{"id":507,"date":"2021-05-07T20:04:19","date_gmt":"2021-05-07T20:04:19","guid":{"rendered":"http:\/\/pr-lakhloufi.com\/?p=507"},"modified":"2021-05-09T15:05:19","modified_gmt":"2021-05-09T15:05:19","slug":"article-tahiri-conclusion","status":"publish","type":"post","link":"https:\/\/pr-lakhloufi.com\/en\/2021\/05\/07\/article-tahiri-conclusion\/","title":{"rendered":"Article Tahiri: Conclusion"},"content":{"rendered":"\t\t
\n\t\t\t\t\t\t
\n\t\t\t\t\t\t
\n\t\t\t\t\t
\n\t\t\t
\n\t\t\t\t\t\t
\n\t\t\t\t
\n\t\t\t\t\t\t\t\t\t

\nFr<\/a> Ar<\/a><\/span> [glt language=\u00a0\u00bbEnglish\u00a0\u00bb label=\u00a0\u00bb(English auto)\u00a0\u00bb image=\u00a0\u00bbyes\u00a0\u00bb text=\u00a0\u00bbyes\u00a0\u00bb image_size=\u00a0\u00bb22″]<\/p>\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/section>\n\t\t\t\t

\n\t\t\t\t\t\t
\n\t\t\t\t\t
\n\t\t\t
\n\t\t\t\t\t\t
\n\t\t\t\t
\n\t\t\t\t\t\t\t\t\t

\u00a0 Nous avions mis en \u00e9vidence le chevauchement ant\u00e9-carbonif\u00e8re du BS vers le sud, \u00e9v\u00e9nement que la datation radiom\u00e9trique des granodiorites de Rabat \u00e0 367 Ma (fin du D\u00e9vonien) corrobore. Aussi, la \u201ccollision\u201d du BS avec le nord de la MM est corrobor\u00e9 par nos donn\u00e9es de terrains qui montrent que la partie E-W du \u00ab\u00a0BSB\u00a0\u00bb que nous avons d\u00e9nomm\u00e9e BBM (situ\u00e9e entre le BS au nord et le Bloc de Zaer \u2013 Oulm\u00e8s au sud) ne s\u2019est ouverte qu\u2019au Vis\u00e9en moyen. Ces faits confirment alors l\u2019absence d\u00e9montr\u00e9e d\u2019une \u00abformation chaotique\u00bb au niveau de la ZRT.<\/p>

\u00a0\u00a0 Par ailleurs, il serait peu concevable que les granodiorites d\u2019\u00e2ge 605 \u2013 609 Ma seuls t\u00e9moignent de la pr\u00e9sence d\u2019un socle prot\u00e9rozo\u00efque que surmontent des terrains ordoviciens. Nous avons montr\u00e9 que ces granito\u00efdes (ind\u00e9pendamment de leur \u00e2ge) affleurent au sein de la ZCNM, o\u00f9 ils c\u00f4toient tectoniquement des roches s\u00e9dimentaires allant du Cambrien moyen (BS) au Vis\u00e9en sup\u00e9rieur et des roches basiques (d\u2019\u00e2ge ordovicien). Ce m\u00e9lange tectonique de terrains de nature et d\u2019\u00e2ge tr\u00e8s vari\u00e9s r\u00e9sulte d\u2019un coulissage dextre majeur \u00e0 composante inverse de vergence nord d\u2019\u00e2ge post vis\u00e9en. C\u2019est dans cette logique et celle du chevauchement fini D\u00e9vonien du BS vers le sud qu\u2019il faut chercher l\u2019explication de la pr\u00e9sence des granodiorites du Prot\u00e9rozo\u00efque tardif. Enfin, le mod\u00e8le de Simancas et al (2009) doit \u00eatre r\u00e9vis\u00e9 \u00e0 la lumi\u00e8re de nos r\u00e9centes donn\u00e9es et en tenant compte du chevauchement du BS vers le sud vers la fin du D\u00e9vonien dat\u00e9 relativement et radio-m\u00e9triquement.<\/p>

R\u00e9f\u00e9rences\u00a0 bibliographiques<\/strong><\/p>

Bouabdelli, M., Piqu\u00e9, A., 1996. Du bassin sur d\u00e9crochement au bassin d\u2019avant pays : dynamique du bassin d\u2019Azrou \u2013 Kh\u00e9nifra (Maroc hercynien central). J. Afr. Earth Sci. 22, 213-224.<\/p>

