Cu-ID: https://cu-id.com/2277/v15n2e78 Redirecciones: 82 URL: https://rgi.edicionescervantes.com/index.php/rgi/article/view/78 OAI: https://rgi.edicionescervantes.com/index.php/rgi/oai?verb=GetRecord&metadataPrefix=oai_dc&identifier=oai:ojs.pkp.sfu.ca:article/78 BibTeX: @article{GEOLOGICAL_AND_GEOCHMICAL_CHARACTERIZATION_OF_PINOS_TERRANE,_ISLA_DE_LA_JUVENTUD, title = {GEOLOGICAL AND GEOCHMICAL CHARACTERIZATION OF PINOS TERRANE, ISLA DE LA JUVENTUD}, author = {Peralta Barquin , Cyntia and Lastra Rivero , José Francisco and Torres Zafra , Jorge Luis}, journal = {Geoinformativa}, volume = {15}, number = {2}, pages = {76-88}, year = {2023-07-24}, publisher = { Instituto de Geología y Paleontología/Servicio Geológico de Cuba}, language = {spa}, url = {https://cu-id.com/2277/v15n2e78}, cu_id = {https://cu-id.com/2277/v15n2e78}, abstract = {Insufficient knowledge of the geochemical particularities of the Pinos Terrane, Isla de la Juventud, prevent the definition of criteria that contribute to a more effective evaluation of the existing metallic mineral potential. Therefore, in the following investigation, it is intended to determine the prospecting criteria for endogenous metallic mineral deposits through the integration and interpretation of geochemical geological information and its link with the metallogeny of the Terrain. Pinos is a metamorphic Terrain of continental, which is part of the folded substratum of Cuba. Specifically, the geochemical method used is the soil method (pedogeochemical). Based on the method, analyzing and associating the trace elements, maps of monoelemental and complex anamolies were created. The information was linked with the geology where metallogeny intervenes guided by the main deposits of endogenous origin of the territory. The research was integrated through the superposition of vectors through cartographic representations, analyzed in previous reports due to the loss of primary data. On the other hand, the fundamental tool for the integration of all the existing geoscientific information was the geographic information system (ArcGis). After integrating the information, the main mineralization controls were identified for each genetic type of mineral deposit and thus to issue criteria that allowed categorizing the prospecting sectors, which were later representend as a percentage of favorability for each genetic type of mineral deposits. As for the areas indicated with prospecting criteria, it is expected that they will be verified in the future.}, }
Cu-ID: https://cu-id.com/2277/v14n2e71 Redirecciones: 78 URL: https://rgi.edicionescervantes.com/index.php/rgi/article/view/71 OAI: https://rgi.edicionescervantes.com/index.php/rgi/oai?verb=GetRecord&metadataPrefix=oai_dc&identifier=oai:ojs.pkp.sfu.ca:article/71 BibTeX: @article{RADIOLARIANS_TAXONOMIC_LISTING_FROM_CUBAˈS_JURASSIC-CRETACEOUS, title = {RADIOLARIANS TAXONOMIC LISTING FROM CUBAˈS JURASSIC-CRETACEOUS}, author = {Pérez-Machado Milán, Osmany and Delgado Carballo, Iliana Luisa and Florez Abín, Emilio}, journal = {Geoinformativa}, volume = {14}, number = {2}, pages = {1-23}, year = {2021-10-20}, publisher = { Instituto de Geología y Paleontología/Servicio Geológico de Cuba}, language = {spa}, url = {https://cu-id.com/2277/v14n2e71}, cu_id = {https://cu-id.com/2277/v14n2e71}, abstract = {Within Cretaceous sequences, important reservoirs are reported in Cuban North Hydrocarbon Belt (FNHC). In them, siliceous facies appear in which calcareous shell microfossils are scarce or do not exist, but contain large quantities of radiolarians, making their study very important. This happens mainly in those rocks of deeper water facies, accumulated below the Carbonate Compensation Level (CCL), in which many times it is only possible to date them according to the content of radiolarians. They, in a relevant way, allow biostratigraphic determinations and more accurate paleoenvironmental analyses, in deposits where other microfossils are not abundant. In our country many investigations have been carried out on this group, fundamentally referred to petroleum activity, which have contributed to the knowledge of them, but they are dispersed and in their minority unpublished, therefore, in occasions they are of difficult access and consultation. To make a list of this taxonomic group is the main objective of this work, for which an extensive literature review was conducted, selecting the works for their contribution to the biostratigraphy of this age, resulting in species cards where a total of 32 families, 69 genera and 185 species are counted, in addition to updating the systematics and incorporating the paleontological results of more recent research.}, }
