FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W4296578032> ?p ?o ?g. }

• W4296578032 endingPage "104731" @default.
• W4296578032 startingPage "104731" @default.
• W4296578032 abstract "At the northern border of the West African Craton (WAC), the Saghro massif of the Moroccan Anti-Atlas belt is renowned for its tectonic complexity inherited from Pan-African, Variscan, and Alpine orogenic cycles. This makes it an ideal area to investigate the tectonic evolution of the northern fringe of the WAC from Precambrian to present times. In this study, remote sensing structural mapping and extensive field observations and measurements have been integrated to decipher the tectonic style and fault kinematic history in the Precambrian-Cambrian and Cenozoic outcrops of the southwestern Saghro massif. The structural analysis shows three fault systems, namely N–S to NNE-SSW, NE-SW to E-W, and NNW-SSE to NW-SE. Extensive and transpressive/compressive tectonics reactivated the NE to ENE major faults, while most of the NW-SE pan-African structures are tectonically aborted. This fault pattern played a major role in the thick-skinned Variscan tectonics of the area and the origin of the present-day reliefs of the Saghro massif. The thin-skinned deformation style characterizes the superimposed Ouarzazate foreland basin, accommodated by deep detachment faults and fault-propagation folds favored by multiple post-Variscan incompetent levels. The increased fracture frequency with increasing rock strength and deformation intensity has a significant implication in the fault distribution over the basement and cover outcrops. The resulting structural map allows the revision and updating of existing geological maps and helps to understand the tectonic correlations between the southern orogenic border of the High Atlas and the Anti-Atlas fold and thrust belt." @default.
• W4296578032 created "2022-09-22" @default.
• W4296578032 creator A5009656089 @default.
• W4296578032 creator A5029588716 @default.
• W4296578032 creator A5035715531 @default.
• W4296578032 creator A5036728925 @default.
• W4296578032 creator A5045483994 @default.
• W4296578032 creator A5069158674 @default.
• W4296578032 creator A5088645785 @default.
• W4296578032 date "2022-12-01" @default.
• W4296578032 modified "2023-10-16" @default.
• W4296578032 title "Polyphase tectonics, fault kinematics and metallogenic implications at the fringe of a craton (Anti-Atlas, Morocco)" @default.
• W4296578032 cites W1967490232 @default.
• W4296578032 cites W1967597677 @default.
• W4296578032 cites W1968849391 @default.
• W4296578032 cites W1973871913 @default.
• W4296578032 cites W1974531849 @default.
• W4296578032 cites W1979240913 @default.
• W4296578032 cites W1979982652 @default.
• W4296578032 cites W1984421070 @default.
• W4296578032 cites W1985876329 @default.
• W4296578032 cites W1991034974 @default.
• W4296578032 cites W1994261648 @default.
• W4296578032 cites W2000845802 @default.
• W4296578032 cites W2003410124 @default.
• W4296578032 cites W2018188298 @default.
• W4296578032 cites W2021254835 @default.
• W4296578032 cites W2026384151 @default.
• W4296578032 cites W2028217178 @default.
• W4296578032 cites W2029014434 @default.
• W4296578032 cites W2035717954 @default.
• W4296578032 cites W2036622817 @default.
• W4296578032 cites W2037313001 @default.
• W4296578032 cites W2038771710 @default.
• W4296578032 cites W2039421626 @default.
• W4296578032 cites W2047097742 @default.
• W4296578032 cites W2050959825 @default.
• W4296578032 cites W2054099812 @default.
• W4296578032 cites W2058399625 @default.
• W4296578032 cites W2059762112 @default.
• W4296578032 cites W2059964545 @default.
• W4296578032 cites W2065806869 @default.
• W4296578032 cites W2068582210 @default.
• W4296578032 cites W2078622163 @default.
• W4296578032 cites W2081806262 @default.
• W4296578032 cites W2084347945 @default.
• W4296578032 cites W2086558702 @default.
• W4296578032 cites W2087333066 @default.
• W4296578032 cites W2089808263 @default.
• W4296578032 cites W2094616558 @default.
• W4296578032 cites W2109934455 @default.
• W4296578032 cites W2110496782 @default.
• W4296578032 cites W2115135275 @default.
• W4296578032 cites W2127752167 @default.
• W4296578032 cites W2136625467 @default.
• W4296578032 cites W2152848429 @default.
• W4296578032 cites W2338342104 @default.
• W4296578032 cites W2496066723 @default.
• W4296578032 cites W2509610480 @default.
• W4296578032 cites W2538645831 @default.
• W4296578032 cites W2550787127 @default.
• W4296578032 cites W2594846742 @default.
• W4296578032 cites W2605799627 @default.
• W4296578032 cites W2771186497 @default.
• W4296578032 cites W2792186536 @default.
• W4296578032 cites W2886114347 @default.
• W4296578032 cites W2903832244 @default.
• W4296578032 cites W2967959965 @default.
• W4296578032 cites W2982878616 @default.
• W4296578032 cites W3000245380 @default.
• W4296578032 cites W3007584159 @default.
• W4296578032 cites W3007821725 @default.
• W4296578032 cites W3011006757 @default.
• W4296578032 cites W3027402360 @default.
• W4296578032 cites W3168813988 @default.
• W4296578032 cites W346585641 @default.
• W4296578032 cites W4210275159 @default.
• W4296578032 cites W4253600674 @default.
• W4296578032 cites W4291278420 @default.
• W4296578032 doi "https://doi.org/10.1016/j.jafrearsci.2022.104731" @default.
• W4296578032 hasPublicationYear "2022" @default.
• W4296578032 type Work @default.
• W4296578032 citedByCount "3" @default.
• W4296578032 countsByYear W42965780322022 @default.
• W4296578032 countsByYear W42965780322023 @default.
• W4296578032 crossrefType "journal-article" @default.
• W4296578032 hasAuthorship W4296578032A5009656089 @default.
• W4296578032 hasAuthorship W4296578032A5029588716 @default.
• W4296578032 hasAuthorship W4296578032A5035715531 @default.
• W4296578032 hasAuthorship W4296578032A5036728925 @default.
• W4296578032 hasAuthorship W4296578032A5045483994 @default.
• W4296578032 hasAuthorship W4296578032A5069158674 @default.
• W4296578032 hasAuthorship W4296578032A5088645785 @default.
• W4296578032 hasConcept C105492442 @default.
• W4296578032 hasConcept C127313418 @default.
• W4296578032 hasConcept C127413603 @default.
• W4296578032 hasConcept C147717901 @default.
• W4296578032 hasConcept C151730666 @default.

• next