Oil and Gas Exploration in Cuba: Geological-Structural by Manuel Enrique Pardo Echarte,Jorge Luis Cobiella Reguera

By Manuel Enrique Pardo Echarte,Jorge Luis Cobiella Reguera

A summary of the implications completed within the geological-structural mapping, by means of power fields and airborne gamma spectrometry info, of the devices of igneous and metamorphic rocks within the western areas (Havana-Matanzas), vital (Cienfuegos, Villa Clara-Sancti Spiritus) and central-eastern (Camagüey-Las Tunas-Holguín) of Cuba is gifted. In addition, the structural- tectonic regionalization with hydrocarbon exploration reasons, focusing mapping of attainable new oil-gas objectives within the areas of Land Blocks nine, 23 and 17-18 are unique during this quantity. In definite case examine destinations (Majaguillar, North Motembo, Guamutas and Maniabón) reconnaissance paintings via a profile of Redox Complex (complex of unconventional geophysical-geochemical exploration innovations) was once played with optimistic effects.

In an try and give a contribution to the geological-structural mapping of the metamorphic massif Isla de los angeles Juventud, with emphasis on acid magmatism, the gravi-magnetometric info is used. in response to the implications, the presumed publish metamorphic granitic our bodies of low density can be found, in general, within the significant and southwestern a part of the massif. The granitic our bodies it sounds as if have been brought throughout the approach of longitudinal faults (syn metamorphic) and transverse (post metamorphic) on the finish of the method multyfolding and metamorphism of the massif sequences, taking a number one function the deep longitudinal fracture zones of sublatitudinal path within the critical and southern a part of the massif. at the map of the magnetic box vertical spinoff  the anomalies, essentially, mirrored the course and boundaries of the folded tectonic constitution, the improvement region of ​​ volcanogenic rocks, the presumed improvement zones of migmatitic rocks and tectonised rocks in North and heart of the massif, respectively, and the existing course of the most tectonic dislocations.

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