| dc.contributor | Univ Barcelona | |
| dc.creator | Gilles Levresse | |
| dc.creator | Pinto Linares, Porfirio Julio | |
| dc.date | 2018-03-22T23:17:33Z | |
| dc.date | 2018-03-22T23:17:33Z | |
| dc.date | 2007 | |
| dc.date.accessioned | 2023-07-17T22:04:22Z | |
| dc.date.available | 2023-07-17T22:04:22Z | |
| dc.identifier | G. P. R. LEVRESSE, J. TRITLLA I CAMBRA, E. DELOULE, P. J. PINTO LINARES. Is there a Grenvillian basement in the Guerrero-Morelos Platform of Mexico?. Geologica Acta, Vol.5, Nº 2, 2007, 167-175, | |
| dc.identifier | http://hdl.handle.net/11627/3562 | |
| dc.identifier | http://dx.doi.org/10.1344/105.000000302 | |
| dc.identifier.uri | https://repositorioslatinoamericanos.uchile.cl/handle/2250/7543923 | |
| dc.description | "In the Guerrero-Morelos platform (Guerrero State, Mexico) the adakitic rocks of Early Tertiary age contain abundant hornblende-rich tonalite xenoliths. Zircon crystals have been concentrated from both adakites and xenoliths, and dated using in-situ U-Pb ion microprobe analyses. These analyses indicate the presence of inherited Grenvillian and early Triassic/late Permian crust ages, as well as a Paleocene age related with the adakite rock intrusion. This range of inherited ages is reported for the first time in the Guerrero-Morelos platform, suggesting that a continous Grenvillian crust exists between the Oaxacan complex,to the East, and the Guerrero-Morelos platform." | |
| dc.format | application/pdf | |
| dc.rights | Attribution-NonCommercial-NoDerivatives 4.0 Internacional | |
| dc.rights | http://creativecommons.org/licenses/by-nc-nd/4.0/ | |
| dc.rights | Acceso Abierto | |
| dc.subject | U-Pb dating | |
| dc.subject | Zircon | |
| dc.subject | Guerrero | |
| dc.subject | Grenvillian Age | |
| dc.subject | CIENCIAS FÍSICO MATEMÁTICAS Y CIENCIAS DE LA TIERRA | |
| dc.title | Is there a grenvillian basement in the Guerrero-Morelos platform of Mexico? | |
| dc.type | article | |
