Cu-ID: https://cu-id.com/2277/v16n1e86 Redirecciones: 94 URL: https://rgi.edicionescervantes.com/index.php/rgi/article/view/86 OAI: https://rgi.edicionescervantes.com/index.php/rgi/oai?verb=GetRecord&metadataPrefix=oai_dc&identifier=oai:ojs.pkp.sfu.ca:article/86 BibTeX: @article{DEFINITION_OF_MAGMATIC-METALLOGENIC_BELTS_IN_THE_CRETACEOUS-PALEOGENE_ISLAND_ARC_IN_EASTERN_CENTRAL_CUBA, title = {DEFINITION OF MAGMATIC-METALLOGENIC BELTS IN THE CRETACEOUS-PALEOGENE ISLAND ARC IN EASTERN CENTRAL CUBA}, author = {Lugo-Primelles, René and Pimentel-Olivera , Higinio and Pérez-Peña , Eduardo and Pardo-Echarte , Manuel}, journal = {Geoinformativa}, volume = {16}, number = {1}, pages = {53-67}, year = {2023-08-14}, publisher = { Instituto de Geología y Paleontología/Servicio Geológico de Cuba}, language = {spa}, url = {https://cu-id.com/2277/v16n1e86}, cu_id = {https://cu-id.com/2277/v16n1e86}, abstract = {The aim of the work was the disclosure of 6 metallogenic belts revealed from 1996 to 1998, through the compilation, organisation and reinterpretation of all the geophysical, geological and geochemical information of Ciego de Avila-Camagüey-Las Tunas, to update the stratigraphic knowledge and the generalisation of the alteration and mineralisation processes by types of existing and expected deposits. The descriptive method of investigation was applied to the information of the different physical fields. Aeromagnetic field transformations (∆T) were performed for the whole region (pole reduction, upward analytical continuations at the heights of H=1 km and H=7 km, residual fields and first vertical derivative), the production of a shadow map with declination (0°) and inclination of 45° at 1:250 000 scale, maps of the total magnetic field and pole reduction and residual field for the sheets at 1:100 000 scale, the production of Bouger anomaly maps for an intermediate layer density of 2. 67 g/cm3, maps of upward analytical continuations for H=5 km, H=7 km, H=250 m and H=500 m and other transformations such as derivatives and residual fields. For the first time in Cuba, geophysical and geological conditions were established for the definition of magmatic-metallogenic axes and similar alignments in the Cretaceous-Paleogene volcano-plutonic arc terrain in East Central Cuba. The belts were distinguished: Cubano Axial, La Yaya-Guáimaro[1]Golden Hill, Jobabo-Vertientes, Arroyo Blanco and del Sur in the Camagüey territory, as well as the Ciego de Ávila bordering Camagüey, Vertientes-El Chorro.}, }
Cu-ID: https://cu-id.com/2277/v16n1e85 Redirecciones: 77 URL: https://rgi.edicionescervantes.com/index.php/rgi/article/view/85 OAI: https://rgi.edicionescervantes.com/index.php/rgi/oai?verb=GetRecord&metadataPrefix=oai_dc&identifier=oai:ojs.pkp.sfu.ca:article/85 BibTeX: @article{GUIDE_TO_LOCALITIES_OF_GEOLOGICAL_INTEREST_(GEOSITES)_OF_THE_CITY_OF_HAVANA, title = {GUIDE TO LOCALITIES OF GEOLOGICAL INTEREST (GEOSITES) OF THE CITY OF HAVANA}, author = {Gutiérrez Domech , Manuel Roberto and Pantaleón Vento, Guillermo and Rosa Romeu , Adriana}, journal = {Geoinformativa}, volume = {16}, number = {1}, pages = {68-79}, year = {2023-08-14}, publisher = { Instituto de Geología y Paleontología/Servicio Geológico de Cuba}, language = {spa}, url = {https://cu-id.com/2277/v16n1e85}, cu_id = {https://cu-id.com/2277/v16n1e85}, abstract = {Although a few geological sites in the country have been declared local monuments and due to their landscape or their historical importance and therefore form part of the national heritage, the vast majority are at the mercy of the needs or the will of individuals and/or communities that without adequate instruction on the values of each site can harm them, partially destroy them or make them disappear, as has already happened. In the city of Havana, despite the degree of urbanization that exists, 12 geological sites of interest have been recognized, not registered in the MINEM resolution that was published in the Official Gazette. Here, 13 geosites are recognized and recommended for the practice of geotourism, without attempting to take into account all that may exist. Four are Quaternary geosites, related to the glacieustatic and neotectonic processes of the Pleistocene that generated the formation of terrace fronts, at the corner of Avenidas 23 and Paseo, on Avenida de los Presidentes (G) and Calle 21; at the corners of 11th and 18th and 26th and 13th streets, among others, and also the stratotypes of the Vedado and Guanabo formations. The stratotypes of the Príncipe Formation and the Informal Unit, Urría, both from the Paleogene, are also found in the city; Cojímar, from the Middle Miocene, and La Cabaña and Guanabo.}, }
