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Journal articles on the topic 'Eburnean'

Author: Grafiati

Published: 4 June 2021

Last updated: 12 February 2022

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1

Rezaeifar, Maryam, and Mahdi Rezaeifar. "Effect of Amygdalus eburnea on third degree burns in rats and comparison with silver sulfadiazine ointment." Asian Journal of Pharmaceutical and Clinical Research 10, no. 5 (2017): 376. http://dx.doi.org/10.22159/ajpcr.2017.v10i5.16877.

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Amygdalus eburnea is a perennial herb that has been valued for its important biological perspectives and it has been used to treat the burn. In this study, the extract from the Iranian medicinal herb is investigated on its wound healing activity in comparison with silver sulfadiazine ointment as the standard treatment for burn wound in rats. Our results demonstrated that, Amygdalus eburnean can be an effective treatment for third degree burns. Advanced clinical and pharmaceutical studies are recommended in order to the production of novel natural drugs for burn wound treatment.

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2

Chardon, Dominique, Ousmane Bamba, and Kalidou Traoré. "Eburnean deformation pattern of Burkina Faso and the tectonic significance of shear zones in the West African craton." BSGF - Earth Sciences Bulletin 191 (2020): 2. http://dx.doi.org/10.1051/bsgf/2020001.

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Shear zones of the Paleoproterozoic Eburnean accretionary Orogen (West African craton) are investigated by means of large-scale structural mapping. Regional scale (10-100 km) mapping was based on the aeromagnetic survey of Burkina Faso and craton-scale (1000 km) mapping on a compilation of fabric data. At both scales, shear zones are arranged as an anastomosed transpressional network that accommodated distributed shortening and lateral flow of the orogenic lithosphere between the converging Kénéma-Man and Congo Archean provinces. Structural interference patterns at both scales were due to thre

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3

Thiéblemont, Denis, Jean Christian Goujou, Emmanuel Egal, et al. "Archean evolution of the Leo Rise and its Eburnean reworking." Journal of African Earth Sciences 39, no. 3-5 (2004): 97–104. http://dx.doi.org/10.1016/j.jafrearsci.2004.07.059.

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4

Schofield, D. I., M. S. A. Horstwood, P. E. J. Pitfield, Q. G. Crowley, A. F. Wilkinson, and H. Ch O. Sidaty. "Timing and kinematics of Eburnean tectonics in the central Reguibat Shield, Mauritania." Journal of the Geological Society 163, no. 3 (2006): 549–60. http://dx.doi.org/10.1144/0016-764905-097.

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5

Schofield, D. I., and M. R. Gillespie. "A tectonic interpretation of “Eburnean terrane” outliers in the Reguibat Shield, Mauritania." Journal of African Earth Sciences 49, no. 4-5 (2007): 179–86. http://dx.doi.org/10.1016/j.jafrearsci.2007.08.006.

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6

Baratoux, Lenka, Václav Metelka, Séta Naba, Mark W. Jessell, Michel Grégoire, and Jérôme Ganne. "Juvenile Paleoproterozoic crust evolution during the Eburnean orogeny (∼2.2–2.0Ga), western Burkina Faso." Precambrian Research 191, no. 1-2 (2011): 18–45. http://dx.doi.org/10.1016/j.precamres.2011.08.010.

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7

Ouzegane, Khadidja, Abderrahmane Bendaoud, Jean‐Robert Kienast, and Jacques L. R. Touret. "Pressure‐Temperature‐Fluid Evolution in Eburnean Metabasites and Metapelites from Tamanrasset (Hoggar, Algeria)." Journal of Geology 109, no. 2 (2001): 247–63. http://dx.doi.org/10.1086/319238.

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8

Dabo, Moussa, and Tahar Aïfa. "Late Eburnean deformation in the Kolia-Boboti sedimentary basin, Kédougou-Kéniéba Inlier, Sénégal." Journal of African Earth Sciences 60, no. 3 (2011): 106–16. http://dx.doi.org/10.1016/j.jafrearsci.2011.02.005.