Cailleux, Y., Deloche, Ch., Gonord\u00a0, H. et Rolin, P. (1984)\u00a0: Mise en \u00e9vidence de deux couloirs de cisaillement dans la zone pal\u00e9ozo\u00efque de Rabat \u2013 Tiflet (Maroc nord). C. R. Acad. Sci., Paris, 299, II. Pp. 569 \u2013 572.<\/p>

El Hassani, A., 1991. La zone de Rabat \u2013 Tiflet. Bordure Nord de la cha\u00eene cal\u00e9dono \u2013 hercynienne du Maroc. Bull. Inst. Sci. Rabat. 15, 1-134.<\/p>

El Hassani, A., Zahraoui, M., 1989. Le Pal\u00e9ozo\u00efque de la r\u00e9gion de Rabat (Maroc)\u00a0: structures hercyniennes tangentielles, \u00e2ge des d\u00e9formations superpos\u00e9es et mise en place de nappes. Notes et M\u00e9m. Serv. g\u00e9ol. Maroc, n\u00b0 335. pp.211-219.<\/p>

Hamel, C., 1968. Etude g\u00e9ologique des sites de barrage des oueds Grou et Bou Regreg (r\u00e9gion de Rabat). Rapp. In\u00e9dit, Div. Ressources en eau, Min. Trav. Publi. Et Comm., Rabat.<\/p>

Hoepffner, ch., Soulaimani, A. et Piqu\u00e9, A. (2005). The Moroccan Hercynides. J. Afr. Earth Sci. 43, 144 \u2013 165.<\/p>

Izart, A., Vieselet, J.L., 1988. Stratigraphie, s\u00e9dimentologie et micropal\u00e9ontologie des s\u00e9diments du Bassin de Sidi Bettache et ses bordures (Meseta marocaine nord occidentale) du Famennien au Vis\u00e9en sup\u00e9rieur. Notes et M\u00e9m. Serv. g\u00e9ol. Maroc, 334, pp. 7-41.<\/p>

LAKHLOUFI, A., HAMOUMI, N., SAQUAQUE, A., AARAB, A. et JERMOUNI, A. 2000. EL Magmatismo Basico en la Cuenca Fameno- Dinantiense de Sidi Bettache (Marruecos Hercinico Noroccidental)\u00a0: Nuevos Datos. Geogaceta, 28.<\/p>

Lakhloufi, A., Hammoumi, N., Saquaque, A., 2001. Vergence des structures varisques et modalit\u00e9s de la structuration du Bassin de Sidi Bettache (Maroc hercynien nord occidental)\u00a0: implications g\u00e9odynamiques. Bol. R. Soc. Esp. Hit. Nat. (Sec. Geol.), 96 (3-4), 17-28.<\/p>

Lakhloufi, A., 2007. Les bassins famenno \u2013 dinantiens (Maroc)\u00a0: nouvelle conception de la g\u00e9odynamique hercynienne. Notes et M\u00e9m. Serv. G\u00e9ol. Maroc, n\u00b0 526. 255 p.<\/p>

Padgett, G., Ehrlich, R., Moody, M. 1977. Submarine debris flow deposit in extensional setting. Upper Devonian of western Morocco. J. Sedim. Petrol., 47, pp. 811-818.<\/p>

Piqu\u00e9, A., 1979. Evolution structurale d\u2019un segment de la cha\u00eene hercynienne\u00a0: la Meseta marocaine nord \u2013 occidentale. Sci. G\u00e9ol. M\u00e9m., Strasbourg, 56, 243p.<\/p>

Piqu\u00e9, A., 1984. Faci\u00e8s s\u00e9dimentaire et \u00e9volution d\u2019un bassin\u00a0: le bassin d\u00e9vono \u2013 dinantien de Sidi Bettache (Maroc nord-ocidental). Bull. Soc. G\u00e9ol. France 6, 1015-1024.<\/p>

Piqu\u00e9, A., 1994. G\u00e9ologie du Maroc\u00a0: les domaines r\u00e9gionaux et leur \u00e9volution structurale. 239p, \u00e9dit. pumag, El Jadida, Maroc.<\/p>