Cu-ID: https://cu-id.com/2277/v16n1e84 Redirecciones: 59 URL: https://rgi.edicionescervantes.com/index.php/rgi/article/view/84 OAI: https://rgi.edicionescervantes.com/index.php/rgi/oai?verb=GetRecord&metadataPrefix=oai_dc&identifier=oai:ojs.pkp.sfu.ca:article/84 BibTeX: @article{NEW_IGP/SGC_PROJECTS_FOR_2023, title = {NEW IGP/SGC PROJECTS FOR 2023}, author = {Karell Arrechea, Dinorah N.}, journal = {Geoinformativa}, volume = {16}, number = {1}, pages = {80-86}, year = {2023-08-14}, publisher = { Instituto de Geología y Paleontología/Servicio Geológico de Cuba}, language = {spa}, url = {https://cu-id.com/2277/v16n1e84}, cu_id = {https://cu-id.com/2277/v16n1e84}, abstract = {}, }
Cu-ID: https://cu-id.com/2277/v16n2e98 Redirecciones: 67 URL: https://rgi.edicionescervantes.com/index.php/rgi/article/view/98 OAI: https://rgi.edicionescervantes.com/index.php/rgi/oai?verb=GetRecord&metadataPrefix=oai_dc&identifier=oai:ojs.pkp.sfu.ca:article/98 BibTeX: @article{PALEOGEOGRAPHIC_DOMAIN_OF_THE_NEOAUTOCHTONOUS_IN_THE_REPUBLIC_OF_CUBA, title = {PALEOGEOGRAPHIC DOMAIN OF THE NEOAUTOCHTONOUS IN THE REPUBLIC OF CUBA}, author = {Linares Cala, Evelio and García Delgado, Dora Elisa}, journal = {Geoinformativa}, volume = {16}, number = {2}, pages = {1-14}, year = {2023-12-04}, publisher = { Instituto de Geología y Paleontología/Servicio Geológico de Cuba}, language = {spa}, url = {https://cu-id.com/2277/v16n2e98}, cu_id = {https://cu-id.com/2277/v16n2e98}, abstract = {The objetive of this paper is argue the rejuvenation of the Neo-autochtonous Paleogeographic Domain (DP) from the west to the east of the Cuban archipelago. Using the Terranoestratigraphy methodology. 77 Neo-autochtonous lithostratigraphy formations are characterized: 27 from the Western Neo-autochtonous; 31 from the Central Neo-autochtonous; 19 from the Eastern Neo-autochtonous and the unnamed deposits distributed in Cuba. The Neo-autochtonous Domain corresponds to a stage of greater tectonic stability after the climax of the main Cuban Orogenic. The Neo-autochtonous litostratigraphic units usually occupy one or more structural levels. Several formations constitute a continuation of the Upper Oligocen deposits while others reach the Pleistocene. The final consolidation of the folded substratum has been previosly proposed in the Upper Eocene; however, recently it has been formulated that the peak of the movements that caused folding and overthrust ended in unequal periods according to the regions of the national territory. The Neo- autochtonous DP moves in time from the West to the East, rejuvenating itself. The oldest formation of the Western Neo-autochtonous Petrotectonic Complex (CPT) is the Toledo Formation of the Universidad Group and is dated as Late Ypresian, while the oldest of the Eastern CPT is the Lower Oligocen Yateras Formation. The Neo-autochtonous is an important source for construction materials and aquifer reservoirs. There are quarries that provide materials for the cement factory; the clayey materials can be used for produce bricks and ceramics. Excelents agriculture soil are derived from some of these Neoautoctonous units.}, }
