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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 (...

https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_doaj_primary_oai_doaj_org_article_2c47748b08f1412f83b55f0fd14c7b74

Post-Hercynian ultrahigh-temperature tectono-metamorphic evolution of the Middle Atlas lower crust (central Morocco) revealed by metapelitic granulite xenoliths

About this item

Full title

Post-Hercynian ultrahigh-temperature tectono-metamorphic evolution of the Middle Atlas lower crust (central Morocco) revealed by metapelitic granulite xenoliths

Publisher

Gottingen: Copernicus GmbH

Journal title

Solid earth (Göttingen), 2025-01, Vol.16 (1), p.1-22

Language

English

Formats

Publication information

Publisher

Gottingen: Copernicus GmbH

More information

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...

Alternative Titles

Full title

Post-Hercynian ultrahigh-temperature tectono-metamorphic evolution of the Middle Atlas lower crust (central Morocco) revealed by metapelitic granulite xenoliths

Authors, Artists and Contributors

Identifiers

Primary Identifiers

Record Identifier

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

Other Identifiers

ISSN

1869-9529,1869-9510

E-ISSN

1869-9529

DOI

10.5194/se-16-1-2025

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