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dc.contributor.author |
Lamri, Mourad |
|
dc.contributor.author |
Bourefis, Ahcene |
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dc.date.accessioned |
2022-05-24T11:15:32Z |
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dc.date.available |
2022-05-24T11:15:32Z |
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dc.date.issued |
2017-06-15 |
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dc.identifier.uri |
http://depot.umc.edu.dz/handle/123456789/7454 |
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dc.description.abstract |
The region of Cap Bougaroun is part of the Kabylie of Collo. Structurally the massif of
Cape Bougaroun is integrated in the Maghrebian chain; it belongs to the internal domain and more precisely to the base Kabyle.
The tertiary magmatic complex of the Kabylie of Collo is exposed in a metamorphic and
sedimentary complex that participates in the formation of this structural edifice.
The granites occupy a large surface of outcropping which cover almost the whole massif
of Cape Bougaroun, it is the ""pericuminous granites with cordierite"". These granites are of a clear color, often porphyroids. The essential minerals are: quartz, potassium feldspar,
plagioclases, biotite, cordierite and muscovite. Tourmaline, zircon, apatite and ilmenite are
the accessory minerals. |
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dc.language.iso |
fr |
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dc.publisher |
Université Frères Mentouri - Constantine 1 |
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dc.subject |
complexe magmatique |
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dc.subject |
granites |
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dc.subject |
granites péralumineux à cordiérite |
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dc.title |
Etudes mineralogique et geochimique des granitoides de la region de Collo |
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dc.type |
Thesis |
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