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Diversity of Gold Deposits, Geodynamics and Conditions of Formation: A Perspective View

Open Journal of Geology 2017年第11期7卷 1690-1709页

作者： franck wilfried dongmo nguimatsia Anthony Temidayo Bolarinwa Rose Fouateu Yongue Jean de Dieu Ndikumana Jerry Olugbenga Olajide-Kayode Olugbenga G. Olisa Maryam O. Abdu-Salam Marc Anselme Kamga Ernest Serge Djou Department of Geology Pan African University Life and Earth Science Institute-University of Ibadan Ibadan Nigeria Department of Earth Sciences University of Yaounde 1 Yaounde Cameroon

Gold occurs in a wide range of deposit types and settings. In the last decade, significant progress has been made in the definition, classification, characterization, thereby aiding understanding of the main gold deposit types. The present work aims to provide an update on the current state of knowledge on the different types of gold deposits models, geodynamics, their mode of formation and the condition suitable for their formation Several subsets of gold deposits are distinguished from one another on the bases of and their main geological models and their mode of formation described. Gold deposits of magmatic-hydrothermal origin are classified into Porphyry, Epithermal, Skarn, Iron Oxide-Copper-Gold and Intrusion related deposits;those of hydrothermal origin are Orogenic, Volcanogenic Massive Sulphide deposits, and Carlin-type;while those of Sedimentary Origin are placers. In terms of the major Period of gold deposit formation, the Mesoarchean was the largest gold period. Other gold peaks followed, particularly in the Neoarchean, Paleoproterozoic and Paleozoic while numerous and diverse gold deposit types were formed during the Cenozoic *** varieties of geodynamic contexts in which each of the gold deposits are formed being explained while the conditions favourable for its formation are also being summarized. With the recent rise in the price of gold, mining companies and research centers continue to provide lighting of the key geology features of then ore-forming environments and the key geologic manifestations of the different deposit types.

关键词： Gold Tectonic Porphyry Epithermal Skarns Placer

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Evaluation of the Geological and Metallogenic Potential of Koffissiokaha Permit, Area of Katiola, Côte d’Ivoire

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Open Journal of Geology 2022年第10期12卷 767-786页

作者： Houssou N’guessan Nestor Adingra Martial Pohn Koffi Allialy Marc Ephrem Kouassi Kra wilfried Kouakou Loba Gbriga franck Cyrille UFR-STRM Université Félix Houphou&euml t-Boigny Abidjan C&ocirc te d’Ivoire Blue-Hill Exploration Sarl Abidjan C&ocirc te d’Ivoire

The semi-industrial permit of Koffissiokaha, south-eastern area of Katiola, is located in the northern part of Fêtêkro Birimian Greenstone Belt (Côte d’Ivoire). This permit, applicated by the company Blue-Hill Exploration Sarl (BHEX), is in the southern continuity area of Lafigué permit (Endeavour Mining). Blue-Hill will have to work to highlight potential gold mineralization, quantify it (resource calculation) and initiate administrative procedures to obtain a Semi-Industrial Exploitation Authorization (AESI). Our recent works, including field mapping coupled with petrographic and microstructural studies, are therefore intended to contribute to the knowledge of the geology and to the evaluation of the gold potential of this permit. They suggest that Koffissiokaha permit includes four major lithologic units: 1) a sedimentary unit formed by metaarenites and metasiltites, 2) a unit of mafic pyroclastites (cinerites, tuffs and volcanic breccias) 3) a plutonic unit of metagabbro and finally, 4) a lode-type unit made up of metarhyodacites. The metamorphism that affected the volcano-sedimentary rocks is of low grade to greenschist facies. On the structural level, deformations with variable gradients are noted. The major planary structure, the schistosity, is oriented N20 - 40 with weak (°), moderate (50°- 60°) and steep dips (>70°) or subvertical. The faults generally correspond to narrow dextral or senestral shear-zones (75°) towards south-east or subvertical. They are most often intersected by late strike-slip faults-oriented NW-SE, NNW-SSE and N-S. Quartz veins are associated with faults or deformation zones. They are generally oriented N20 to N40, with weak (°), moderate (55°- 65°) and steep dips (>75°). Orientations of joints and fractures are mostly subparallel to the plans of schistosity, shears and most of quartz veins. However, ENE, WNW and N-S fractures are also distinguished. The sulphide paragenesis consists o

关键词： Petro-Structural Metallogeny Gold Mineralization Birimian Koffissiokaha Côte d’Ivoire

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