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Delve into the captivating geology of Cuba in this in-depth study, covering geological history, tectonic units, mineral resources, and more. Discover the island's rich landscapes and natural resources, from mineral waters to oil and gas deposits. Explore the intriguing tectonic units like the Northern Foldbelt and Guaniguanico terrane, and learn about the region's stratigraphy and metamorphic terranes. Unravel the geological evolution of Cuba, from the Paleogene volcanic arc to the Synorogenic Basins, providing valuable insights into the island's geological heritage. Witness the geological marvels that make Cuba a unique destination for alien planetologists.
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Overview of the Geology of Cuba Overview of the Geology of Cuba Manuel A. Iturralde-Vinent Cuban Academy of Sciences Manuel A. Iturralde-Vinent Cuban Academy of Sciences
1869 Geological research and cartography in Cuba started in the second half of the XIX Century FIRST GEOLOGICAL MAP
The origin of the island have been explained according to the theories of Geosyncline, Continental Drift, Oceanization, Tectonic Layering, Earth Expansion, Surge Tectonics and several models of Plate Tectonics.
IfalienplanetologistseverlandonEarth, itwillbe in Cuba IfalienplanetologistseverlandonEarth, itwillbe in Cuba
WATER DEPOSITS Mineral waters UNDERGROUND KARSTIC BASINS LIMITED UNDERGROUND WATERS HOT SPRINGS
Oil and Gas Gulf of Mexico prospecting area OIL AND GAS Dense crude oil belt
Industrial minerals MARBLES, QUARTZ & QUARTZ SANDS, BARITE, CLAY MINERALS, ZEOLITE, SEMIPRECIOUS MINERALS, CONSTRUCTION MATERIALS, SOIL.
The Northern Foldbelt and the Guaniguanicoterrane GUANIGUANICO NORTHERN FOLDBELT
The stratigraphy of the Northern Foldbelt and Guaniguanico POST OROGENIC FOREDEEP CONTINENTAL MARGIN
Stratigraphy of Caribeana POST OROGENIC SUBDUCTION /EXHUMATION CONTINENTAL MARGIN
´ ´ Caribeana LowerCretaceouspaleogeography Location of the Caribeana submarine platform
The subduction melange: Blocks of HP/LT rocks Some of this rocks are dated as 120 Ma.
Synorogenic basins NORTHERN FOLDBELT GUANIGUANICO TERRANE PIGGYBACK BASINS
K SYNOROGENIC BASINS Onto the volcanics and mafic-ultramafic rocks Pg K
Latest Eocene to Recent BASINS UPLIFT
The evolution continues 2008 1941 2009 1955 - 1997 LOST
VII International EarthScienceConvention April 2017, La Habana www.cubacienciasdelatierra.com
THE SYNOROGENIC BASINS Olistostromes between the volcanics thrust front and the underlying mafic-ultramafic allochthon.