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The Late Neoproterozoïc Continental Tholeiitic Basalts of the Toubkal Inlier (Western High-Atlas, Morocco): A Post-Pan-African Rifting Witness in the Northern Margin of the West African Craton

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Open Journal of Ecology 2016年第8期6卷 509-516页

作者： Ghalem Zahour Hassan El Hadi Abdelfatah Tahiri youssef zerhouni Saida Alikouss Rachid Zahour Aicha Reddad Laboratory of Paleobelts Geodynamic Sciences Faculty of Ben M’sik Hassan II University of Casablanca Casablanca Morocco Geology and Remote Sensing Laboratory URAC46 Mohammed V University of Rabat Scientific Institute Rabat Morocco Laboratory of Géosciences Science and Techniques Faculty Guéliz Cadi Ayyad University Marrakech Morocco

The late Neoproterozoïc Toubkal inlier (Ancient Massif of the High-Atlas, Morocco) contains two igneous basaltic series (Tircht and Sidi Chamharouch). Investigated rocks display characteristics of within-plate continental tholeiitic and are similar to rocks originated in orogenic contexts. The geochemical results allow the assumption that subduction active processes are indirectly responsible for the genesis of theses rocks. The orogenic signature is linked probably to a Pan-African magmatic source previously metasomatized in the northern margin of the West African Craton.

关键词： Toubkal Inlier Late Neoproterozoïc Continental Tholeiites Rift West African Craton

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Exploration and Mapping of Metalliferous Black Shales in the Saghro Temporary Subsidence Zones (Anti-Atlas, Morocco)

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Open Journal of Geology 2023年第7期13卷 740-762页

作者： Ali Bouayachi Saida Alikouss Zouhir Baroudi youssef zerhouni Lahcen Rakhis Mohammed Zouhair Assia Idrissi Mourad Essalhi Barzouk Abdelhafed Department of Geology Faculty of Sciences Ben M’Sik University Hassan II Casablanca Morocco MANAGEM Group 191 bd Med Zerktouni Twin Center Tour A. 20100 Casablanca Morocco Department of Geology Faculty of Sciences University Mohamed V Rabat Morocco Faculty of Sciences and Techniques University Molay Ismail Errachidia Morocco Faculty of Sciences Semlalia Caddi Ayyad University Marrakech Morocco

The Saghro massif constitutes a vast metallogenic province with numerous deposits and shows of base metals (lead, zinc, copper) and precious metals (gold and silver), besides various useful substances (talc, pyrophyllite, barite, fluorite). Silver/lead occurrences are concentrated along the Cryogenian Imiter series and moderately at Boumalne and Sidi Flah. Copper occupies the plutonic intrusions and intrusive rocks of the East-Central Saghro while barite deposits are widespread throughout the Cambrian cover of the East Saghro in contact with the Ediacaran basement. To justify this distribution, the new contributions of the cartography and the organic geochemistry of the black shales of Jbel Saghro have clearly shown the particularity of the Imiter black shales in terms of the richness in organic matter (TOC = 0.18%), the blackish color and the friability. The Boumalne and Sidi Flah groups present some similarities with the Imiter group, such as the sub-equatorial structuring, the friable pelites and the richness in organic matter (Boumalne TOC = 0.11% and SidiFlah TOC = 0.16%), which is a quite good show that requires to reinforce the exploration works. For Western Saghro in the Iknioun and Qalaa’t M’Gouna groups, the variations in the thickness of the volcanic cover show an irregular paleotopography with hard, greenish, organic-poor pelitic sediments (TOC = 0.01 to 0.04%). We can conclude that the formation of Imiter-type silver concentrations requires the combination of the sedimentological, the volcanic and structural factors. For Imiter-type silver these factors are: a fine pelitic and argillic casing deposited in a confined environment, a basic volcanism source of metals and other intermediate to acid generated by the hydrothermalism and heat, a convenable paleotopography and a network of fracturations to trap the mineralizations.

关键词： Saghro Metallic Shales Silver TOC Exploration Cryogenic Polymetallic Imiter

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Mineralogy and Geochemistry of EtekéEburnean Gold Deposit (Gabon)

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Open Journal of Geology 2022年第3期12卷 294-311页

作者： Makarim Dalil Nazaire Nzaou Mabika Amina Wafik Zohir Baroudi Abdelmalek Ouadjou Mohamed Gharrabi Amine Bouwafoud Nouamane El Aouad youssef zerhouni Saida Alikouss Laboratoire géosciences et applications Faculté des sciences Ben M’sik Casablanca Morocco Laboratoire Dynamique de la Lithosphère et Genèse des Ressources Faculté des Sciences Semlalia Marrakech Morocco Managem Group Twin Center Casablanca Morocco

The Gabon geology offered favorable and natural environments for the formation of various types of mineralization. The Etéké gold district, aim of this study, is located in the Ngounié province (southern Gabon) on the western edge of the Chaillu massif. Geologically, the gold mineralization is associated with the Eburnean orogeny and hosted in the Archean greenstone belts. Also, this deposit is covered by a significant vegetation cover and a very extensive lateritic weathering profile, which hinders the most accurate study. Through this paper, we aim to propose a genesis pattern of this mineralization via a multidisciplinary approach. To do this, a petrographic, metallogenic, and geochemical characterization has been established in the different sectors of the Etéké deposit. The studied deposits display varied facies which are encased in granitoid. They are essentially formed of abundant granitoid, and amphibolite compared to the volcano-sedimentary formations. These rocks display magmatic textures, affected by metamorphism, and not sufficiently preserved. Based on our multidisciplinary approach, the studied samples collected from the core’s boreholes allowed us to decipher a volcanogenic and metamorphosed origin of the gold genesis.

关键词： Eburnean Orogeny Gabon Gold Greenstone Granitoids Amphibolite

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Exploration and Mapping of Metalliferous Black Shales in the Saghro Temporary Subsidence Zones (Anti-Atlas, Morocco)

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Open Journal of Geology（地质学期刊） 2023年第7期

作者： Ali Bouayachi Saida Alikouss Zouhir Baroudi youssef zerhouni Lahcen Rakhis Mohammed Zouhair Assia Idrissi Mourad Essalhi Barzouk Abdelhafed

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