Simancas, J. F., Azor, A., Martines-Poyatos, D., Tahiri, A., El Hadi, H., Gonzalez-Lodeiro, F., P\u00e9rez-Estaun, A., et Carbonell, R. (2009). Tectonic relationships of southwest Iberian with the allochtons of Northwest Iberia and the Moroccan Variscides, C. R. Geoscience, doi: 10.101\/j.crte.2008.11.003.<\/p>\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/section>\n\t\t\t\t

\n\t\t\t\t\t\t
\n\t\t\t\t\t
\n\t\t\t
\n\t\t\t\t\t\t
\n\t\t\t\t
\n\t\t\t\t\t\t\t\t\t
\n

\u0644\u0642\u062f \u0628\u0631\u0647\u0646\u0627 \u0633\u062a\u0631\u0627\u062a\u064a\u063a\u0631\u0627\u0641\u064a\u0627\u060c \u0645\u0646 \u062e\u0644\u0627\u0644 \u0627\u0644\u062a\u0623\u0631\u064a\u062e \u0627\u0644\u0646\u0633\u0628\u064a\u060c \u0639\u0644\u0649 \u0623\u0646 \u062a\u0631\u0627\u0643\u0628 \u0643\u062a\u0644\u0629 \u0627\u0644\u0633\u0647\u0648\u0644 \u0646\u062d\u0648 \u0627\u0644\u062c\u0646\u0648\u0628 \u062d\u062f\u062b \u0642\u0628\u0644 \u0627\u0644\u0643\u0627\u0631\u0628\u0648\u0646\u0641\u064a\u0631 (\u0627\u0644\u0639\u0635\u0631 \u0627\u0644\u0643\u0631\u0628\u0648\u0646\u064a)\u060c \u0648\u0647\u0648 \u0645\u0627 \u0623\u0643\u062f\u0647 \u0627\u0644\u062a\u0623\u0631\u064a\u062e \u0627\u0644\u0625\u0634\u0639\u0627\u0639\u064a \u0644\u063a\u0631\u0627\u0646\u064a\u062a \u0627\u0644\u0631\u0628\u0627\u0637 (\u0627\u0644\u0645\u0642\u0627\u0644\u0629 \u0645\u0648\u0636\u0639 \u0627\u0644\u0646\u0642\u062f) \u0627\u0644\u0630\u064a \u064a\u0641\u064a\u062f \u0628\u0623\u0646\u0647 \u062a\u0645\u0648\u0636\u0639 \u0642\u0628\u0644 367 \u0645\u0644\u064a\u0648\u0646 \u0633\u0646\u0629 \u0645\u0646 \u0627\u0644\u0622\u0646\u060c \u0623\u064a \u062e\u0644\u0627\u0644 \u0646\u0647\u0627\u064a\u0629 \u0627\u0644\u062f\u064a\u0641\u0648\u0646\u064a\u0627\u0646. \u0643\u0645\u0627 \u0623\u0646 \u00ab\u00a0\u062a\u0635\u0627\u062f\u0645\u00a0\u00bb \u0643\u062a\u0644\u0629 \u0627\u0644\u0633\u0647\u0648\u0644 \u0628\u0634\u0645\u0627\u0644 \u0627\u0644\u0645\u064a\u0633\u064a\u0637\u0627 \u0627\u0644\u063a\u0631\u0628\u064a\u0629 \u062a\u0624\u0643\u062f\u0647 \u0643\u0630\u0644\u0643 \u0627\u0644\u0645\u0639\u0637\u064a\u0627\u062a \u0627\u0644\u0645\u064a\u062f\u0627\u0646\u064a\u0629 \u0627\u0644\u062a\u064a \u062a\u0641\u064a\u062f \u0628\u0623\u0646 \u062d\u0648\u0636 \u0628\u0631\u0627\u0634\u0648\u0627 \u2013 \u0645\u0639\u0627\u0632\u064a\u0632 (\u0627\u0644\u0642\u0637\u0627\u0639 \u0627\u0644\u0634\u0631\u0642\u064a \u0644\u062d\u0648\u0636 \u0633\u064a\u062f\u064a \u0628\u0637\u0627\u0634 \u0643\u0645\u0627 \u0639\u0631\u0641\u0647 \u0628\u064a\u0643\u064a\u060c 1979 ) \u0627\u0644\u0630\u064a \u062a\u062d\u062f\u0647 \u0643\u062a\u0644\u0629 \u0627\u0644\u0633\u0647\u0648\u0644 \u0634\u0645\u0627\u0644\u0627 \u0648\u0643\u062a\u0644\u0629 \u0632\u0639\u064a\u0631 \u2013 \u0648\u0644\u0645\u0627\u0633 \u062c\u0646\u0648\u0628\u0627\u060c \u062a\u0643\u0648\u0646 \u0641\u0642\u0637 \u062e\u0644\u0627\u0644 \u0627\u0644\u0641\u064a\u0632\u064a\u0627\u0646 \u0627\u0644\u0623\u0648\u0633\u0637. \u0647\u0627\u062a\u0647 \u0627\u0644\u062d\u0642\u0627\u0626\u0642 \u062a\u0624\u0643\u062f\u0647\u0627 \u0643\u0630\u0644\u0643 \u062d\u0642\u064a\u0642\u0629 \u0639\u062f\u0645 \u0648\u062c\u0648\u062f \u062a\u0634\u0643\u064a\u0644 \u0641\u0648\u0636\u0648\u064a \u0631\u0633\u0648\u0628\u064a \u0639\u0644\u0649 \u0645\u0633\u062a\u0648\u0649 \u0645\u0646\u0637\u0642\u0629 \u0627\u0644\u0631\u0628\u0627\u0637 \u2013 \u062a\u0641\u0644\u062a \u0627\u0644\u0628\u0627\u0644\u064a\u0648\u0632\u0648\u064a\u0629\u060c \u0643\u0645\u0627 \u0623\u0648\u0636\u062d\u0646\u0627 \u0630\u0644\u0643 \u0628\u0627\u0644\u062f\u0644\u064a\u0644 \u0648\u0627\u0644\u0628\u0631\u0647\u0627\u0646.<\/span><\/p>\n

