https://www.redalyc.org/articulo.oa?id=94370787019
Autor:
Luis F. Auqué, Edith Fuentes-Guzmán, Pilar Ortega-Larrocea, Antoni Camprubí, Vanessa Colás, Eduardo González-Partida, María Colín-García, Janet Gabites
Publikováno v:
Zaguán. Repositorio Digital de la Universidad de Zaragoza
instname
Zaguán: Repositorio Digital de la Universidad de Zaragoza
Universidad de Zaragoza
Universidad Nacional Autónoma de México
UNAM
Redalyc-UNAM
Boletín de la Sociedad Geológica Mexicana (México) Num.3 Vol.72
instname
Zaguán: Repositorio Digital de la Universidad de Zaragoza
Universidad de Zaragoza
Universidad Nacional Autónoma de México
UNAM
Redalyc-UNAM
Boletín de la Sociedad Geológica Mexicana (México) Num.3 Vol.72
The Ntacamaxtithin area in northern Puebla (central Mexico) contains middle Miocene Cu-Mo-Au porphyry/skarn and Pliocene low-sulfidation Au-Ag epithermal deposits that are geologically associated with the evolution of the Timis-Mexican Volcanic Belt
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::97e2e890ef320122dfe9abf4325721b5
http://zaguan.unizar.es/record/98205
http://zaguan.unizar.es/record/98205
Autor:
Edith Fuentes-Guzmán, Eduardo González-Partida, Antoni Camprubí, Geovanny Hernández-Avilés, Janet Gabites, Alexander Iriondo, Giovanni Ruggieri, Margarita López-Martínez
Publikováno v:
Universidad Nacional Autónoma de México
UNAM
Redalyc-UNAM
Boletín de la Sociedad Geológica Mexicana (México) Num.3 Vol.72
UNAM
Redalyc-UNAM
Boletín de la Sociedad Geológica Mexicana (México) Num.3 Vol.72
"The Cu- and Au-rich Tatatila-Las Minas IOCG skarn deposits in Veracruz (central-east Mexico) are circumscribed to the earliest stages of the Trans-Mexican Volcanic Belt (TMVB) and stand for a metallogenic province directly linked to its tectonomagma
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______3056::6ef365acbfc23f5dfc3319e4d5bcfdad
https://www.redalyc.org/articulo.oa?id=94370787008
https://www.redalyc.org/articulo.oa?id=94370787008
Autor:
Luis E. González-Ruiz, Claire Legouix, Antoni Camprubí, Daniel González-Ruiz, Marie-Christine Boiron, Edith Fuentes-Guzmán, Eduardo González-Partida, César F. Aguilar-Ramírez, Antonin Richard
Publikováno v:
Minerals
Minerals, MDPI, 2019, 9 (1), pp.58. ⟨10.3390/min9010058⟩
Volume 9
Issue 1
Minerals, Vol 9, Iss 1, p 58 (2019)
Minerals, MDPI, 2019, 9 (1), pp.58. ⟨10.3390/min9010058⟩
Volume 9
Issue 1
Minerals, Vol 9, Iss 1, p 58 (2019)
The formation of most fluorite deposits in northern Coahuila (NE Mexico) is explained by MVT models, and is a part of the metallogenic province of northeastern Mexico. However, fluorite skarn deposits also occur in the same region, and there is evide
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::b90817952714303b747db75252706b93
https://doi.org/10.3390/min9010058
https://doi.org/10.3390/min9010058