Geology, structure, geochemistry and ASTER-based mapping of Neoproterozoic Gebel El-Delihimmi granites, Central Eastern Desert of Egypt

The Gebel El-Delihimmi granite intrusion, located in the Central Eastern Desert of Egypt, cuts the core of a major anticlinal structure of calc-alkaline metavolcanics and ophiolitic mélange rocks. The intrusion is microscopically differentiated into granodiorite, monzogranite, syenogranite and alkal...

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Published inLithos Vol. 282-283; pp. 358 - 372
Main Authors Asran, Asran Mohamed, Emam, Ashraf, El-Fakharani, Abdelhamid
Format Journal Article
LanguageEnglish
Published Elsevier B.V 01.06.2017
Subjects
ASTER-SWIR
Central Eastern Desert
Deformation
El-Delihimmi
I-type granites
Deformation
Central Eastern Desert
I-type granites
El-Delihimmi
ASTER-SWIR
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Abstract The Gebel El-Delihimmi granite intrusion, located in the Central Eastern Desert of Egypt, cuts the core of a major anticlinal structure of calc-alkaline metavolcanics and ophiolitic mélange rocks. The intrusion is microscopically differentiated into granodiorite, monzogranite, syenogranite and alkali-feldspar granite. Decorrelation stretch and band-ratio techniques were applied to Advanced Spaceborne Thermal Emission and Reflection Radiometer data. Processing of ASTER-SWIR bands enabled discrimination of El-Delihimmi granite phases and generation of a detailed lithologic map of the study area. The structural and microfabric data suggest that the El-Delihimmi granite underwent at least two phases of deformations. The first was related to the Najd fault system during which the older granodiorite phase of the intrusion was affected by sinistral ductile shearing. During the second phase, monzogranite and syenogranite in the intrusion were affected by brittle E–W compressional deformation. Geochemical data reported here reveal that the granodiorite phase has K2O/Na2O ratio <1 and represents an evolved calc-alkaline granite. The monzogranite, syenogranite and alkali-feldspar granite phases have K2O/Na2O ratio >1. The granite phases are generally I-type, metaluminous to slightly peraluminous and are interpreted as formed above subducted slabs of oceanic lithosphere rather than in continental collision zones. [Display omitted] •SWIR-ASTER data processing led to create a detailed geological map of El-Delihimmi granite area.•Gebel El-Delihimmi granites are granodiorite, monzogranite, syenogranite and alkali-feldspar granite.•Granodiorite was affected by ductile shearing, while monzogranite and syenogranite were affected by brittle deformation.•El-Delihimmi granites could be pertaining to well-known uraniferous granites in Egypt.•Gebel El-Delihimmi granites are comparable with monzogranite-association of Central Hijaz region, Arabian shield.
AbstractList The Gebel El-Delihimmi granite intrusion, located in the Central Eastern Desert of Egypt, cuts the core of a major anticlinal structure of calc-alkaline metavolcanics and ophiolitic mélange rocks. The intrusion is microscopically differentiated into granodiorite, monzogranite, syenogranite and alkali-feldspar granite. Decorrelation stretch and band-ratio techniques were applied to Advanced Spaceborne Thermal Emission and Reflection Radiometer data. Processing of ASTER-SWIR bands enabled discrimination of El-Delihimmi granite phases and generation of a detailed lithologic map of the study area. The structural and microfabric data suggest that the El-Delihimmi granite underwent at least two phases of deformations. The first was related to the Najd fault system during which the older granodiorite phase of the intrusion was affected by sinistral ductile shearing. During the second phase, monzogranite and syenogranite in the intrusion were affected by brittle E–W compressional deformation. Geochemical data reported here reveal that the granodiorite phase has K2O/Na2O ratio <1 and represents an evolved calc-alkaline granite. The monzogranite, syenogranite and alkali-feldspar granite phases have K2O/Na2O ratio >1. The granite phases are generally I-type, metaluminous to slightly peraluminous and are interpreted as formed above subducted slabs of oceanic lithosphere rather than in continental collision zones. [Display omitted] •SWIR-ASTER data processing led to create a detailed geological map of El-Delihimmi granite area.•Gebel El-Delihimmi granites are granodiorite, monzogranite, syenogranite and alkali-feldspar granite.•Granodiorite was affected by ductile shearing, while monzogranite and syenogranite were affected by brittle deformation.•El-Delihimmi granites could be pertaining to well-known uraniferous granites in Egypt.•Gebel El-Delihimmi granites are comparable with monzogranite-association of Central Hijaz region, Arabian shield.
Author Asran, Asran Mohamed
El-Fakharani, Abdelhamid
Emam, Ashraf
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Central Eastern Desert
I-type granites
El-Delihimmi
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Snippet The Gebel El-Delihimmi granite intrusion, located in the Central Eastern Desert of Egypt, cuts the core of a major anticlinal structure of calc-alkaline...
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StartPage 358
SubjectTerms ASTER-SWIR
Central Eastern Desert
Deformation
El-Delihimmi
I-type granites
Title Geology, structure, geochemistry and ASTER-based mapping of Neoproterozoic Gebel El-Delihimmi granites, Central Eastern Desert of Egypt
URI https://dx.doi.org/10.1016/j.lithos.2017.03.022
Volume 282-283
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