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9

Aïfa, Tahar, and Moussa Dabo. "Microstructures and temperature variability during the Eburnean deformations in the Daléma area, Eastern Senegal." Arabian Journal of Geosciences 8, no. 2 (2014): 677–89. http://dx.doi.org/10.1007/s12517-013-1254-1.

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10

Zamil, M. Sh. "A possible model of the Paleozoic sedimentary basins evolution at the North African platform." Proceedings of higher educational establishments. Geology and Exploration, no. 6 (December 28, 2017): 68–73. http://dx.doi.org/10.32454/0016-7762-2017-6-68-73.

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A dual model of the Paleozoic basins development, disposing on the Late Proterozoic (Pan-African) and the Early Proterozoic (Eburnean) crust, has been proposed. The formation of the first group basins is connected with the subsiding of the sections of the cooling gneissic-domes of«rejuvenated» (Early Precambrian but tectonically reworked at the end of the Proterozoic) Pan-African crust. Accordingly, the development of the second group basins is a result of the Precambrian deep sited (mantle) magmatic chambers cooling and subsiding together with the sites of the old lithosphere, covering them.

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11

Djeneb, Camara, Coulibaly Kiyinlma, Kanga Yao, Bisanz Cordelia, Delauw Marie-France, and Zirihi Guédé Noël. "Activité anti-toxoplasmose, screening phytochimique et étude de la cytotoxicité de l’extrait éthanolique 70% de Hunteria eburnea Pichon (Apocynaceae)." European Scientific Journal, ESJ 14, no. 30 (2018): 37. http://dx.doi.org/10.19044/esj.2018.v14n30p37.

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Hunteria eburnea is a medicinal plant used in traditional medicine in the Sassandra Region (Ivory Coast) in the treatment of malaria and skin diseases. The aim of this study is to study the inhibitory effect of 70% ethanolic extract of Hunteria eburneaa stem bark on Toxoplasma gondii, a protozoan parasite such as Plasmodium falciparum that causes toxoplasmosis. The 70% ethanolic extract was obtained from the parts of the plant that are used by traditional health practitioners in the Haut-Sassandra Region (Ivory Coast).The 70% ethanolic extract of Hunteria eburnea stem bark revealed high anti-T

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12

Tairou, Mahaman Sani, Pascal Affaton, Solomon Anum, and Thomas Jules Fleury. "Pan-African Paleostresses and Reactivation of the Eburnean Basement Complex in Southeast Ghana (West Africa)." Journal of Geological Research 2012 (July 17, 2012): 1–15. http://dx.doi.org/10.1155/2012/938927.

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This faulting tectonics analysis concerns the southernmost segment of the Dahomeyide Orogen and the West-African craton eastern margin in southeast Ghana. The analysis of strike-slip faults in the frontal units of the Dahomeyide Belt indicates that four distinct compressive events (NE-SW, ENE-WSW to E-W, ESE-WNW to SE-NW and SE-NW to SSE-NNW) originated the juxtaposition of the Pan-African Mobile Zone and the West-African craton. These paleostress systems define a clockwise rotation of the compressional axis during the structuring of the Dahomeyide Orogen (650–550 Ma). The SE-NW and SSE-NNW to

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13

FERRÉ, E., J. DÉLÉRIS, J. L. BOUCHEZ, A. U. LAR, and J. J. PEUCAT. "The Pan-African reactivation of Eburnean and Archaean provinces in Nigeria: structural and isotopic data." Journal of the Geological Society 153, no. 5 (1996): 719–28. http://dx.doi.org/10.1144/gsjgs.153.5.0719.

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14

Parra-Avila, Luis A., Lenka Baratoux, Aurélien Eglinger, Marco L. Fiorentini, and Sylvain Block. "The Eburnean magmatic evolution across the Baoulé-Mossi domain: Geodynamic implications for the West African Craton." Precambrian Research 332 (September 2019): 105392. http://dx.doi.org/10.1016/j.precamres.2019.105392.