Cu-ID: https://cu-id.com/2277/v16n2e97 Redirecciones: 71 URL: https://rgi.edicionescervantes.com/index.php/rgi/article/view/97 OAI: https://rgi.edicionescervantes.com/index.php/rgi/oai?verb=GetRecord&metadataPrefix=oai_dc&identifier=oai:ojs.pkp.sfu.ca:article/97 BibTeX: @article{DEVELOPMENT_AND_EVOLUTION_OF_GEOLOGIC_RESEARCHS_FOR_GOLD_IN_CUBA,_PERSPECTIVES, title = {DEVELOPMENT AND EVOLUTION OF GEOLOGIC RESEARCHS FOR GOLD IN CUBA, PERSPECTIVES}, author = {López Kramer, Jesús Manuel}, journal = {Geoinformativa}, volume = {16}, number = {2}, pages = {15-26}, year = {2023-12-11}, publisher = { Instituto de Geología y Paleontología/Servicio Geológico de Cuba}, language = {spa}, url = {https://cu-id.com/2277/v16n2e97}, cu_id = {https://cu-id.com/2277/v16n2e97}, abstract = {The background information on geological investigations for gold in each Economic-Social Formation provides an overview of its development and evolution over time. The analysis of the information is carried out as a first approach to the most relevant aspects taking into account the international circumstances in the context of its development. This work is based on archival materials related to geological and mining studies carried out by different authors and entities, mainly those with a higher level of research, which are shown as standard deposits. With special interest are highlighted the achievements and difficulties obtained by the so-c alled basic stages suc h as: The mining preserves, The Economic Mutual Aid Council, Foreign investment, The Cuba-Venezuela Collaboration Agreement, The gold development program- National Program for the Development of Geological Activity, the latter of great importance since it assumes, with the state budget, gold prospectingas a challenge for the economic development of the country and for the role achieved in this endeavor by the National Geological Service, the universities, research institutes and the territorial companies of the Geominsal Group. In the different Economic-Social Formations and their basic stages, geologic al research was developed, differentiated in geological knowledge, these currently face challenges common to the whole world as the need for foreign investment and the prospects for discovering new sources of gold.}, }
Cu-ID: https://cu-id.com/2277/v16n2e96 Redirecciones: 73 URL: https://rgi.edicionescervantes.com/index.php/rgi/article/view/96 OAI: https://rgi.edicionescervantes.com/index.php/rgi/oai?verb=GetRecord&metadataPrefix=oai_dc&identifier=oai:ojs.pkp.sfu.ca:article/96 BibTeX: @article{QUENCH_TEXTURES_IN_BASALTS_OF_THE_MINERAL_FIELD_HIERRO-MANTUA._PINAR_DEL_RÍO_PROVINCE, title = {QUENCH TEXTURES IN BASALTS OF THE MINERAL FIELD HIERRO-MANTUA. PINAR DEL RÍO PROVINCE}, author = {Cobas Torres, René Yasmany and Torres La Rosa, Mercedes}, journal = {Geoinformativa}, volume = {16}, number = {2}, pages = {27-33}, year = {2023-12-22}, publisher = { Instituto de Geología y Paleontología/Servicio Geológico de Cuba}, language = {spa}, url = {https://cu-id.com/2277/v16n2e96}, cu_id = {https://cu-id.com/2277/v16n2e96}, abstract = {The Hierro-Mantua mineral field (Pinar del Río, Cuba) is a deposit type siliciclastic- mafic VMS of lenticular morphology in concordance with host rocks belonging to the Esperanza Formation of J3ox K1ne age, constituted by a sequence of terrigenous sediments and carbonates (schistose limestones, calcareous sandstones, black shales, argillites and siltstones) and concordant bodies of diabases and gabbro-diabases representative of submarine tholeiitic rift magmatism. Basic volcanic rocks were analyzed by petrographic analysis and quench textures in pyroxenes and plagioclases were identified for the first time. The plagioclases show swallow-tail, feathery and rosette morphologies while the pyroxenes have a feathery and herringbone habit. Much of these textures are identical to those reported in submarine basalts, lunar basalts, rocks with spinifex texture and experimentally produced textures. According to the recognized types of quench textures, it is inferred that crystallization occurred in submarine conditions with high supercooling rates, in the order of 32-66ºC/h in a range of temperature rates (ΔT) between 150-300ºC.}, }
