RT Journal Article
T1 Geomorphotectonic approach to geology of the Viñales National Park, Cuba
A1 Goy Goy, José Luis
A1 Corvea, Jose Luis
A1 Martinez-Graña, 
A1 Zazo Cardeña, Caridad
A1 Dabrio González, Cristino José
A1 Nieto, Carlos E.
A1 Bustamante, Irene de
AB 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.
PB Taylor and Francis
YR 2026
FD 2026-02-03
LK https://hdl.handle.net/20.500.14352/133084
UL https://hdl.handle.net/20.500.14352/133084
LA eng
NO 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
NO MCIN/AEI/ 10.13039/501100011033
NO Universidad de Salamanca
DS Docta Complutense
RD 11 abr 2026