气候变化领域集成服务门户(CCPortal): The structure of the Central-Eastern External Rif (Morocco); Poly-phased deformation and role of the under-thrusting of the North-West African paleo-margin

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DOI	10.1016/j.earscirev.2020.103198
	The structure of the Central-Eastern External Rif (Morocco); Poly-phased deformation and role of the under-thrusting of the North-West African paleo-margin
	Gimeno-Vives O.; de Lamotte D.F.; Leprêtre R.; Haissen F.; Atouabat A.; Mohn G.
发表日期	2020
ISSN	00128252
卷号	205
英文摘要	The Rif belt (Northern Morocco) forms the western edge of the Alpine-Himalayan orogenic system, resulting from the progressive closure of the Tethys oceanic domain between the Africa and Eurasia plates. The External Rif, topic of this paper, comprises three paleogeographic zones, namely the Prerif, Mesorif and Intrarif, inherited from the zonation of the North-West African paleo-margin from proximal to distal domains, respectively. Its current architecture displays tectonic windows (belonging to the Mesorif) at depth supporting far-travelled thrust-sheets (namely, the Senhadja and Higher Nappes of Mesorif and Intrarif origin, respectively). A puzzling aspect of the Mesorif structure is the coexistence of metamorphic and non-metamorphic units within the tectonic windows and Senhadja Nappes. In particular, the latter presents a chaotic structure, which origin remains under debate. We integrate previous studies and new data (field observations, geological mapping and thermochronology results) to reassess the structure of the External Rif and propose an up-dated interpretation of its Cenozoic evolution. In the Prerif and Mesorif, we highlight a poly-phased tectonic evolution occurring before and after a major unconformity (the “Mesorif Unconformity”). This unconformity seals a pre-Miocene compressional event that we relate to the under-thrusting of the North-African paleo-margin below the Maghrebian Tethys (the former Tethys branch located between South Iberia and North Africa). The MP-LT metamorphism, recorded in the metamorphic tectonic window of the Temsamane Massif, is a direct vestige of this process. After the “Mesorif Unconformity”, i.e. during the Miocene, the regional geodynamics is ruled by the westward translation of the Alboran Domain and the coeval out-of-sequence deformation of the “oceanic” units in front of it (Flyschs and Intrarif Units, the most internal parts of the External Rif). This process directly results from the subduction of the Maghrebian Tethys below the Alboran Domain. The docking of the Intrarif Units against the already exhumed Temsamane Units and Senhadja Nappes generated an uplift and the subsequent detachment of the top of the Intrarif lithostratigraphic pile, forming the Higher Nappes. We show that the chaotic structure of the Senhadja Nappes is only apparent, being mostly inherited from the Mesozoic rifting. Results of apatite fission track, apatite helium dating and thermal modeling from the gabbroic intrusions of the Senhadja Nappes confirm an overburden by the Higher Nappes and their subsequent exhumation during the Upper Miocene. Finally, all these elements are integrated in a coherent model incorporating the External Rif in the geodynamics of the West Mediterranean. © 2020
关键词	External Rif structure North-West African paleo-margin under-thrusting Senhadja Nappe Thermochronology
英文关键词	African plate; continental margin; deformation; Eurasian plate; fission track dating; metamorphism; paleoceanography; rifting; tectonic evolution; Tethys; thrust; unconformity; Morocco; Rif; West Africa
语种	英语
来源期刊	Earth Science Reviews
文献类型	期刊论文
条目标识符	http://gcip.llas.ac.cn/handle/2XKMVOVA/203720
作者单位	CY Cergy Paris Université, Département Géosciences et Environnement (GEC), 1 rue DescartesNeuville/Oise Cedex 95000, France; Université Hassan II de Casablanca, Faculté des Sciences Ben M'sik, Département de Géologie, LGAGE, B, Casablanca, P 7955, Morocco; Università Roma Tre, Dipartimento di Scienze Geologiche, Largo San Leonardo Murialdo 1, Roma, 00146, Italy
推荐引用方式 GB/T 7714	Gimeno-Vives O.,de Lamotte D.F.,Leprêtre R.,et al. The structure of the Central-Eastern External Rif (Morocco); Poly-phased deformation and role of the under-thrusting of the North-West African paleo-margin[J],2020,205.
APA	Gimeno-Vives O.,de Lamotte D.F.,Leprêtre R.,Haissen F.,Atouabat A.,&Mohn G..(2020).The structure of the Central-Eastern External Rif (Morocco); Poly-phased deformation and role of the under-thrusting of the North-West African paleo-margin.Earth Science Reviews,205.
MLA	Gimeno-Vives O.,et al."The structure of the Central-Eastern External Rif (Morocco); Poly-phased deformation and role of the under-thrusting of the North-West African paleo-margin".Earth Science Reviews 205(2020).