Cu-ID: https://cu-id.com/2277/v16n2e95 Redirecciones: 67 URL: https://rgi.edicionescervantes.com/index.php/rgi/article/view/95 OAI: https://rgi.edicionescervantes.com/index.php/rgi/oai?verb=GetRecord&metadataPrefix=oai_dc&identifier=oai:ojs.pkp.sfu.ca:article/95 BibTeX: @article{TECTONIC-STRUCTURAL_INTERPRETATION_OF_GEOPHYSICAL_DATA_(1998)_OF_CENTRAL_EASTERN_CUBA_(PART_II)._SYNTHESIS_OF_FIRST_GEOLOGICAL_SURVEYS, title = {TECTONIC-STRUCTURAL INTERPRETATION OF GEOPHYSICAL DATA (1998) OF CENTRAL EASTERN CUBA (PART II). SYNTHESIS OF FIRST GEOLOGICAL SURVEYS}, author = {Lugo Primelles, René and Pimentel Olivera, Higinio and Alonso Díaz, Jorge and Rubante Martin, Dania}, journal = {Geoinformativa}, volume = {16}, number = {2}, pages = {34-50}, year = {2023-12-21}, publisher = { Instituto de Geología y Paleontología/Servicio Geológico de Cuba}, language = {spa}, url = {https://cu-id.com/2277/v16n2e95}, cu_id = {https://cu-id.com/2277/v16n2e95}, abstract = {The work is a synthesis of the results of the first geological reconnaissance projects for gold and other metals in several of the magmatic-metallogenic belts, interpreted by a team of geophysicists and geologists of Empresa Geominera Camagüey, in 1998, whose main objective was to demonstrate its existence in the selected territories and its scope when defining the mineral potential in a preliminary way, specifying what was executed in the Cretaceous-Paleogene volcano-plutonic arc in Camagüey province. It is a continuation of the first a rticle p ublished i n G eoinformativa a nd does not include field verifications (the field work was already carried out), using the descriptive method of scientific research, based on the compilation, revision, analysis and generalization of the necessary geophysical and geological information, using analogy criteria when possible. Due to the economic situation of the special period in the country, these projects were cancelled in full development, but important results that confirm t he r eal e xistence o f t hese " corridors" o r m etallogenic b elts were always obtained. The results of the advanced work for gold and other metals in the sectors, from west to east, are presented: Cuatro Compañeros-Guaicanamar, Jimirú-La Luna, Cuatro Caminos de Najasa-La Esperanza, Martí-La Yaya and Colombia- Barrueto. The main objective of these investigations has been to create a bank of prospecting-exploration projects that will increase the number of mineral deposits, mostly gold, potentially exploitable from the economic point of view. These results are still incomplete to define the real potential of the investigated areas, but they are proof of the correct interpretation of the prospecting orientation according to a deep geophysical-metallogenic interpretation.}, }
Cu-ID: https://cu-id.com/2277/v16n2e93 Redirecciones: 59 URL: https://rgi.edicionescervantes.com/index.php/rgi/article/view/93 OAI: https://rgi.edicionescervantes.com/index.php/rgi/oai?verb=GetRecord&metadataPrefix=oai_dc&identifier=oai:ojs.pkp.sfu.ca:article/93 BibTeX: @article{LA_MINERÍA_A_CIELO_ABIERTO_ABANDONADA_EN_CUBA:_SU_VÍNCULO_E_INTEGRACIÓN_CON_LA_TAREA_VIDA, title = {LA MINERÍA A CIELO ABIERTO ABANDONADA EN CUBA: SU VÍNCULO E INTEGRACIÓN CON LA TAREA VIDA}, author = {Ponce Seoane, Nyls Gustavo and Díaz Comesañas, Jorge L. and Rivada Suárez, Ramón}, journal = {Geoinformativa}, volume = {16}, number = {2}, pages = {51-56}, year = {2023-12-21}, publisher = { Instituto de Geología y Paleontología/Servicio Geológico de Cuba}, language = {spa}, url = {https://cu-id.com/2277/v16n2e93}, cu_id = {https://cu-id.com/2277/v16n2e93}, abstract = {In the year 2100, 5-6% of the surface of Cuba will be submerged by the elevation of the sea due to climate change, affecting some 6,000 km2 of coastline. This will force the rational use of the emerged territory. To solve the problems of this situation, the Cuban Government created the State Plan to Confront Climate Change - Life Task, which includes the territorial dimension to solve it with the implementation of actions for changes in land use, developing conceptions construction of infrastructures, the efficient adaptation of agricultural activity for food security, increase in water productivity, tourism development, reforestation and others that should lead to the integration