检索结果-南通市图书馆

International Journal of Geosciences 2024年第2期15卷 180-203页

作者： fossou jean-luc hervé kouadio Alain Nicaise Kouamelan Topka Kakeu Lionel Boya Roger Nicaise Kanga Laboratory of Geology Mineral and Energy Resources (LGRME) Faculty of Earth Science and Mineral Resources Félix Houphou&#235t Boigny University Abidjan C&#244te d’Ivoire

The Gouméré region is located in the North-East of Côte d’Ivoire and is located in the South-West of the Bui furrow. In order to highlight the geology of the area studied, 14 samples were taken for studies using petrographic, geochemical and metallogenic methods. The study of macroscopic and microscopic petrography made it possible to highlight two major lithological units: 1) a volcano-plutonic unit, formed of gabbros, basalt, volcaniclastics and rhyodacite;2) a sedimentary unit (microconglomerate). From a geochemical point of view, the results obtained indicate that the plutonites are gabbro and gabbro diorite while the volcanics have compositions of basaltic andesites, rhyolite and dacites. The sediments have a litharenitic to sublitharenitic character. The metallogenic study made it possible to highlight hydrothermal alterations and metalliferous paragenesis on the formations studied. Hydrothermal alteration is characterized by the presence of carbonation, silicification, sericitization, sulfidation and to a lesser degree chloritization. Metalliferous paragenesis consists of pyrite, chalcopyrite, hematite and magnetite.

关键词： Petrography Geochemistry Metallogeny Gouméré Côte d’Ivoire

Geochemistry of Mafic Rocks from the Birimian Basement of Doropo (Northeast of Côte d’Ivoire): Petrogenetic and Geodynamic Implications

在线全文

维普期刊数据库

学校读者我要写书评

暂无评论

Open Journal of Geology 2022年第6期12卷 504-520页

作者： Wilfried Digbeu Alain Nicaise Kouamelan Asinne Tshibubudze Ziandjêdé hervé Siagne fossou jean-luc hervé kouadio Laboratoire de Géologie Ressources Minérales et Energétiques Université Félix Houphou&#235 t-Boigny Abidjan-Cocody C&#244 te d’Ivoire Council for Geosciences Pretoria South Africa

The northeastern region of Côte d’Ivoire is characterised by a granitic basement mainly composed of biotite granite rocks. According to mapping work in the Gbabédjou and Doropo areas, these Birimian granitoids are cut by gabbro dykes and amphibolite enclaves, which are the subject of this study. In order to better understand the role and the implication of mafic rocks in the Doropo basement emplacement, a multidisciplinary methodology integrating microscopic observations and geochemical analyses of major and trace elements was carried out on 4 samples considered representative of the outcrops studied. Green hornblende, clinopyroxene, and accessory sphene minerals are found in mafic mineral phases, according to petrographic research. Whole-rock analyses reveal that mafic samples with TiO2 contents 1.1 ratios giving them an orogenic granite nature (I-type). Their REE patterns are moderately fractionated (La/Sm)N = 2.66 - 6.13 and (La/Yb)N = 11.17 - 43.70) with a very negative Eu anomaly (Eu/Eu* = 0.75 - 0.97). The multi-element diagrams are characterized by negative Nb-Ta anomalies and geotectonic studies have identified them as volcanic arc formations. All these characteristics allowed us to distinguish the Doropo mafic rocks as formations originating from the juvenile continental crust, emplaced under the Archean tectonics model with significant crustal contamination in the source. Magma driven by mantle diapir has been injected at the base of the continental crust and the heat induces the partial melting of the overlying crust giving rise to mixed liquids. This magma now enriched in LILE was immediately drained to the upper crust to form the mafic rocks from the studied area.

关键词： Doropo Mafic Intrusive Birimian Crustal Contamination

Petrogenetic Characterization of the Geological Formations of the Localities of Goumere-Iguela in the South West of the Bui Belt (North-East of Cote d’Ivoire)

在线全文

维普期刊数据库

学校读者我要写书评

暂无评论

Open Journal of Geology 2022年第11期12卷 947-972页

作者： fossou jean-luc hervé kouadio Tokpa Kakeu Lionel-Dimitri Boya N’Guessan Nestor Houssou Roger Nicaise Kanga Alain Nicasie Kouamelan Laboratoire de Géologie Ressources Minérales et Energétiques Université Félix Houphou&#235 t-Boigny Abidjan-Cocody C&#244 te d’Ivoire