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15

Bouchot, Vincent, and Jean-Louis Feybesse. "Palaeoproterozoic gold mineralization of the Etéké Archaean greenstone belt (Gabon): its relation to the Eburnean orogeny." Precambrian Research 77, no. 3-4 (1996): 143–59. http://dx.doi.org/10.1016/0301-9268(95)00047-x.

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16

White, Alistair, Ray Burgess, Norman Charnley, et al. "Constraints on the timing of late-Eburnean metamorphism, gold mineralisation and regional exhumation at Damang mine, Ghana." Precambrian Research 243 (April 2014): 18–38. http://dx.doi.org/10.1016/j.precamres.2013.12.024.

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17

Block, S., J. Ganne, L. Baratoux, et al. "Petrological and geochronological constraints on lower crust exhumation during Paleoproterozoic (Eburnean) orogeny, NW Ghana, West African Craton." Journal of Metamorphic Geology 33, no. 5 (2015): 463–94. http://dx.doi.org/10.1111/jmg.12129.

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18

Weber, Francis, François Gauthier-Lafaye, Hubert Whitechurch, Marc Ulrich, and Abderrazak El Albani. "The 2-Ga Eburnean Orogeny in Gabon and the opening of the Francevillian intracratonic basins: A review." Comptes Rendus Geoscience 348, no. 8 (2016): 572–86. http://dx.doi.org/10.1016/j.crte.2016.07.003.

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19

Caen-Vachette, M., and A. C. Umeji. "Geology and geochronology of the Okene area: evidence for an Eburnean orogenic cycle in south-central Nigeria." Journal of African Earth Sciences (and the Middle East) 7, no. 1 (1988): 121–26. http://dx.doi.org/10.1016/0899-5362(88)90058-9.

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20

Aidoo, Felix, Prosper M. Nude, Fang-Yuan Sun, Ting Liang, and Shao-Bing Zhang. "Paleoproterozoic TTG-like metagranites from the Dahomeyide Belt, Ghana: Constraints on the evolution of the Birimian-Eburnean Orogeny." Precambrian Research 353 (February 2021): 106024. http://dx.doi.org/10.1016/j.precamres.2020.106024.

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21

Dabo, Moussa, and Tahar Aïfa. "Pure shear to simple shear-dominated transpression during the Eburnean major D2 deformation, Daléma sedimentary basin, eastern Senegal." International Geology Review 55, no. 9 (2013): 1073–86. http://dx.doi.org/10.1080/00206814.2012.760711.

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22

Mapeo, R. B. M., L. V. Ramokate, F. Corfu, D. W. Davis, and A. B. Kampunzu. "The Okwa basement complex, western Botswana: U–Pb zircon geochronology and implications for Eburnean processes in southern Africa." Journal of African Earth Sciences 46, no. 3 (2006): 253–62. http://dx.doi.org/10.1016/j.jafrearsci.2006.05.005.

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23

Tanko Njiosseu, Evine Laure, Jean-Paul Nzenti, Théophile Njanko, Badibanga Kapajika, and Anne Nédélec. "New UPb zircon ages from Tonga (Cameroon): coexisting Eburnean–Transamazonian (2.1 Ga) and Pan-African (0.6 Ga) imprints." Comptes Rendus Geoscience 337, no. 6 (2005): 551–62. http://dx.doi.org/10.1016/j.crte.2005.02.005.

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24

Metelka, Václav, Lenka Baratoux, Séta Naba, and Mark W. Jessell. "A geophysically constrained litho-structural analysis of the Eburnean greenstone belts and associated granitoid domains, Burkina Faso, West Africa." Precambrian Research 190, no. 1-4 (2011): 48–69. http://dx.doi.org/10.1016/j.precamres.2011.08.002.

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25

Denchev, Teodor T., and Cvetomir M. Denchev. "Anthracoidea caricis-reznicekii (Anthracoideaceae), a new species on Carex reznicekii, and A. eburneae, a new record for the USA." Phytotaxa 244, no. 1 (2016): 69. http://dx.doi.org/10.11646/phytotaxa.244.1.5.