of Geology and Mining with the Task of Life. Open pit mining is one of the activities that most impacts the environment. After having analyzed more than 300 abandoned quarries in the provinces of Havana, Artemisa and Mayabeque, rehabilitation solutions and new uses were proposed that revert to economic and environmental benefits for the country, such as: location of agricultural, industrial and urban; recreation areas; regulation of micro mining activity; recycling of rubble for building materials; new technologies for the deposit and treatment of urban solid waste; physical-chemical treatment of water that emerges in the quarries to use them; reforestation, revegetation; all based on sustainable local development, which is in correspondence with the Life Task for the achievement of its purposes.}, }
Cu-ID: https://cu-id.com/2277/v16n2e92 Redirecciones: 47 URL: https://rgi.edicionescervantes.com/index.php/rgi/article/view/92 OAI: https://rgi.edicionescervantes.com/index.php/rgi/oai?verb=GetRecord&metadataPrefix=oai_dc&identifier=oai:ojs.pkp.sfu.ca:article/92 BibTeX: @article{COMMENTS_ON_"UPDATE_OF_THE_INSTITUTIONAL_REGISTRY_OF_FALLEN_METEORITES_IN_CUBA"., title = {COMMENTS ON "UPDATE OF THE INSTITUTIONAL REGISTRY OF FALLEN METEORITES IN CUBA".}, author = {Iturralde Vinent, Manuel A.}, journal = {Geoinformativa}, volume = {16}, number = {2}, pages = {57-61}, year = {2023-12-21}, publisher = { Instituto de Geología y Paleontología/Servicio Geológico de Cuba}, language = {spa}, url = {https://cu-id.com/2277/v16n2e92}, cu_id = {https://cu-id.com/2277/v16n2e92}, abstract = {A critical evaluation of the institutional catalog of fallen meteorites in Cuba of the Institute of Geophysics and Astronomy is presented, offering solutions to achieve the necessary quality.}, }
Cu-ID: https://cu-id.com/2277/v15n1e129 Redirecciones: 63 URL: https://rgi.edicionescervantes.com/index.php/rgi/article/view/129 OAI: https://rgi.edicionescervantes.com/index.php/rgi/oai?verb=GetRecord&metadataPrefix=oai_dc&identifier=oai:ojs.pkp.sfu.ca:article/129 BibTeX: @article{THE_CLASSIFICATION_OF_THE_GOSSANS._IMPLICATIONS_FOR_PROSPECTING, title = {THE CLASSIFICATION OF THE GOSSANS. IMPLICATIONS FOR PROSPECTING}, author = {López Kramer, Jesús Manuel and Pérez Aragón , Ramón Omar and Gallardo Eupierre, Emiliano and Pimentel Olivera , Higinio}, journal = {Geoinformativa}, volume = {15}, number = {1}, pages = {18-31}, year = {2023-09-19}, publisher = { Instituto de Geología y Paleontología/Servicio Geológico de Cuba}, language = {spa}, url = {https://cu-id.com/2277/v15n1e129}, cu_id = {https://cu-id.com/2277/v15n1e129}, abstract = {The gossans constitute an industrial genetic type of deposits. In Cuba, 161 are reported, of which 3 are exploited: Lote Grande, the Golden Hill mineral field, a mineral zone enriched in gold from the El Cobre deposit, called Barita. All of them with limited resources. The government budget annually allocates approximately 33 % of funding for geological research work for gold. Research is needed to achieve greater effectiveness in the selection of new deposits and obtain a greater volume of ores. The presence of small primary deposits of different genesis, the non-existence of a classification based on the use of Cuban patterns for gossans and the little experience in their exploration, generate a significant margin of error in terms of selecting the targets to be prospected. Starting from the degree of study of the primary ores, the existence of 141 virgin gossans (of which their potentialities to host Au and Ag ores are unknown) and the main regularities formulated from the standard gossans by geoenvironments, a classification is proposed, where empirical evidence, supported by accumulated practice, are key factors taken into account. The main expected impact, is the contribution of a general tool that helps a more efficient selection of the objectives for the geological exploration of this type of gold deposits by provinces, giving priority to those objectives with the greatest prospects for the development of the mining activity.}, }
