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83:. The domain is split in two by the Middle Atlas fold belt. The Western Meseta has relatively little sedimentary cover and well-developed massifs, while the Eastern Meseta spanning the border with Algeria has numerous, small Paleozoic massifs. Continuing from the Neoproterozoic until the
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deposition and post-orogeny volcanism. Southern
Morocco was flooded by a massive shallow marine shelf, building up significant carbonates, mixed with continental sediments pouring in from inland areas now in the Sahara. In the
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sedimentary rocks. Forming
Morocco's Central Massif, the Meseta Domain completely conceals Precambrian rocks, although boreholes have found Neoproterozoic rocks in a Meseta
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153:"From rifting to Alpine inversion: Mesozoic and Cenozoic subsidence history of some Moroccan basins"
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The Meseta Domain, taking its name from Spain's Meseta
Central inner plateau, is an area of stable
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228:"Meseta Iberica: United Nations Educational, Scientific and Cultural Organization"
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This article is about a
Moroccan orogenic belt. For the geological feature, see
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rock that was never affected by the
Hercynian orogeny and was later covered by
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31:Structural map of Northern Morocco
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208:Food and Agriculture Organization
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200:"Inland fisheries of Europe"
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279:Mountain ranges of Morocco
257:Geological Atlas of Africa
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255:Schluter, Thomas (2006).
175:earthobservatory.nasa.gov
259:. Springer. p. 175.
51:rocks exposed along the
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20:. For other uses, see
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157:Sedimentary Geology
289:Geology of Morocco
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273:Categories
241:2019-12-11
213:2019-12-11
185:2019-12-11
139:References
49:Palaeozoic
81:anticline
69:Paleozoic
177:. U.S.:
77:Cenozoic
73:Mesozoic
53:Moroccan
284:Maghreb
63:Geology
45:terrane
236:UNESCO
89:redbed
22:Meseta
179:NASA
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