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A new ovariicolous smut fungus, Anthracoidea caricis-reznicekii on Carex reznicekii (C. sect. Acrocystis), is described and illustrated from the USA. The new species is compared with the known Anthracoidea species on sedges in Carex sect. Acrocystis and other closely related sections. Anthracoidea caricis-reznicekii is characterized by a complex of characters: medium-sized spores (15–24.5 μm long), thick spore wall (up to 6.0 μm thick), with conspicuous, often numerous (up to 8) protuberances, and warts 0.2–0.5 μm high. A key to the four known Anthracoidea species on sedges in section Acrocyst

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26

Ganne, J., M. Gerbault, and S. Block. "Thermo-mechanical modeling of lower crust exhumation—Constraints from the metamorphic record of the Palaeoproterozoic Eburnean orogeny, West African Craton." Precambrian Research 243 (April 2014): 88–109. http://dx.doi.org/10.1016/j.precamres.2013.12.016.

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27

Bowell, R. J., R. P. Foster, and C. J. Stanley. "Telluride mineralization at Ashanti gold mine, Ghana." Mineralogical Magazine 54, no. 377 (1990): 617–27. http://dx.doi.org/10.1180/minmag.1990.054.377.15.

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AbstractGold mineralization at the Ashanti Mine occurs in shear zones which are second-order components of a major transcrustal shear zone. However, gold-rich telluride mineralization in veins in the hangingwall of the Obuasi ore zone at Ashanti appears to have post-dated development of the major gold-bearing shear zone. Complex assemblages of goethite, chalcocite, coloradoite, calaverite, sylvanite, kostovite, petzite, stutzite, hessite, altaite, rickardite, weissite and henryite were succeeded by a relatively simple assemblage of altaite-petzite-hessite ± sylvanite ± coloradoite. Precipitati

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28

Block, Sylvain, Mark Jessell, Laurent Aillères, et al. "Lower crust exhumation during Paleoproterozoic (Eburnean) orogeny, NW Ghana, West African Craton: Interplay of coeval contractional deformation and extensional gravitational collapse." Precambrian Research 274 (March 2016): 82–109. http://dx.doi.org/10.1016/j.precamres.2015.10.014.

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29

McFarlane, H. B., L. Ailleres, P. Betts, et al. "Episodic collisional orogenesis and lower crust exhumation during the Palaeoproterozoic Eburnean Orogeny: Evidence from the Sefwi Greenstone Belt, West African Craton." Precambrian Research 325 (June 2019): 88–110. http://dx.doi.org/10.1016/j.precamres.2019.02.012.

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30

Peucat, Jean-Jacques, Ramon Capdevila, Amar Drareni, Yamina Mahdjoub, and Mohamed Kahoui. "The Eglab massif in the West African Craton (Algeria), an original segment of the Eburnean orogenic belt: petrology, geochemistry and geochronology." Precambrian Research 136, no. 3-4 (2005): 309–52. http://dx.doi.org/10.1016/j.precamres.2004.12.002.

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31

D’Lemos, R. S., J. D. Inglis, and S. D. Samson. "A newly discovered orogenic event in Morocco: Neoproterozic ages for supposed Eburnean basement of the Bou Azzer inlier, Anti-Atlas Mountains." Precambrian Research 147, no. 1-2 (2006): 65–78. http://dx.doi.org/10.1016/j.precamres.2006.02.003.

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32

Egal, Emmanuel, Denis Thiéblemont, Didier Lahondère, et al. "Late Eburnean granitization and tectonics along the western and northwestern margin of the Archean Kénéma–Man domain (Guinea, West African Craton)." Precambrian Research 117, no. 1-2 (2002): 57–84. http://dx.doi.org/10.1016/s0301-9268(02)00060-8.

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33

Debat, Pierre, Serge Nikiéma, Alain Mercier, et al. "A new metamorphic constraint for the Eburnean orogeny from Paleoproterozoic formations of the Man shield (Aribinda and Tampelga countries, Burkina Faso)." Precambrian Research 123, no. 1 (2003): 47–65. http://dx.doi.org/10.1016/s0301-9268(03)00046-9.