Located in the north-east of Côte d’Ivoire, the Gouméré-Iguéla sectors were the subject of a geological mapping. These geological formations are located southwest of the Bui trench. In order to improve the petrogenetic knowledge of the study area, a multidisciplinary methodology integrating microscopic observations and geochemical analyses of major and trace elements was carried out on 15 samples considered as representative of the studied outcrops. The macroscopic and microscopic petrographic study allowed to highlight three major lithological units: 1) a volcano-plutonic unit, formed by gabbros and amphibole-pyroxenite, basalt and rhyodacite;2) a volcano-sedimentary unit containing pyroclastites (of basaltic and andesitic composition);3) a sedimentary unit (meta-sedimentary). These rocks are affected by a general metamorphism of green schist facies and a hydrothermal alteration with pervasive and vein alteration marked by the presence of quartz, calcite, epidote, chlorite and sericite. From a geochemical point of view, the results obtained indicate that the plutonites are gabbros while the volcanites and volcanosedimentary rocks have compositions of basalts, basaltic andesites, rhyolites and dacites. They have mainly a tholeitic character related to subduction zones with crustal contamination. The metasediments are arenites emplaced in an active continental margin environment.

关键词： Petrography Geochemistry Petrogenetics Gouméré-Iguéla Côte d’Ivoire

The Geological Formations of Koun Fao (East of Côte d’Ivoire): Petrographic Characterization and Associated Deformations

在线全文

维普期刊数据库

学校读者我要写书评

暂无评论

Open Journal of Geology 2022年第10期12卷 787-810页

作者： Tokpa Kakeu Lionel-Dimitri Boya fossou jean-luc hervé kouadio Allou Gnanzou Martial Pohn Koffi Adingra Odrouro Ablan Anne Marie Kouame Marc Ephrem Allialy Laboratory of Geology Mineral and Energy Resources/Training and Research Unit in Earth Sciences and Mineral Resources Félix Houphou&euml t-Boigny University Abidjan C&ocirc te d’Ivoire

This study aims to contribute to improve knowledge on geological formations of Comoé basin. The petrographic study of the geological formations of Koun Fao has highlighted two major lithological families: magmatic rocks consisting of monzonites, monzogranites, diorites, biotite granodiorites, syenites, porphyritic micromonzonites and porphyritic dacite and metamorphic rocks from sedimentary origin (quartz schists, meta-greywackes, schists, andalusite chloritoschist and paragneiss). These formations are affected by amphibolite to greenschist facies metamorphism and hydrothermal alteration (pervasive and vein) marked by the presence of quartz, epidotes, chlorites and sericite. Minerals such as andalusite, muscovite and chlorite characterize a local low pressure contact metamorphism in the andalusite chloritoschist. Remote sensing data (Landsat 8 image) coupled with field data allowed the production of a geological map of the area. The study of the structures and microstructures highlighted two deformation mechanisms. These are flattening and simple shear (ductile and brittle). The study area is affected by four deformation phases: D1 marked by a N-S to NNE-SSW elongation, D2 marked by a NW-SE to NNW-SSE compression phase, D3 which is a NE-SW to NNE-SSW transpression phase and D4, responsible for late structures, marked by a NW-SE to NNW-SSE transpression phase.

关键词： Petro-Structural Geological Formations Comoé Basin Koun Fao Côte d’Ivoire

Structural Control of Auriferous Mineralization in the Birimian: Case of the Agbahou Deposit in the Region of Divo, Côte d’Ivoire

在线全文

维普期刊数据库

学校读者我要写书评

暂无评论

International Journal of Geosciences 2017年第2期8卷 189-204页

作者： N’Guessan Nestor Houssou Marc Ephrem Allialy fossou jean-luc hervé kouadio Allou Gnanzou Geology of Basement and Metallogeny Laboratory (GBML) Training and Research Unit of Earth Sciences and Mining Re-sources University of Felix HOUPHOUET-BOIGNY Abidjan-Cocody Cote d’Ivoire

Located in the southwestern of the Oume-Fettekro greenstone belt, the Agbahou gold deposit is controlled by structural factors. Geophysics, teledetection and core data suggest the presence of NE and NW faults. However, the NE-faults define two major shear zones (ATZ: Agbahou Tectonic Zone and WTZ: West Tectonic Zone) that control the Agbahou gold mineralization. These first order structures are subparallel to the regional tectonic grain mostly north-east oriented. They seem to respectively develop on the both arms (eastern and western) of an anticline moderately plunging ~25° towards northeast. Each shear-zone contains several second-order shear-zones or lenses of variable direction and of 50° - 80° dip. NW-faults however correspond to strike-slip faults and their development should be related to transcurrent tectonics. They acted as control channels on the distribution of gold mineralizations. The ductile-brittle character of shear-zones favored the ascent of hydrothermal fluids and the formation of multiple auriferous quartz veins: veins Type IIa and veins Type IIb relating respectively to the shear-veins and extensional veins. However, Agbahou also shows the existence of a disseminated sulphides-bearing mineralization within host-rocks. At Agbahou, the precipitation of gold probably occurred in a post to late ductile-brittle deformation period.

