Late Cadomian rifting of the NW Gondwana margin and the reworking of Precambrian crust – evidence from bimodal magmatism in the early Paleozoic Moroccan Meseta-Reference-Cited by-同舟云学术

Late Cadomian rifting of the NW Gondwana margin and the reworking of Precambrian crust – evidence from bimodal magmatism in the early Paleozoic Moroccan Meseta

Published:2020-09-27 Issue:16 Volume:63 Page:2013-2036
ISSN:0020-6814
Container-title:International Geology Review
language:en
Short-container-title:International Geology Review

Author:

Ouabid Muhammad¹²^ORCID,Garrido Carlos J.¹,Ouali Houssa³,Harvey Jason⁴,Hidas Károly⁵,Marchesi Claudio¹⁶,Acosta-Vigil Antonio¹,Dautria Jean-Marie⁷,El Messbahi Hicham⁸,Román-Alpiste Manuel J.¹

Affiliation:

1. Instituto Andaluz De Ciencias De La Tierra (IACT), CSIC–UGR, Armilla, Granada, Spain

2. Geology & Sustainable Mining, Mohammed VI Polytechnic University, Benguerir, Morocco

3. Département De Géologie, Faculté Des Sciences, Université Moulay Ismail, Zitoune, Meknès, Morocco

4. School of Earth and Environment, University of Leeds, Leeds, UK

5. Departamento de Investigacióny Prospectiva Geocientífica, Instituto Geológico y Minero de España (IGME), Tres Cantos, Madrid, Spain

6. Dep. Mineralogía y Petrología, Facultad de Ciencias, Universidad de Granada, Granada, Spain

7. Géosciences Montpellier, Université de Montpellier–CNRS, Montpellier, France

8. Département de Géologie, Faculté Polydisciplinaire, Université Sidi Mohamed Ben Abdellah, Taza, Morocco

Publisher

Informa UK Limited

Subject

Geology

Link

https://www.tandfonline.com/doi/pdf/10.1080/00206814.2020.1818301

Reference132 articles.

1. Late Ediacaran syn-rift/post-rift transition and related fault-driven hydrothermal systems in the Anti-Atlas Mountains, Morocco

2. Diachronism in the late Neoproterozoic–Cambrian arc-rift transition of North Gondwana: A comparison of Morocco and the Iberian Ossa-Morena Zone

3. Neoproterozoic–Cambrian stratigraphic framework of the Anti-Atlas and Ouzellagh promontory (High Atlas), Morocco

4. Syn-rift unconformities punctuating the lower–middle Cambrian transition in the Atlas Rift, Morocco

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1. Evidence of a large igneous province at ca. 347–330 Ma along the northern Gondwana margin linked to the assembly of Pangea: Insights from U Pb zircon geochronology and geochemistry of the South-Western Branch of the Variscan Belt (Morocco);Earth-Science Reviews;2024-08

2. The tectonic significance of peri-Gondwanan Late Neoproterozoic-Early Palaeozoic felsic peraluminous magmatism;Earth-Science Reviews;2024-07

3. Integrating facies, mineralogy, and paleomagnetism to constrain the age and provenance of Paleozoic siliciclastic sedimentary rocks along the northern Gondwana margin: insights from the Araba and Naqus formations in western Gulf of Suez, Egypt;International Journal of Earth Sciences;2024-04-18

4. Provenance and source-to-sink of lower-middle Jurassic sediments from hinterland mounts to NW-Gondwana hyper-extended passive margin (Prerif sub-domain, External Rif, Morocco): First evidence from sedimentary petrology and detrital Zircon geochronology;Marine and Petroleum Geology;2023-11

5. Volcanic rocks from Amensif-Tnirt district in the Western High Atlas (Morocco): Geochemistry, magma features and new age dating;Journal of African Earth Sciences;2023-09