Zobrazeno 1 - 10
of 157
pro vyhledávání: '"J. Guimerà"'
Autor:
X.A. Sabaté Arroyo, F. Grases Freixedas, J. L. Bauzà Quetglas, J. Guimerà Garcia, E. Pieras Ayala
Publikováno v:
BMC Urology, Vol 20, Iss 1, Pp 1-6 (2020)
Abstract Background Our purpose was to study the relationship of the 3 different types of endoscopic calcifications of the renal papilla (Randall’s plaque, intratubular calcification, papillary crater) with the type of stone and urine analysis. Met
Externí odkaz:
https://doaj.org/article/e1d11fdd6b7743c3ba1094e8a5a88828
Publikováno v:
European Urology Open Science, Vol 19, Iss , Pp e2216- (2020)
Externí odkaz:
https://doaj.org/article/a5e75efb58974264967418f9d52a0586
Publikováno v:
European Urology Open Science, Vol 19, Iss , Pp e2335- (2020)
Externí odkaz:
https://doaj.org/article/76dd38d5f8cd4012845ede2c54be928e
Autor:
J.L. Bauza Quetglas, E. Pieras, P. Murthy, V. Tubau, M. De La Cruz, A. Martínez, J. Guimerà, D. Sagalovich, R. Bertolo, J. Kaouk
Publikováno v:
European Urology Open Science, Vol 19, Iss , Pp e2394- (2020)
Externí odkaz:
https://doaj.org/article/b02146af89634575b7953a6c01baa3c5
Publikováno v:
Geologica Acta, Vol 18 (2020)
The present study provides new data of the Middle-Upper Triassic successions and their deformation in the eastern Iberian Chain, where contractional tectonics during the Cenozoic disrupted this Mediterranean type of Triassic rocks. The succession, di
Externí odkaz:
https://doaj.org/article/8ca9aaf27a11449ba96bf3ae818c60cf
Autor:
J. Guimerà
Publikováno v:
Geologica Acta, Vol 16, Iss 4.6, Pp 427-438 (2018)
The Iberian Chain is a complex intraplate fold-and-thrust belt resulting from the convergence between the Eurasian, Iberian and African plates during the late Eocene to the Miocene. The main trend of its contractional structures is NW-SE, but E-W, N
Externí odkaz:
https://doaj.org/article/304b2f55f5bc436ea029331dc2253384
Autor:
J. Guimerà
Publikováno v:
Estudios Geologicos, Vol 43, Iss 1-2, Pp 63-69 (1987)
No disponible
Externí odkaz:
https://doaj.org/article/42428ccfc76e48b883c9fe8ab99b5404
Akademický článek
Tento výsledek nelze pro nepřihlášené uživatele zobrazit.
K zobrazení výsledku je třeba se přihlásit.
K zobrazení výsledku je třeba se přihlásit.
Autor:
R. Guldris, E. Pieras, V. Tubau, M. De La Cruz, A. Martínez, P. Benito, A. Tienza, J. Guimerà, J. Bauzà, M. Amer
Publikováno v:
European Urology Open Science. 44:S417
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9192e6d39e8e2334ed6de6912e1541b3
https://doi.org/10.1016/s2666-1683(22)02264-9
https://doi.org/10.1016/s2666-1683(22)02264-9
Publikováno v:
Recercat: Dipósit de la Recerca de Catalunya
Varias* (Consorci de Biblioteques Universitáries de Catalunya, Centre de Serveis Científics i Acadèmics de Catalunya)
Ortí, F, Guimerà, J & Goetz, A E 2020, ' Middle-Upper Triassic stratigraphy and structure of the Alt Palància (eastern Iberian Chain): a multidisciplinary approach ', Geologica Acta, vol. 18, 4 . https://doi.org/10.1344/GeologicaActa2020.18.4
Dipòsit Digital de la UB
Universidad de Barcelona
Dipòsit Digital de Documents de la UAB
Universitat Autònoma de Barcelona
Recercat. Dipósit de la Recerca de Catalunya
instname
Geologica Acta; Vol. 18 (2020); 1-26, I-II
RCUB. Revistas Científicas de la Universidad de Barcelona
Varias* (Consorci de Biblioteques Universitáries de Catalunya, Centre de Serveis Científics i Acadèmics de Catalunya)
Ortí, F, Guimerà, J & Goetz, A E 2020, ' Middle-Upper Triassic stratigraphy and structure of the Alt Palància (eastern Iberian Chain): a multidisciplinary approach ', Geologica Acta, vol. 18, 4 . https://doi.org/10.1344/GeologicaActa2020.18.4
Dipòsit Digital de la UB
Universidad de Barcelona
Dipòsit Digital de Documents de la UAB
Universitat Autònoma de Barcelona
Recercat. Dipósit de la Recerca de Catalunya
instname
Geologica Acta; Vol. 18 (2020); 1-26, I-II
RCUB. Revistas Científicas de la Universidad de Barcelona
The present study provides new data of the Middle-Upper Triassic successions and their deformation in the eastern Iberian Chain, where contractional tectonics during the Cenozoic disrupted this Mediterranean type of Triassic rocks. The succession, di
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::9f62e844ce7bf2e3a1d4e51ac7d22c24
http://hdl.handle.net/2072/442778
http://hdl.handle.net/2072/442778
