Post-Hercynian ultrahigh-temperature tectono-metamorphic evolution of the Middle Atlas lower crust (...
Post-Hercynian ultrahigh-temperature tectono-metamorphic evolution of the Middle Atlas lower crust (central Morocco) revealed by metapelitic granulite xenoliths
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Gottingen: Copernicus GmbH
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Language
English
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Publisher
Gottingen: Copernicus GmbH
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Scope and Contents
Contents
The study of metapelitic sillimanite- and garnet-bearing granulite xenoliths brought to the surface by the basanite of the 650 ka Tafraoute maar shed new light on the lower crust of the Tabular Middle Atlas (Morocco). Two main types of granulites are distinguished: (1) layered quartzo-feldspathic and (2) unlayered restitic. Mineralogy, petrology, P...
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Full title
Post-Hercynian ultrahigh-temperature tectono-metamorphic evolution of the Middle Atlas lower crust (central Morocco) revealed by metapelitic granulite xenoliths
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TN_cdi_doaj_primary_oai_doaj_org_article_2c47748b08f1412f83b55f0fd14c7b74
Permalink
https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_doaj_primary_oai_doaj_org_article_2c47748b08f1412f83b55f0fd14c7b74
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ISSN
1869-9529,1869-9510
E-ISSN
1869-9529
DOI
10.5194/se-16-1-2025