关键词： Gold-Bearing Mineralization Structural Control Birimian Agbahou Ivory Coast

Petro-Structural Study of Paragneiss in the SASCA Domain(GbowéSector at Grand-Bereby),Southwestern Cote d’Ivoire

在线全文

维普期刊数据库

学校读者我要写书评

暂无评论

Journal of Geoscience and Environment Protection 2020年第5期8卷 1-16页

作者： fossou jean-luc hervé kouadio Mamadou Sangare N’Guessan Nestor Houssou Marc Ephrem Allialy Sagbrou Chérubin Djro Laboratory of Geology Mineral and Energy Resources(LGRME)Faculty of Earth Science and Mineral ResourcesFélix Houphouet Boigny UniversityAbidjanCote d’Ivoire

The petrographic and structural study of Gbowé (Grand-Béréby) formations located in the SASCA domain (South-West of Côte d’Ivoire) revealed migmatitic paragneisses. For an in-depth understanding of the petrographic, structural and metamorphic characteristics, six (6) thin sections were made from these paragneisses. These gneisses are characterized by paleosomes and neosomes (leucosome and melanosome), consisting of quartz, garnet, plagioclase, biotite, cordierite, sillimanite, myrmekite and microcline. The mineralogical assemblage thus described indicates a retrograde metamorphism (transition from granulitic facies to amphibolitic facies). The structural and microstructural study identified two types of deformation (ductile and brittle). The ductile deformation is characterized by phases D1 (NE-SW flattening) and D2 (NW-SE flattening), materialized by foliations (N140˚, N050˚), folds (asymmetrical folds, similar folds, concentric folds, ptymatic folds) and boudins. Fracture schistosity and fold fracture schistosity are characteristic of the brittle deformation (phase D3). The microstructural study coupled with the metamorphic study shows that the deformations had an impact on the texture of the minerals (recrystallization and mineral reactions). It also allowed giving the paragenesis of phases D1 and D2. The D1 phase is characterized by garnet1, biotite1, quartz1, sillimanite1 and cordierite1 and the D2 phase is characterized by garnet1, quartz2, sillimanite2, biotite2, garnet2 and orthose2. These parageneses thus highlighted bear witness to a polydeformation and polymorphism that affects the study area.

关键词： Petrography Structural Migmatitic Paragneiss Retrograde Metamorphism Gbowé SASCA Domain C?te d’Ivoire

Mapping and Petro-Structural Study of the Geological Formations of the Alépé Region (South-East of Côte d’Ivoire)

在线全文

维普期刊数据库

学校读者我要写书评

暂无评论

International Journal of Geosciences 2023年第2期14卷 187-208页

作者： Allialy Marc Ephrem Diakite Sekou Houssou N’guessan Nestor kouadio fossou jean-luc Adingra Martial Pohn Koffi Laboratory of Geology Mineral and Energy Resources (LGRME) Faculty of Earth Science and Mineral Resources Félix Houphoue&#235t Boigny University Abidjan C &#244te d’Ivoire Laboratory of Geology Mineral and Energy Resources (LGRME) Faculty of Earth Science and Mineral Resources Félix Houphoue&#235t Boigny University Abidjan C&#244te d’Ivoire

This study focuses on the petrographic and structural characteristics of the geological formations of the Alépé region in the Comoé basin. The petrographic characterization allows us to retain that the study area abounds in a variety of lithologies: amphibole metagranite, metadiorite, amphibolite and metagrauwacke. The lineament map attests that the study area was affected by polyphase tectonics (ductile and brittle), all these deformations have NW-SE to NNW-SSE;NW-ESE to NW-SE;ENE-OSW and NE-SW directions. Coupled geochemical data show that the protoliths of the studied rocks evolve between granites and gabbros that are weakly to moderately be altered. They would originate from continental crust and mantle and would be emplaced in collision contex.