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34

Frimmel, Hartwig E., Ian R. Jonasson, and Petronella Mubita. "An Eburnean base metal source for sediment-hosted zinc-lead deposits in Neoproterozoic units of Namibia: Lead isotopic and geochemical evidence." Mineralium Deposita 39, no. 3 (2004): 328–43. http://dx.doi.org/10.1007/s00126-004-0410-7.

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35

Melcher, Frank. "Genesis of chemical sediments in Birimian greenstone belts: evidence from gondites and related manganese-bearing rocks from Northern Ghana." Mineralogical Magazine 59, no. 395 (1995): 229–51. http://dx.doi.org/10.1180/minmag.1995.059.395.08.

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AbstractEarly Proterozoic chemical sediments of the Birimian Supergroup in northern Ghana host several types of metamorphosed manganese-bearing rocks. Differences in the mineralogy and geochemistry can be attributed to facies changes in a mixed volcanic-volcaniclastic depositional environment. Manganese oxide-bearing phyllite, which is enriched in transition metals (Cu, Ni, Co, Zn), formed on the flanks of submarine volcanic edifices above an oxidation boundary. Towards the deeper basin, manganese silicate-rich gondites occur. These consist either of spessartine + quartz + ilmenite, or of spes

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36

Mériaud, Nicolas, Nicolas Thébaud, Quentin Masurel, et al. "Lithostratigraphic evolution of the Bandamian Volcanic Cycle in central Côte d’Ivoire: Insights into the late Eburnean magmatic resurgence and its geodynamic implications." Precambrian Research 347 (September 2020): 105847. http://dx.doi.org/10.1016/j.precamres.2020.105847.

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37

Perrouty, Stéphane, Laurent Aillères, Mark W. Jessell, Lenka Baratoux, Yan Bourassa, and Brenton Crawford. "Revised Eburnean geodynamic evolution of the gold-rich southern Ashanti Belt, Ghana, with new field and geophysical evidence of pre-Tarkwaian deformations." Precambrian Research 204-205 (May 2012): 12–39. http://dx.doi.org/10.1016/j.precamres.2012.01.003.

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38

Amores-Casals, Sandra, Antonio Olimpio Gonçalves, Joan-Carles Melgarejo, and Joan Martí Molist. "Nb and REE Distribution in the Monte Verde Carbonatite–Alkaline–Agpaitic Complex (Angola)." Minerals 10, no. 1 (2019): 5. http://dx.doi.org/10.3390/min10010005.

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The Angolan alkaline–carbonatite complex of Monte Verde has a semi-circular shape and is comprised of a central intrusion of foidolite rocks surrounded by concentrically arranged minor bodies of other alkaline rocks and carbonatite magmatic breccias. This rock association is hosted by fenitized Eburnean granites. Concentric swarms of alkaline dykes of late formation, mostly of nepheline trachyte composition, crosscut the previous units. Most high-field strength elements (HFSE) and rare earth elements (REE) are concentrated in pyrochlore crystals in the carbonatite and alkaline breccias. Magmat

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39

Pawlowski, M. L., and G. L. Hartman. "Impact of Arbuscular Mycorrhizal Species on Heterodera glycines." Plant Disease 104, no. 9 (2020): 2406–10. http://dx.doi.org/10.1094/pdis-01-20-0102-re.

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Soybean cyst nematode (SCN, Heterodera glycines) is a widely occurring pest and the leading cause of soybean yield losses in the U.S.A. There is a need to find additional SCN management strategies as sources of SCN resistance have become less effective in managing SCN populations. Arbuscular mycorrhizal fungi (AMF) form symbiotic relationships with roots of most plants including soybean. Research has shown that AMF can reduce disease severity in plants caused by pathogens and pests, including plant parasitic nematodes. The goal of this study was to evaluate the impact of AMF on SCN cyst produc

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40

Wane, Ousmane, Jean-Paul Liégeois, Nicolas Thébaud, John Miller, Václav Metelka, and Mark Jessell. "The onset of the Eburnean collision with the Kenema-Man craton evidenced by plutonic and volcanosedimentary rock record of the Masssigui region, southern Mali." Precambrian Research 305 (February 2018): 444–78. http://dx.doi.org/10.1016/j.precamres.2017.11.008.

