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Geochemical insights, physico-mechanical properties and lithological enhancement using PRISMA hyperspectral data of intrusive rocks at Gabal Nikeiba area, South Eastern Desert, Egypt

Abdel-Rahman, Ahmed M.; Abuamarah, Bassam A. ; Shebl, Ali; Abdel Latif, Mahmoud L.; Drüppel, Kirsten 1; Azer, Mokhles K.
1 Institut für Angewandte Geowissenschaften (AGW), Karlsruher Institut für Technologie (KIT)

Abstract:

This study presents an integrated study of remote sensing, fieldwork, petrographic, geochemical analyses and geotechnical properties of intrusive rocks in the Nikeiba area, South-Eastern Desert, Egypt. Gabal Nikeiba area is composed of Neoproterozoic rocks, including island-arc
assemblages (mafic metavolcanics and metagabbro-diorite) and syn- (granodiorite and tonalite) to post-tectonic granitoids (syenogranite, alkali feldspar granite and quartz syenite), followed by post-granitic dikes of various compositions. PRISMA (PRecursore IperSpettrale della Missione Applicativa) hyperspectral data effectively delineated lithological units and structural features. The lithological discrimination serves as a spatial blueprint, ensuring that field sampling for geochemical analysis is optimized and geomechanical characterization is strategically targeted. The old magmatic phase is represented by a calc-alkaline series, typical of magmas formed in a subduction or continental collision setting. The post-collisional granites are subdivided into two magmatic phases, an older one including syenogranite and alkali feldspar granite, and a younger event includes quartz syenite. ... mehr


Verlagsausgabe §
DOI: 10.5445/IR/1000197687
Veröffentlicht am 09.10.2026
Cover der Publikation
Zugehörige Institution(en) am KIT Institut für Angewandte Geowissenschaften (AGW)
Publikationstyp Zeitschriftenaufsatz
Publikationsjahr 2026
Sprache Englisch
Identifikator ISSN: 0016-7568, 1469-5081
KITopen-ID: 1000197687
Erschienen in Geological Magazine
Verlag Cambridge University Press (CUP)
Band 163
Seiten e45
Vorab online veröffentlicht am 23.09.2026
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