\u0639\u0644\u0627\u0648\u0629 \u0639\u0644\u0649 \u0630\u0644\u0643 \u060c \u0641\u0644\u064a\u0633 \u0645\u0646 \u0627\u0644\u0645\u0639\u0642\u0648\u0644 \u0623\u0646 \u062a\u0643\u0648\u0646 \u0627\u0633\u062a\u0633\u0637\u0627\u062d\u0627\u062a \u0627\u0644\u063a\u0631\u0627\u0646\u0648\u062f\u064a\u0648\u0631\u064a\u062a \u0627\u0644\u0630\u064a \u062a\u062a\u0631\u0627\u0648\u062d \u0623\u0639\u0645\u0627\u0631\u0647 \u0628\u064a\u0646 605 \u0648 609 \u0645\u0644\u064a\u0648\u0646 \u0633\u0646\u0629 \u0647\u064a \u0627\u0644\u0648\u062d\u064a\u062f\u0629 \u0627\u0644\u0634\u0627\u0647\u062f\u0629 \u0639\u0644\u0649 \u0648\u062c\u0648\u062f \u0642\u0627\u0639 \u0628\u0631\u0648\u062a\u064a\u0631\u0648\u0632\u0648\u064a\u0643\u064a \u064a\u0639\u0644\u0648\u0647 \u0627\u0644\u063a\u0637\u0627\u0621 \u0627\u0644\u0631\u0633\u0648\u0628\u064a \u0627\u0644\u0630\u064a \u064a\u0628\u062f\u0623 \u0645\u0639 \u0627\u0644\u0623\u0648\u0631\u062f\u0648\u0641\u064a\u0633\u064a\u0627\u0646. \u0641\u0644\u0642\u062f \u0628\u064a\u0646\u0627\u060c \u0628\u0645\u0627 \u064a\u0643\u0641\u064a \u0645\u0646 \u0627\u0644\u0628\u0631\u0627\u0647\u064a\u0646 \u0627\u0644\u0645\u064a\u062f\u0627\u0646\u064a\u0629\u060c \u0623\u0646 \u0647\u0630\u0647 \u0627\u0644\u063a\u0631\u0627\u0646\u064a\u062a\u0627\u062a (\u0628\u063a\u0636 \u0627\u0644\u0646\u0638\u0631 \u0639\u0646 \u0639\u0645\u0631\u0647\u0627) \u0639\u0628\u0627\u0631\u0629 \u0639\u0646 \u0627\u0633\u062a\u0633\u0637\u0627\u062d\u0627\u062a \u0645\u0628\u0639\u062b\u0631\u0629\u060c \u0645\u0634\u062a\u062a\u0629 \u062f\u0627\u062e\u0644 \u0645\u062c\u0627\u0644 \u0627\u0646\u0642\u0635\u0627\u0641 \u0634\u0645\u0627\u0644 \u0627\u0644\u0645\u064a\u0633\u064a\u0637\u0627 (ZCNM )\u060c \u062d\u064a\u062b \u062a\u062e\u062a\u0644\u0637 \u062a\u0643\u062a\u0648\u0646\u064a\u0627 \u0628\u0627\u0644\u0635\u062e\u0648\u0631 \u0627\u0644\u0631\u0633\u0648\u0628\u064a\u0629 \u0627\u0644\u062a\u064a \u064a\u0645\u062a\u062f \u0639\u0645\u0631\u0647\u0627 \u0645\u0646 \u0627\u0644\u0643\u0627\u0645\u0628\u0631\u064a\u0627\u0646 \u0627\u0644\u0623\u0648\u0633\u0637 \u0625\u0644\u0649 \u0627\u0644\u0641\u064a\u0632\u064a\u0627\u0646 \u0627\u0644\u0639\u0644\u0648\u064a \u0648\u0643\u0630\u0627 \u0627\u0644\u0635\u062e\u0648\u0631 \u0627\u0644\u0635\u0647\u0627\u0631\u064a\u0629 \u0627\u0644\u0642\u0627\u0639\u062f\u064a\u0629 \u0628\u0639\u0645\u0631 \u0627\u0644\u0623\u0648\u0631\u062f\u0648\u0641\u064a\u0633\u064a\u0627\u0646. \u062a\u062a\u0631\u0627\u0648\u062d \u0645\u0646 \u0627\u0644\u0639\u0635\u0631 \u0627\u0644\u0643\u0645\u0628\u0631\u064a \u0627\u0644\u0623\u0648\u0633\u0637 (BS) \u0625\u0644\u0649 \u0623\u0639\u0627\u0644\u064a Visean \u0648\u0627\u0644\u0635\u062e\u0648\u0631 \u0627\u0644\u0623\u0633\u0627\u0633\u064a\u0629 (\u0627\u0644\u0639\u0635\u0631 \u0627\u0644\u0623\u0648\u0631\u062f\u0648\u0641\u064a\u0634\u064a. \u0647\u0630\u0627 \u0627\u0644\u0645\u0632\u064a\u062c \u0627\u0644\u062a\u0643\u062a\u0648\u0646\u064a \u0645\u0646 \u0627\u0644\u0635\u062e\u0648\u0631 \u0630\u0627\u062a \u0637\u0628\u064a\u0639\u0629 \u0648\u0623\u0639\u0645\u0627\u0631 \u062c\u062f \u0645\u062a\u0646\u0648\u0639\u0629 \u0648\u0627\u0644\u0646\u0627\u062a\u062c\u0629 \u0639\u0646 \u0627\u0644\u0627\u0646\u0632\u0644\u0627\u0642 \u0627\u0644\u0645\u064a\u0627\u0645\u0646 \u0627\u0644\u0630\u064a \u0639\u0631\u0641\u0647 \u0646\u0637\u0627\u0642 \u0627\u0646\u0642\u0635\u0627\u0641 \u0634\u0645\u0627\u0644 \u0627\u0644\u0645\u064a\u0633\u064a\u0637\u0627 \u0645\u0627 \u0628\u0639\u062f \u0627\u0644\u0641\u064a\u0632\u064a\u0627\u0646. \u0641\u0636\u0645\u0646 \u0647\u0630\u0627 \u0627\u0644\u0633\u064a\u0627\u0642 \u0627\u0644\u062a\u0643\u062a\u0648\u0646\u064a \u0644\u0645\u0627 \u0628\u0639\u062f \u0627\u0644\u0641\u064a\u0632\u064a\u0627\u0646 \u062a\u0643\u0645\u0646 \u0627\u0644\u0625\u062c\u0627\u0628\u0629 \u0639\u0646 \u0633\u0628\u0628 \u0648\u062d\u064a\u062b\u064a\u0627\u062a \u062a\u0648\u0627\u062c\u062f \u063a\u0631\u0627\u0646\u0648\u062f\u064a\u0648\u0631\u064a\u062a \u0627\u0644\u0628\u0631\u0648\u062a\u064a\u0631\u0648\u0632\u0648\u064a\u0643. \u0623\u062e\u064a\u0631\u064b\u0627\u060c \u0646\u0645\u0648\u0630\u062c \u00ab\u00a0\u0633\u064a\u0645\u0648\u0646\u0643\u0627\u00a0\u00bb \u0648\u0641\u0631\u064a\u0642\u0647 (Simancas et al., 2009) \u064a\u062a\u0637\u0644\u0628 \u0627\u0644\u0645\u0631\u0627\u062c\u0639\u0629 \u0639\u0644\u0649 \u0645\u0639\u0637\u064a\u0627\u062a\u0646\u0627 \u0627\u0644\u0645\u064a\u062f\u0627\u0646\u064a\u0629 \u0627\u0644\u062d\u062f\u064a\u062b\u0629\u060c \u0623\u062e\u0630\u0627 \u0628\u0639\u064a\u0646 \u0627\u0644\u0627\u0639\u062a\u0628\u0627\u0631 \u062a\u0631\u0627\u0643\u0628 \u0643\u062a\u0644\u0629 \u0627\u0644\u0633\u0647\u0648\u0644 \u0646\u062d\u0648 \u0627\u0644\u062c\u0646\u0648\u0628 \u0641\u064a \u0646\u0647\u0627\u064a\u0629 \u0627\u0644\u062f\u064a\u0641\u0648\u0646\u064a\u0627\u0646 \u0627\u0644\u0645\u0624\u0631\u062e \u0646\u0633\u0628\u064a\u0627 \u0648\u0625\u0634\u0639\u0627\u0639\u064a\u0627.<\/span><\/p>\n