Cu-ID: https://cu-id.com/2277/v14n2e70 Redirecciones: 68 URL: https://rgi.edicionescervantes.com/index.php/rgi/article/view/70 OAI: https://rgi.edicionescervantes.com/index.php/rgi/oai?verb=GetRecord&metadataPrefix=oai_dc&identifier=oai:ojs.pkp.sfu.ca:article/70 BibTeX: @article{MENESES_MAP_SHEET_(4382-IV)_AT_SCALE_1:_50_000._GEOPHYSICAL_INTERPRETATION, title = {MENESES MAP SHEET (4382-IV) AT SCALE 1: 50 000. GEOPHYSICAL INTERPRETATION}, author = {Hechavarría Govin , Elizabeth}, journal = {Geoinformativa}, volume = {14}, number = {2}, pages = {24-38}, year = {2021-10-20}, publisher = { Instituto de Geología y Paleontología/Servicio Geológico de Cuba}, language = {spa}, url = {https://cu-id.com/2277/v14n2e70}, cu_id = {https://cu-id.com/2277/v14n2e70}, abstract = {The interpretation of geophysical data in terrain geological mapping allows to obtain information related to the geological environment and proposing the geometry of structures according to the behavior of the physical fields. The geophysical data most used in this geological task are spectrometric, gravimetric and magnetic due to their effectiveness in identifying the main lithological units and structural features, as well as mapping the main tectonic limits of the area. As part of the preparation of the Meneses cartographic sheet (4382-IV) the interpretation of gamma-spectrometric, magnetic and gravimetric data was performed, using the geophysical interpretation software Oasis Montaj and Geographic Information Systems (GIS). For this, a statistical analysis of the gamma-spectrometric data was carried out to know its variability with respect to geology and to determine the main statistics that were used to identify anomalous areas. With these data, the concentration maps of the three radioelements (K, eTh, eU), ternary maps and gamma-spectrometric relationships were made, which were interpreted. For the interpretation of the magnetic and gravimetric data, mathematical filters such as horizontal gradients and the vertical derivative were applied to identify tectonic and lithological contacts. As a final result, gamma-spectrometric units and alignments were identified and described in an integrated interpretation map.}, }
Cu-ID: https://cu-id.com/2277/v14n2e69 Redirecciones: 61 URL: https://rgi.edicionescervantes.com/index.php/rgi/article/view/69 OAI: https://rgi.edicionescervantes.com/index.php/rgi/oai?verb=GetRecord&metadataPrefix=oai_dc&identifier=oai:ojs.pkp.sfu.ca:article/69 BibTeX: @article{CABO_CRUZ–ZAPATA–SAN_CRISTOBAL_STRUCTURE,_ALINGMENT_OR_EARTHQUAKE-GENERATING_FAULT?, title = {CABO CRUZ–ZAPATA–SAN CRISTOBAL STRUCTURE, ALINGMENT OR EARTHQUAKE-GENERATING FAULT?}, author = {Pérez Aragón, Ramón O. and Echavarría Govin , Elizabeth}, journal = {Geoinformativa}, volume = {14}, number = {2}, pages = {39-52}, year = {2021-10-20}, publisher = { Instituto de Geología y Paleontología/Servicio Geológico de Cuba}, language = {spa}, url = {https://cu-id.com/2277/v14n2e69}, cu_id = {https://cu-id.com/2277/v14n2e69}, abstract = {A great alignment extends throughout the submerged area of the south of de Cuban archipelago and part of the emerged territory of western Cuba. It extends for about 660 km in a NW (328º) direction, from its beginning at a point on Oriente fault, near Cabo Cruz, in the province of Granma, to another located on the north coast of the province of Artemisa, and continues apparently towards the Gulf of Mexico. Although its line is visible to the naked eye in almost all the maps consulted, joining straight segments of the insular platform, the coast and some geological structures, it is not expressly reflected in the tectonic maps. A comparative study is carried out and the reflection of the alignment called in this work as Cabo Cruz-Zapata-San Cristobal is verified in the different thematic maps consulted (geological, tectonic, geophysical, physical, batimetric, hypsometric, seismological). The existence of historical seismic activity in the area of its intersection with the Pinar and Oriente faults, as well as along its extension is highlighted. As a result of the study, a tectonic origin is suggested, proposing to pay special attention to the Cabo Cruz-Zapata-San Cristobal alignment and to carry out geological, geophysical and seismological studies, in order to determine its genesis and geological, tectonic and earthquake-generating implications.}, }
