Mauritanide Belt

E779350

The Mauritanide Belt is a major Paleozoic-age mountain belt in West Africa formed by the collision of continental plates along the western margin of the West African Craton.

Try in SPARQL Jump to: Statements Referenced by

Statements (37)

Predicate Object
instanceOf geological region
orogenic belt
adjacentTo Sahara Desert NERFINISHED
boundedBy West African Craton to the east
continent Africa
country Guinea NERFINISHED
Guinea-Bissau NERFINISHED
Liberia
Mauritania NERFINISHED
Senegal NERFINISHED
Sierra Leone NERFINISHED
The Gambia NERFINISHED
deformationStyle fold-and-thrust belt
economicGeology gold occurrences
mineralization in iron ore
extendsAlong Atlantic margin of West Africa
formedBy continental collision
geodynamicContext Gondwana margin orogen NERFINISHED
geologicalAge Paleozoic NERFINISHED
lithology granitoid intrusions
metasedimentary rocks
metavolcanic rocks
locatedIn West Africa NERFINISHED
locatedOn western margin of the West African Craton
metamorphicGrade low- to medium-grade metamorphism
namedAfter Mauritania NERFINISHED
orogeny Mauritanide orogeny NERFINISHED
parallelTo present Atlantic coastline of West Africa
relatedTo opening of the Central Atlantic Ocean
researchField economic geology
structural geology
tectonics
separates West African Craton from the Atlantic margin
structuralTrend north–south
tectonicPhase Variscan-related deformation
tectonicSetting convergent plate margin
timeOfMainDeformation Late Paleozoic

Referenced by (1)

Full triples — surface form annotated when it differs from this entity's canonical label.

West African Craton boundedBy Mauritanide Belt