R\u00e9f\u00e9rences bibliographiques<\/strong><\/span><\/p>\n

Bouabdelli, M., Piqu\u00e9, A., 1996. Du bassin sur d\u00e9crochement au bassin d\u2019avant pays : dynamique du bassin d\u2019Azrou – Kh\u00e9nifra (Maroc hercynien central). J. Afr. Earth Sci. 22, 213-224.<\/span><\/p>\n

Cailleux, Y., Deloche, Ch., Gonord , H. et Rolin, P. (1984) : Mise en \u00e9vidence de deux couloirs de cisaillement dans la zone pal\u00e9ozo\u00efque de Rabat \u2013 Tiflet (Maroc nord). C. R. Acad. Sci., Paris, 299, II. Pp. 569 \u2013 572.<\/span><\/p>\n

El Hassani, A., 1991. La zone de Rabat \u2013 Tiflet. Bordure Nord de la cha\u00eene cal\u00e9dono \u2013 hercynienne du Maroc. Bull. Inst. Sci. Rabat. 15, 1-134.<\/span><\/p>\n

El Hassani, A., Zahraoui, M., 1989. Le Pal\u00e9ozo\u00efque de la r\u00e9gion de Rabat (Maroc) : structures hercyniennes tangentielles, \u00e2ge des d\u00e9formations superpos\u00e9es et mise en place de nappes. Notes et M\u00e9m. Serv. g\u00e9ol. Maroc, n\u00b0 335. pp.211-219.<\/span><\/p>\n

Hamel, C., 1968. Etude g\u00e9ologique des sites de barrage des oueds Grou et Bou Regreg (r\u00e9gion de Rabat). Rapp. In\u00e9dit, Div. Ressources en eau, Min. Trav. Publi. Et Comm., Rabat.<\/span><\/p>\n

Hoepffner, ch., Soulaimani, A. et Piqu\u00e9, A. (2005). The Moroccan Hercynides. J. Afr. Earth Sci. 43, 144 \u2013 165.<\/span><\/p>\n

Izart, A., Vieselet, J.L., 1988. Stratigraphie, s\u00e9dimentologie et micropal\u00e9ontologie des s\u00e9diments du Bassin de Sidi Bettache et ses bordures (Meseta marocaine nord occidentale) du Famennien au Vis\u00e9en sup\u00e9rieur. Notes et M\u00e9m. Serv. g\u00e9ol. Maroc, 334, pp. 7-41.<\/span><\/p>\n

LAKHLOUFI, A., HAMOUMI, N., SAQUAQUE, A., AARAB, A. et JERMOUNI, A. 2000. EL Magmatismo Basico en la Cuenca Fameno- Dinantiense de Sidi Bettache (Marruecos Hercinico Noroccidental) : Nuevos Datos. Geogaceta, 28.<\/span><\/p>\n

