Permian volcanism of the Khenifra Massif (Central Morocco) Petrography and geochemical affinity

Abstract The Permian volcanic complex of Khenifra (Moroccan Central Hercynian Massif) manifests itself mainly by volcanic rocks of andesite, rhyolite, dacite, rhyodacite, ignimbrite and trachyte nature. These are rocks with a microlitic to porphyritic texture. They are formed by a primary paragenesi...

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Published inIOP conference series. Earth and environmental science Vol. 1090; no. 1; pp. 12010 - 12021
Main Authors Boutsougame, A, Ouazzani, H, Abba, E H, Alaoui, M
Format Journal Article
LanguageEnglish
Published Bristol IOP Publishing 01.10.2022
Subjects
Affinity
Andesite
Biotite
Calcite
Geochemical affinity
Khenifra
Massifs
Moroccan Central Hercynian Massif
Olivine
Permian
Permian Volcanism
Petrography
Plagioclase
Rhyolite
Rocks
Trachyte
Volcanic activity
Volcanic rocks
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Abstract Abstract The Permian volcanic complex of Khenifra (Moroccan Central Hercynian Massif) manifests itself mainly by volcanic rocks of andesite, rhyolite, dacite, rhyodacite, ignimbrite and trachyte nature. These are rocks with a microlitic to porphyritic texture. They are formed by a primary paragenesis made of plagioclase, pyroxene, olivine, feldspar, biotite, amphibole and quartz and a secondary mineral association made of augite, calcite, chlorite and opaque. Intermediate and acidic rocks are widely represented in Khenifra basin. These facies are of calco-alkaline affinity.
AbstractList The Permian volcanic complex of Khenifra (Moroccan Central Hercynian Massif) manifests itself mainly by volcanic rocks of andesite, rhyolite, dacite, rhyodacite, ignimbrite and trachyte nature. These are rocks with a microlitic to porphyritic texture. They are formed by a primary paragenesis made of plagioclase, pyroxene, olivine, feldspar, biotite, amphibole and quartz and a secondary mineral association made of augite, calcite, chlorite and opaque. Intermediate and acidic rocks are widely represented in Khenifra basin. These facies are of calco-alkaline affinity.
Abstract The Permian volcanic complex of Khenifra (Moroccan Central Hercynian Massif) manifests itself mainly by volcanic rocks of andesite, rhyolite, dacite, rhyodacite, ignimbrite and trachyte nature. These are rocks with a microlitic to porphyritic texture. They are formed by a primary paragenesis made of plagioclase, pyroxene, olivine, feldspar, biotite, amphibole and quartz and a secondary mineral association made of augite, calcite, chlorite and opaque. Intermediate and acidic rocks are widely represented in Khenifra basin. These facies are of calco-alkaline affinity.
Author Alaoui, M
Ouazzani, H
Abba, E H
Boutsougame, A
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  surname: Boutsougame
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  organization: Higher School of Technology- Khénifra -, . Morocco
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  surname: Ouazzani
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  organization: Faculty of Sciences Meknes, Department of Geology , . Morocco
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  organization: Sciences and Technologies Faculty of Sultan Moulay Slimane University , . Morocco
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Cites_doi 10.1080/09853111.1995.11105387
10.2475/ajs.274.4.321
10.1093/petrology/27.3.745
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Snippet Abstract The Permian volcanic complex of Khenifra (Moroccan Central Hercynian Massif) manifests itself mainly by volcanic rocks of andesite, rhyolite, dacite,...
The Permian volcanic complex of Khenifra (Moroccan Central Hercynian Massif) manifests itself mainly by volcanic rocks of andesite, rhyolite, dacite,...
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SubjectTerms Affinity
Andesite
Biotite
Calcite
Geochemical affinity
Khenifra
Massifs
Moroccan Central Hercynian Massif
Olivine
Permian
Permian Volcanism
Petrography
Plagioclase
Rhyolite
Rocks
Trachyte
Volcanic activity
Volcanic rocks
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Title Permian volcanism of the Khenifra Massif (Central Morocco) Petrography and geochemical affinity
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