关键词： Lithostructural geochemistry Birimian Comoe Basin Alépé Côte d’Ivoire

Litho-Structural and Geochemistry Analysis of Granitoids from Mount Fouimba and Goma in Seguela Area (Central-Western Côte d’Ivoire)

在线全文

维普期刊数据库

学校读者我要写书评

暂无评论

Open Journal of Geology 2023年第1期13卷 72-89页

作者： Allialy Marc Ephrem Houssou N’guessan Nestor kouadio fossou jean luc Davy Bedel Siogbo Kouassi Brice Roland Konan Houphouet Felix UFR-STRM Felix Houphouet-Boigny University Abidjan-Cocody Abidjan C&#244 te d’Ivoire DGMG Abidjan C&#244 te d’Ivoire UFR-Biological Sciences Géosciences Department Peleforo Gon Coulibaly University of Korhogo Korhogo C&#244 te d’Ivoire

The petrogeochemical analysis of the granitoids of Mount Fouimba and Mount Goma in the Seguela region (central-western C?te d’Ivoire) is the subject of this study. This analysis combines remote sensing, geophysics, petrography and geochemistry, in order to determine the major characteristics of the granitoids in the study area, and above all to participate in the detailed mapping of all the Ivorian terrains. The granitoids encountered in this region are essentially two-mica granites, granodiorites and porphyry basalts. Chemical analysis indicates that these granitoids are of the ferrous and magnesian type with peraluminous to weakly metaluminous characteristics. They originate from the mantle and were emplaced in an active continental margin context.

关键词： Petrogeochemistry Granitoids Seguela Côte d’Ivoire

Fouimba and Goma Mounts Greenstone Belts Litho-Structural Analysis Related to Côte D’Ivoire Birimian Geodynamic Setting and Implying in West-Africa Craton Gold Deposits

在线全文

维普期刊数据库

学校读者我要写书评

暂无评论

Journal of Geoscience and Environment Protection 2023年第1期11卷 150-168页

作者： Marc Ephrem Allialy Brice Roland Kouassi N’guessan Nestor Houssou fossou jean luc kouadio Davy Bedel Siogbo Félix Oufouet Konan UFR-STRM Felix Houphouet-Boigny University Abidjan C&#244 te d’Ivoire UFR-Biological Sciences Géosciences Department Peleforo Gon Coulibaly University of Korhogo Korhogo C&#244 te d’Ivoire Ministry of Mines Petroleum and Energy Abidjan C&#244 te d’Ivoire

Mount Fouimba and Mount Goma (Seguela) greenstone belts petro-structural studies combine remote sensing, geophysics, petrography and structural analysis. In view of establishing mapping details of paleoproterozoic geological formations, geological setting rocks observed are essentially magmatic formations, such as two-mica granite, granodiorites, and porphyritic basalts;and a few metamorphics which are metatonalite, amphibolites and amphibo-lopyroxenites. Remote sensing, such as Landsat 8 OLI satellite imagery and geophysical data, has been combined to show regional NNE-SW shear zone. Tectonic structures and microstructures have enabled to identify two main deformation phases: D1 phase corresponding to compression, and D2 is a transpression phase. Mechanisms responsible for deformations are respectively flattening and transpression. Geological formations derived from mantle origin but contain crustal components, and their tectonic setting occurred during subduction.

关键词： Petro-Structural Mapping Greenstone Belt Birimian Séguéla Côte D’Ivoire

Petrochemical Studies of Fouimba and Goma Mounts, Central-West of Cote d’Ivoire: Implication on Petrogenesis Tectonic Setting

在线全文

维普期刊数据库

学校读者我要写书评

暂无评论

Open Journal of Geology 2023年第2期13卷 91-106页

作者： Allialy Marc Ephrem Siogbo Davy Bedel kouadio fossou jean luc Houssou N’guessan Nestor Kouassi Brice Rolland Konan Félix Oufouet Diakité Sekou Laboratoire GRME UFR STRM University Félix Houphou&#235t-Boigny de Cocody Abidjan Abidjan C&#244te d’Ivoire DGMG Ministère des Mines de C&#244te d’Ivoire Abidjan C&#244te d’Ivoire

Petrogeochemical analysis of mafic rocks of Fouimba and Goma Mount in the Séguéla region (central-western Côte d’Ivoire) is the subject of this study. This analysis combines remote sensing, geophysics, petrography and geochemistry, in order to determine the major characteristics of the mafic formations in the said area, and above all to participate in the detailed mapping of all the Ivorian terrains. The mafic formations encountered in this region are essentially metatonalites to metadiorites, amphibolites, amphibole bearing pyroxenites and porphyry basalts. Chemical analysis indicates that these mafic formations are tonalitic to monzonitic. They are thought to have derived from mantle depleted magmas.

关键词： Petrography Geochemistry Mount Fouimba and Goma Seguela Côte d’Ivoire