Cu-ID: https://cu-id.com/2277/v14n2e68 Redirecciones: 86 URL: https://rgi.edicionescervantes.com/index.php/rgi/article/view/68 OAI: https://rgi.edicionescervantes.com/index.php/rgi/oai?verb=GetRecord&metadataPrefix=oai_dc&identifier=oai:ojs.pkp.sfu.ca:article/68 BibTeX: @article{THE_MARINE_GEOLOGICAL_CARTOGRAPHY_OF_CUBA,_ACHIEVEMENTS_AND_PERSPECTIVES, title = {THE MARINE GEOLOGICAL CARTOGRAPHY OF CUBA, ACHIEVEMENTS AND PERSPECTIVES}, author = {Vázquez Gainza, Betsy and Cabrera Castellano, Miguel and Pérez Aragón, Ramón Omar}, journal = {Geoinformativa}, volume = {14}, number = {2}, pages = {53-64}, year = {2021-10-20}, publisher = { Instituto de Geología y Paleontología/Servicio Geológico de Cuba}, language = {spa}, url = {https://cu-id.com/2277/v14n2e68}, cu_id = {https://cu-id.com/2277/v14n2e68}, abstract = {Cuba has achieved significant results in the geological mapping of its marine-coastal territory. Since the second half of the last century, the oceanographic institutes of Cuba and the USSR began the geological survey of the country's marine-coastal territory at a scale of 1: 1,000,000. In 1985, the Geological Research Center of MINBAS, currently the Ministry of Energy and Mines (MINEM), published the Geological Map of Cuba at scale 1: 500 000, which covered up to the insular slope. In 2016, the Institute of Geology and Paleontology-Cuban Geological Service (IGP-SGC) completed a new geological map with the same territorial extension, but at a scale of 1: 100 000. The IGP-SGC has initiated a Subprogram of the Geological Cartography of Cuba at scale 1: 50 000 (CARTAGEOL 50K), framed in the Geology Development Program until 2030, to raise the geological knowledge of the country, standardizing, increasing and completing its geological cartography. It consists of 420 sheets, 287 of them located totally or partially in marine territory. This work is carried out by the GeoCuba Empresa de GeoCuba Estudios Marinos (GEOEM) and the IGP-SGC. Its main objective is to expose the level of cartographic knowledge on the geology of the marine-coastal territory of Cuba and how it has been developing over the years, specifically within the CARTEGEOL 50K, which already has the required Methodological Instruction and the execution of 13 sheets and their respective explanatory memories, corresponding to the Santa Lucia Bay section, Pinar del Rio-Santa Fe, Havana (9 sheets); Nueva Gerona, Isle of Youth; Siboney, Santiago de Cuba and Buena Vista, Villa Clara, one in each case.}, }
Cu-ID: https://cu-id.com/2277/v14n2e67 Redirecciones: 55 URL: https://rgi.edicionescervantes.com/index.php/rgi/article/view/67 OAI: https://rgi.edicionescervantes.com/index.php/rgi/oai?verb=GetRecord&metadataPrefix=oai_dc&identifier=oai:ojs.pkp.sfu.ca:article/67 BibTeX: @article{GEOLOGICAL_PROBLEMS_OF_THE_SAFETY_OF_DAMS_AND_RESERVOIRS_IN_PANAMA:_CANAL_BASIN_((1_stARTICLE), title = {GEOLOGICAL PROBLEMS OF THE SAFETY OF DAMS AND RESERVOIRS IN PANAMA: CANAL BASIN ((1 stARTICLE)}, author = { Morelio-León, Leslie F.}, journal = {Geoinformativa}, volume = {14}, number = {2}, pages = {65-78}, year = {2021-10-20}, publisher = { Instituto de Geología y Paleontología/Servicio Geológico de Cuba}, language = {spa}, url = {https://cu-id.com/2277/v14n2e67}, cu_id = {https://cu-id.com/2277/v14n2e67}, abstract = {The geologic structure, seismics and volcanism together with paleoseismology, paleohydrology and neotec-tonics are remarkable restrictions in the management of geologic, hydrologic and structural safety of dams, lakes and the hy-draulic infrastructure. The geologic boundaries on the design, construction, operation and dam safety and in the watershed management are evaluated in this paper for two hydrologic regions of noticeable importance: The Panama Canal Basin and the Western Watersheds. In the first of two papers the background of the problem and the geological satiation of the Panama Canal is discussed. Bibliography is included at the end of the second article of the contribution.}, }
