Post-hercynian ultra-high temperature tectono-metamorphic evolution of the Middle Atlas lower crust...
Post-hercynian ultra-high temperature tectono-metamorphic evolution of the Middle Atlas lower crust (Central Morocco) revealed by metapelitic granulites xenoliths
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Publisher
European Geosciences Union
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Language
English
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European Geosciences Union
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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 ultra-high temperature tectono-metamorphic evolution of the Middle Atlas lower crust (Central Morocco) revealed by metapelitic granulites xenoliths
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TN_cdi_hal_primary_oai_HAL_hal_04752185v1
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https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_hal_primary_oai_HAL_hal_04752185v1
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ISSN
1869-9510
E-ISSN
1869-9529