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Oil and Gas Exploration in Cuba - Geological-Structural Cartography using Potential Fields and Airborne Gamma Spectrometry (Paperback, 1st ed. 2017)
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Oil and Gas Exploration in Cuba - Geological-Structural Cartography using Potential Fields and Airborne Gamma Spectrometry (Paperback, 1st ed. 2017)
Series: SpringerBriefs in Earth System Sciences
Expected to ship within 10 - 15 working days
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A summary of the results achieved in the geological-structural
mapping, by potential fields and airborne gamma spectrometry data,
of the units of igneous and metamorphic rocks in the western
regions (Havana-Matanzas), central (Cienfuegos, Villa Clara-Sancti
Spiritus) and central-eastern (Camaguey-Las Tunas-Holguin) of Cuba
is presented. In addition, the structural- tectonic regionalization
with hydrocarbon exploration purposes, focusing mapping of possible
new oil-gas targets in the regions of Land Blocks 9, 23 and 17-18
are detailed in this volume. In certain case study locations
(Majaguillar, North Motembo, Guamutas and Maniabon) reconnaissance
work by a profile of Redox Complex (complex of unconventional
geophysical-geochemical exploration techniques) was performed with
positive results. In an attempt to contribute to the
geological-structural mapping of the metamorphic massif Isla de la
Juventud, with emphasis on acid magmatism, the gravi-magnetometric
data is used. According to the results, the presumed post
metamorphic granitic bodies of low density are located, mainly, in
the central and southwestern part of the massif. The granitic
bodies apparently were introduced through the system of
longitudinal faults (syn metamorphic) and transverse (post
metamorphic) at the end of the process multyfolding and
metamorphism of the massif sequences, taking a leading role the
deep longitudinal fracture zones of sublatitudinal direction in the
central and southern part of the massif. On the map of the magnetic
field vertical derivative the anomalies, basically, reflected the
direction and limits of the folded tectonic structure, the
development area of volcanogenic rocks, the presumed development
zones of migmatitic rocks and tectonised rocks in North and center
of the massif, respectively, and the prevailing direction of the
main tectonic dislocations.
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