Goy, J.L. and Corvea, J.L. and Martínez-Graña, A.M. and Zazo, C. and Dabrio, C.J. and Nieto, C.E. and De Bustamante, I. (2026) Geomorphotectonic approach to geology of the Viñales National Park, Cuba. Journal of Maps, 22 (1). p. 2614771.
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Geomorphotectonic approach to geology of the Vi ales National Park Cuba.pdf - Published Version Available under License Creative Commons Attribution Non-commercial. Download (7Mb) | Preview |
Abstract
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.
| Item Type: | Article |
|---|---|
| Subjects: | Q Science > QE Geology |
| Depositing User: | José Ángel Gómez Martín |
| Date Deposited: | 05 Feb 2026 07:19 |
| Last Modified: | 05 Feb 2026 07:33 |
| URI: | http://eprints.imdea-agua.org:13000/id/eprint/1790 |
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