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41

Bendaoud, Abderrahmane, Khadidja Ouzegane, Gaston Godard, et al. "Geochronology and metamorphic P-T-X evolution of the Eburnean granulite-facies metapelites of Tidjenouine (Central Hoggar, Algeria): witness of the LATEA metacratonic evolution." Geological Society, London, Special Publications 297, no. 1 (2008): 111–46. http://dx.doi.org/10.1144/sp297.6.

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42

Gassama, Ibrahima, Moussa Dabo, Mamadou Ndiaye, Emmanuel Tama Samoura, and Fatou Bop Ndong. "Meaning of Rocks Basic Enclaves in the Eburnean Granitoids of Mako Area (Kédougou-Kéniéba Inlier, Senegal): Petrogenetic Implications." International Journal of Geosciences 12, no. 01 (2021): 39–56. http://dx.doi.org/10.4236/ijg.2021.121004.

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43

Kouamelan, Alain Nicaise, Kouassi Serge Auguste Kra, Sagbrou Chérubin Djro, Jean-Louis Paquette, and Jean-Jacques Peucat. "The Logoualé Band: A large Archean crustal block in the Kenema-Man domain (Man-Leo rise, West African Craton) remobilized during Eburnean orogeny (2.05 Ga)." Journal of African Earth Sciences 148 (December 2018): 6–13. http://dx.doi.org/10.1016/j.jafrearsci.2017.09.004.

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44

WALDRON, JOHN W. F., DAVID I. SCHOFIELD, GRAHAM PEARSON, CHIRANJEEB SARKAR, YAN LUO, and ROBERT DOKKEN. "Detrital zircon characterization of early Cambrian sandstones from East Avalonia and SE Ireland: implications for terrane affinities in the peri-Gondwanan Caledonides." Geological Magazine 156, no. 07 (2018): 1217–32. http://dx.doi.org/10.1017/s0016756818000407.

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AbstractThe Caledonides of Britain and Ireland include terranes attributed to both Laurentian and Gondwanan sources, separated along the Solway line. Gondwanan elements to the south have been variably assigned to the domains Ganderia and East Avalonia. The Midland Platform forms the core of East Avalonia but its provenance is poorly known. Laser ablation split-stream analysis yields information about detrital zircon provenance by providing simultaneous U–Pb and Lu–Hf data from the same ablated volume. A sample of Red Callavia Sandstone from uppermost Cambrian Stage 3 of the Midland Platform yi

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45

Fotze, Quentin Marc Anaba, Charles Antoine Basseka, Anatole Eugene Djieto Lordon, Albert Eyike Yomba, Yves Shandini, and Jean Marie Tadjou. "Geophysical Data Processing for the Delineation of Tectonic Lineaments in South Cameroon." Earth Science Research 8, no. 2 (2019): 1. http://dx.doi.org/10.5539/esr.v8n2p1.

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The processing of aeromagnetic and gravity data of the Northern part of Congo Craton (South Cameroon region), between latitudes 2&deg;30&rsquo;-3&deg;30&rsquo; N and longitudes 12&deg;-13&deg; E, permitted the determination of the structural features ccurring within the Precambrian basement (Ntem Complex) southwards and the Pan-African belt (Yaounde Group) northwards. The maxima of the Horizontal Gradient within the study area, were obtained using the Blakely and Simpson method (1986). Those maxima were used to trace the magnetic lineaments of the study area. Furthermor

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46

Fernández-Suárez, Javier, Gabriel Gutiérrez-Alonso, George A. Jenner, and Simon E. Jackson. "Geochronology and geochemistry of the Pola de Allande granitoids (northern Spain): their bearing on the Cadomian-Avalonian evolution of northwest Iberia." Canadian Journal of Earth Sciences 35, no. 12 (1998): 1439–53. http://dx.doi.org/10.1139/e98-074.

