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Relevant bibliographies by topics / Eburnean

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Journal articles

Academic literature on the topic 'Eburnean'

Author: Grafiati

Published: 4 June 2021

Last updated: 12 February 2022

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Journal articles on the topic "Eburnean"

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 three-dimensional partitioning of progressive transpressional deformation and interactions among shear zones that absorbed heterogeneities in the regional flow patterns while maintaining the connectivity of the shear zone network. Such orogen-scale kinematic patterns call for caution in using the deformation phase approach without considering the “bigger structural picture” and interpreting displacement history of individual shear zones in terms of plate kinematics. The West African shear zone pattern is linked to that of the Guiana shield through a new transatlantic correlation to produce an integrated kinematic model of the Eburnean-Transamazonian orogen.

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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. The manifestation of the Vendian volcanic units on Anti-Atlas, Ugarta, Regibat-Eglab uplifts is the most possible evidence of the mantle magmatic activity, which could create those chambers.

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