Cu-ID: https://cu-id.com/2277/v14n1e38 Redirecciones: 74 URL: https://rgi.edicionescervantes.com/index.php/rgi/article/view/38 OAI: https://rgi.edicionescervantes.com/index.php/rgi/oai?verb=GetRecord&metadataPrefix=oai_dc&identifier=oai:ojs.pkp.sfu.ca:article/38 BibTeX: @article{THE_REDISH_CLAYS_OF_THE_MARINE-_COASTAL_TERRITORY_OF_CUBA, title = {THE REDISH CLAYS OF THE MARINE- COASTAL TERRITORY OF CUBA}, author = {Cabrera Castellanos, Miguel}, journal = {Geoinformativa}, volume = {14}, number = {1}, pages = {1-8}, year = {2021-05-02}, publisher = { Instituto de Geología y Paleontología/Servicio Geológico de Cuba}, language = {spa}, url = {https://cu-id.com/2277/v14n1e38}, cu_id = {https://cu-id.com/2277/v14n1e38}, abstract = {The main objective of this article is to contribute to characterization of little known Quaternary deposits through the analysis of previous research and field observations of its author, taking into account that the deepening of geological knowledge, object of geological cartography at scale 1: 50 000, currently under development, needs to take them into account even when they are not cartographically representable, since they intervene in important events of the history of geological development. They are redish clays present in the marine-coastal territory, which can be lithified or compacted; as well as other chronologically equivalent deposits. The first ones predominate in the raised coasts of the mainland, of the keys and in the seabed, "embedded" in the karst surface of the limestones of the Jaimanitas Formation. The latter are found in the western and southeastern marine platforms, in vicinity of coastal areas, underlaying Holocene friable deposits and covering the weathered surface of limestones of Jaimanitas Formation or of the metamorphic massif from Isla de la Juventud. Taking into account that these data emanate from regional research drilling, it is probable that there are other localities with the same or similar deposits not discovered yet. As main results it was established that: the lithified clays were formed from the decalcification of limestone rocks and the cementation of insoluble iron-rich clay remains, while the compacted ones, constitute alluvial redeposits of similar clays transported from the mainland. In both cases, the process took place during the late Upper Pleistocene, as a consequence of the Wisconsin regression.}, }
Cu-ID: https://cu-id.com/2277/v14n1e37 Redirecciones: 68 URL: https://rgi.edicionescervantes.com/index.php/rgi/article/view/37 OAI: https://rgi.edicionescervantes.com/index.php/rgi/oai?verb=GetRecord&metadataPrefix=oai_dc&identifier=oai:ojs.pkp.sfu.ca:article/37 BibTeX: @article{THE_BEACH_ROCKS_FROM_CUBAN_ARCHIPELAGO, title = {THE BEACH ROCKS FROM CUBAN ARCHIPELAGO}, author = {Cabrera Castellanos, Miguel}, journal = {Geoinformativa}, volume = {14}, number = {1}, pages = {9-21}, year = {2021-05-02}, publisher = { Instituto de Geología y Paleontología/Servicio Geológico de Cuba}, language = {spa}, url = {https://cu-id.com/2277/v14n1e37}, cu_id = {https://cu-id.com/2277/v14n1e37}, abstract = {Beach rocks are well exposed deposits in the marine-coastal territory of Cuba, however, they are practically unknown and do not appear in the existing stratigraphic classifications. Since the last century, these deposits have been the object of research in different parts of the world, which have provided valuable information on their characteristics and the processes that give rise to them. In Cuba, they have been little investigated, but because they lie on the late Upper Pleistocene Jaimanites Formation and the pearly lustre still preserved on the shells and snails, they can be considered Holocene, with a diapason from contemporary still developing to older well lithified, although patches appear in the first Pleistocene terrace that could be older, genetically they are of the unnamed marine type. This work covers the entire marine-coastal territory of Cuba and is based on the author's field observations and previous research in Cuba and numerous other countries. Its aim is to draw attention to the geological-environmental interest that these deposits could have if investigated, since they constitute evidence of lithomorphogenetic processes and factors in certain coastal sectors.}, }