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The Pola de Allande pre-Variscan tonalite-granodiorite plutons are located in the Narcea Antiform, at the boundary zone between the Cantabrian and west Asturian Leonese zones of the Iberian Variscan belt. These granitoids were intruded into a Neoproterozoic siliciclastic sedimentary sequence with subordinate volcanic intercalations and were subsequently overprinted by Variscan thrust-related shear deformation. U-Pb laser ablation inductively coupled plasma - mass spectrometry (ICP-MS) dating of zircons from two plutons yielded concordant ages of intrusion of 605 ± 10 and 580 ± 15 Ma. To the au

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47

Kanouo, Nguo Sylvestre, David Richard Lentz, Khin Zaw, et al. "New Insights into Pre-to-Post Ediacaran Zircon Fingerprinting of the Mamfe PanAfrican Basement, SW Cameroon: A Possible Link with Rocks in SE Nigeria and the Borborema Province of NE Brazil." Minerals 11, no. 9 (2021): 943. http://dx.doi.org/10.3390/min11090943.

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The pre- to post-Late Neoproterozoic geological histories in the south to southwestern part of Mamfe Basin (SW Cameroon) were reported following analysis of the zircon crystals from their host rocks. A genetic model was developed for the zircon host rocks’ formation conditions, and the registered post-emplacement events were presented. The obtained ages were correlated with the data available for rocks in the Cameroon Mobile Belt, SE Nigeria, and the Borborema Province of NE Brazil. Separated zircons from Araru black to whitish gneiss, Araru whitish-grey gneiss, and Mboifong migmatite were ana

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Hirdes, W., and D. W. Davis. "U–Pb Geochronology of Paleoproterozoic Rocks in the Southern Part of the Kedougou-Kéniéba Inlier, Senegal, West Africa: Evidence for Diachronous Accretionary Development of the Eburnean Province." Precambrian Research 118, no. 1-2 (2002): 83–99. http://dx.doi.org/10.1016/s0301-9268(02)00080-3.

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Marzoli, Andrea, Hervé Bertrand, Nasrrddine Youbi, et al. "The Central Atlantic Magmatic Province (CAMP) in Morocco." Journal of Petrology 60, no. 5 (2019): 945–96. http://dx.doi.org/10.1093/petrology/egz021.

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Abstract The Central Atlantic Magmatic Province (CAMP) is a large igneous province (LIP) composed of basic dykes, sills, layered intrusions and lava flows emplaced before Pangea break-up and currently distributed on the four continents surrounding the Atlantic Ocean. One of the oldest, best preserved and most complete sub-provinces of the CAMP is located in Morocco. Geochemical, geochronologic, petrographic and magnetostratigraphic data obtained in previous studies allowed identification of four strato-chemical magmatic units, i.e. the Lower, Intermediate, Upper and Recurrent units. For this s

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Gouedji, Franck, Christian Picard, Yacouba Coulibaly, et al. "The Samapleu mafic-ultramafic intrusion and its Ni-Cu-PGE mineralization: an Eburnean (2.09 Ga) feeder dyke to the Yacouba layered complex (Man Archean craton, western Ivory Coast)." Bulletin de la Société Géologique de France 185, no. 6 (2014): 393–411. http://dx.doi.org/10.2113/gssgfbull.185.6.393.

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Abstract The Yacouba layered complex intrudes the Archean (3.5–2.7 Ga) Kenema-Man craton in the Samapleu-Yorodougou area, western Ivory Coast. In Samapleu area, the complex was recognized in drill holes at three locations: Samapleu Main (SM); Samapleu Extension 1 (E1) and Yorodougou (Yo). It comprises websterites, peridotites and gabbro-norites arranged symmetrically with mafic layers at the center and ultramafic layers at both margins. The complex is inclined at 70–80° to the SE. The thickness of individual layers varies from 2 to 60 m and the total thickness is 120 to 200 m. At the E1 site,

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