Zobrazeno 1 - 4
of 4
pro vyhledávání: '"María Isabel Hernández-Ocaña"'
Autor:
Elizabeth Chacón-Baca, Felipe Torres de la Cruz, Gabriel Chávez-Cabello, María Isabel Hernández-Ocaña
Publikováno v:
Revista Mexicana de Ciencias Geológicas. 37:9-25
Depositional episodes are readily identified along representative localities of the Lower Cretaceous Cupido platform in northeastern Mexico. The basal part of the Cupido Formation exhibits a progradational reef platform that, at the upper limit, is t
Autor:
María Isabel Hernández-Ocaña, Samuel Eguiluz de Antuñano, Felipe Torres de la Cruz, Gabriel Chávez-Cabello, Elizabeth Chacón-Baca, Sara A. Quiroz-Barroso
Publikováno v:
Journal of South American Earth Sciences. 90:107-117
The present paper address the occurrence of Venericardia shell concentrations distributed over hundreds of meters along terrigenous horizons as a typical sedimentary facies of the Wilcox Formation in the Burgos Basin. These extensive deposits overlie
Autor:
Elizabeth Chacón-Baca, Felipe Torres de la Cruz, Gabriel Chávez-Cabello, Sara A. Quiroz-Barroso, María Isabel Hernández-Ocaña, Samuel Eguiluz de Antuñano
Publikováno v:
Journal of South American Earth Sciences. 98:102350
The Jenchen's comment appears to assume that Venericardia and Ophiomorpha were the main objectives in our work and that we used random criteria to assign genera. However our paper addressed the presence of previously reported V. and Oph. from new loc
Publikováno v:
Universidad Nacional Autónoma de México
UNAM
Redalyc-UNAM
Boletín de la Sociedad Geológica Mexicana (México) Num.2 Vol.70
UNAM
Redalyc-UNAM
Boletín de la Sociedad Geológica Mexicana (México) Num.2 Vol.70
espanolUna de las sucesiones mas completas de rocas paleozoicas de Mexico aflora en el sur de su territorio, en el area de Santiago Ixtaltepec, en el estado de Oaxaca. En esta sucesion, las rocas carboniferas corresponden a las formaciones Santiago (
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::e98da2937fadc136c6ee6451e72d3113
https://www.redalyc.org/articulo.oa?id=94362562005
https://www.redalyc.org/articulo.oa?id=94362562005