Cu-ID: https://cu-id.com/2277/v14n1e36 Redirecciones: 85 URL: https://rgi.edicionescervantes.com/index.php/rgi/article/view/36 OAI: https://rgi.edicionescervantes.com/index.php/rgi/oai?verb=GetRecord&metadataPrefix=oai_dc&identifier=oai:ojs.pkp.sfu.ca:article/36 BibTeX: @article{PEAT_AS_TRACES_OF_HOLOCENE_PALEOLITHIC_COASTAL_PALEOLINES_IN_CUBA, title = {PEAT AS TRACES OF HOLOCENE PALEOLITHIC COASTAL PALEOLINES IN CUBA}, author = {Cabrera Castellanos, Miguel}, journal = {Geoinformativa}, volume = {14}, number = {1}, pages = {22-29}, year = {2021-05-02}, publisher = { Instituto de Geología y Paleontología/Servicio Geológico de Cuba}, language = {spa}, url = {https://cu-id.com/2277/v14n1e36}, cu_id = {https://cu-id.com/2277/v14n1e36}, abstract = {Peat is an organic material, consisting of a light, spongy mass in which the plant components that gave rise to it are still visible. In the genetic classification of the Quaternary deposits Quaternary deposits of Cuba belong to the biogenic type. The article examines these deposits not as a mineral resource, but as traces of coastal palaeolines in the last 11700 ka of the history of geological development in the marine territory of Cuba, through their thin lenticular horizons, which alternate with other types of deposits. According to previous research peats predominate at four depth levels, with their own ages: > 14 m (probable 11.7 ka), 14-12 m (7-6 ka), 6-5 m (5.5-4.7 ka) and 3.4- 1.5 m (4.2 ka or less). The hypsometric age-position correlations should be considered as a guideline for their considered as a guideline for their application, since the values obtained are regional in nature and, moreover, are values obtained are regional in nature and, in addition, the different regions of the marine territory have been affected by neogene movements, different regions of the marine territory have been affected by neotectonic movements of different trends. What is unequivocal is that the peat deposits of the sub-seabed peat deposits are useful for the determination of coastal palaeolines and, consequently, are a valuable are therefore valuable information for reconstructing the history of the geological of the geological development of the place where they are discovered, and are an important contribution to the important contribution to the deepening of geological knowledge, which is the object of geological mapping at the of geological mapping at a scale of 1: 50 000, currently under development.}, }
Cu-ID: https://cu-id.com/2277/v14n1e35 Redirecciones: 81 URL: https://rgi.edicionescervantes.com/index.php/rgi/article/view/35 OAI: https://rgi.edicionescervantes.com/index.php/rgi/oai?verb=GetRecord&metadataPrefix=oai_dc&identifier=oai:ojs.pkp.sfu.ca:article/35 BibTeX: @article{ABOUT_MINERAL_PLACERS_IN_CUBA'S_MARINE_TERRITORY, title = {ABOUT MINERAL PLACERS IN CUBA'S MARINE TERRITORY}, author = {Cabrera Castellanos, Miguel}, journal = {Geoinformativa}, volume = {14}, number = {1}, pages = {30-37}, year = {2021-05-02}, publisher = { Instituto de Geología y Paleontología/Servicio Geológico de Cuba}, language = {spa}, url = {https://cu-id.com/2277/v14n1e35}, cu_id = {https://cu-id.com/2277/v14n1e35}, abstract = {The article is the result of the reinterpretation of existing information on heavy and precious minerals in Cuba's marine territory, as well as the geological constitution in terms of the factors and lithomorphogenetic processes involved in the formation, transport, accumulation and modification o f s ediments p resent o n t he s eabed. I t i s a contribution to the new geological mapping at a scale of 1:50 000, as it aims to re- evaluate the potential of economically exploitable placers, as well as to specify some concepts and definitions, i n o rder t o c ontribute t o a m ore a ppropriate u se o f t he existing results, both from the point of view of classification according to their size or magnitude of resources and importance, as well as the characterization of the sediment accumulation environments. The results obtained show a low content of useful minerals disseminated in the sediments and the coexistence of chemically stable and unstable minerals on the seabed. These do not constitute mineral deposits as recorded in some investigations and, consequently, do not form mineral placers, due to: 1) low presence of terrigenous deposits and predominance of a carbonate environment, 2) low level of reworking and redeposition of the terrigenous sediments, 3) lack of appropriate input sources in the emerged territory and 4) 4) the gold that could have formed placers in the marine territory was deposited in the fluvial valleys. Their importance lies in the fact that they are good indicators to reconstruct the accumulation environment of terrigenous sediments in the marine environment.}, }
