2026-08-16T05:38:30Zhttps://docta.ucm.es/rest/oai/request

oai:docta.ucm.es:20.500.14352/1330842026-02-25T00:51:41Zcom_20.500.14352_14col_20.500.14352_15

Goy Goy, José Luis Corvea, Jose Luis Martinez-Graña Zazo Cardeña, Caridad Dabrio González, Cristino José Nieto, Carlos E. Bustamante, Irene de 2026-02-24T15:29:04Z 2026-02-24T15:29:04Z 2026-02-03 Goy, J. L., Corvea, J. L., Martinez-Graña, A. M., Zazo, C., Dabrio, C. J., Nieto, C. E., & De Bustamante, I. (2026). Geomorphotectonic approach to geology of the viñales national park, cuba. Journal of Maps, 22(1), 2614771. https://doi.org/10.1080/17445647.2026.2614771 10.1080/17445647.2026.2614771 https://hdl.handle.net/20.500.14352/133084 1744-5647 https://doi.org/10.1080/17445647.2026.2614771 https://www.tandfonline.com/doi/full/10.1080/17445647.2026.2614771 The geological substratum of Viñales National Park is crossed by fractures and over-thrusts. It includes siliciclastic (Jurassic San Cayetano Formation), carbonate (Late Jurassic to Early Eocene Jagua, Guasasa, Pons and Ancón Formations) and olistostrome (Early-Middle Eocene Manacas Formation) rocks, covered by Quaternary deposits. Cartographic methodology includes Fundamental maps (geologic formations, Quaternary, tectonics and geomorphology) and Auxiliary maps (substratum-structures-drainage, slopes and lithology). Auxiliary maps provide basic information, whereas fundamental maps contribute, by means of superposition and selection, to elaborating the final geomorph-tectonic map as an essential part of the geological map. Results and conclusions are derived from the various cartographies. eng http://creativecommons.org/licenses/by-nc/4.0/ open access Attribution-NonCommercial 4.0 International Geomorphotectonic approach to geology of the Viñales National Park, Cuba journal article