Lakhloufi, A., Hammoumi, N., Saquaque, A., 2001. Vergence des structures varisques et modalit\u00e9s de la structuration du Bassin de Sidi Bettache (Maroc hercynien nord occidental) : implications g\u00e9odynamiques. Bol. R. Soc. Esp. Hit. Nat. (Sec. Geol.), 96 (3-4), 17-28.<\/span><\/p>\n

Lakhloufi, A., 2007. Les bassins famenno \u2013 dinantiens (Maroc) : nouvelle conception de la g\u00e9odynamique hercynienne. Notes et M\u00e9m. Serv. G\u00e9ol. Maroc, n\u00b0 526. 255 p.<\/span><\/p>\n

Padgett, G., Ehrlich, R., Moody, M. 1977. Submarine debris flow deposit in extensional setting. Upper Devonian of western Morocco. J. Sedim. Petrol., 47, pp. 811-818.<\/span><\/p>\n

Piqu\u00e9, A., 1979. Evolution structurale d\u2019un segment de la cha\u00eene hercynienne : la Meseta marocaine nord \u2013 occidentale. Sci. G\u00e9ol. M\u00e9m., Strasbourg, 56, 243p. <\/span><\/p>\n

Piqu\u00e9, A., 1984. Faci\u00e8s s\u00e9dimentaire et \u00e9volution d\u2019un bassin : le bassin d\u00e9vono \u2013 dinantien de Sidi Bettache (Maroc nord-ocidental). Bull. Soc. G\u00e9ol. France 6, 1015-1024.<\/span><\/p>\n

Piqu\u00e9, A., 1994. G\u00e9ologie du Maroc : les domaines r\u00e9gionaux et leur \u00e9volution structurale. 239p, \u00e9dit. pumag, El Jadida, Maroc.<\/span><\/p>\n

Simancas, J. F., Azor, A., Martines-Poyatos, D., Tahiri, A., El Hadi, H., Gonzalez-Lodeiro, F., P\u00e9rez-Estaun, A., et Carbonell, R. (2009). Tectonic relationships of southwest Iberian with the allochtons of Northwest Iberia and the Moroccan Variscides, C. R. Geoscience, doi: 10.101\/j.crte.2008.11.003.<\/span><\/p>\n\n<\/div>\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/section>\n\t\t\t\t<\/div>\n\t\t","protected":false},"excerpt":{"rendered":"

Fr Ar [glt language=\u00a0\u00bbEnglish\u00a0\u00bb label=\u00a0\u00bb(English auto)\u00a0\u00bb image=\u00a0\u00bbyes\u00a0\u00bb text=\u00a0\u00bbyes\u00a0\u00bb image_size=\u00a0\u00bb22″] \u00a0 Nous avions mis en \u00e9vidence le chevauchement ant\u00e9-carbonif\u00e8re du BS vers le sud, \u00e9v\u00e9nement que la datation radiom\u00e9trique des granodiorites de Rabat \u00e0 367 Ma (fin du D\u00e9vonien) corrobore. Aussi, la \u201ccollision\u201d du BS avec le nord de la MM est corrobor\u00e9 par nos donn\u00e9es […]<\/p>\n","protected":false},"author":1,"featured_media":0,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[2],"tags":[],"class_list":["post-507","post","type-post","status-publish","format-standard","hentry","category-article"],"_links":{"self":[{"href":"https:\/\/pr-lakhloufi.com\/en\/wp-json\/wp\/v2\/posts\/507","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/pr-lakhloufi.com\/en\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/pr-lakhloufi.com\/en\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/pr-lakhloufi.com\/en\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/pr-lakhloufi.com\/en\/wp-json\/wp\/v2\/comments?post=507"}],"version-history":[{"count":13,"href":"https:\/\/pr-lakhloufi.com\/en\/wp-json\/wp\/v2\/posts\/507\/revisions"}],"predecessor-version":[{"id":907,"href":"https:\/\/pr-lakhloufi.com\/en\/wp-json\/wp\/v2\/posts\/507\/revisions\/907"}],"wp:attachment":[{"href":"https:\/\/pr-lakhloufi.com\/en\/wp-json\/wp\/v2\/media?parent=507"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/pr-lakhloufi.com\/en\/wp-json\/wp\/v2\/categories?post=507"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/pr-lakhloufi.com\/en\/wp-json\/wp\/v2\/tags?post=507"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}