C
Crispin Katongo
Researcher at University of Vienna
Publications - 5
Citations - 104
Crispin Katongo is an academic researcher from University of Vienna. The author has contributed to research in topics: Gneiss & Geochronology. The author has an hindex of 5, co-authored 5 publications receiving 89 citations. Previous affiliations of Crispin Katongo include University of Zambia.
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Journal ArticleDOI
Petrography, geochemistry, and geochronology of granitoid rocks in the Neoproterozoic-Paleozoic Lufilian-Zambezi belt, Zambia: Implications for tectonic setting and regional correlation
TL;DR: In this paper, the authors conducted petrographic and whole-rock chemical analyses of the Neoproterozoic Nchanga granite, Lusaka Granite, Ngoma Gneiss and felsic metavolcanic rocks from the Lufilian-Zambezi belt in Zambian, in order to evaluate their chemical characteristics and tectonic settings.
Journal ArticleDOI
Geochemistry, Geochronology and Isotopic Evolution of the Chewore–Rufunsa Terrane, Southern Irumide Belt: a Mesoproterozoic Continental Margin Arc
Simon P. Johnson,Bert De Waele,F. Tembo,Crispin Katongo,Kenichiro Tani,Qing Chang,Tsuyoshi Iizuka,Daniel J. Dunkley +7 more
TL;DR: The southern Irumide belt (SIB) is an ENE-WSW-trending, late Mesoproterozoic orogenic belt located between the Congo-Tanzania-Bangweulu (CTB) and Kalahari cratons in central southern Africa.
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Geochemistry and shock petrography of the Crow Creek Member, South Dakota, USA: Ejecta from the 74‐Ma Manson impact structure
TL;DR: In this paper, the authors used planar deformation features (PDFs) of shocked quartz from the 74-Ma Manson impact structure (MIS) to determine the bulk chemical compositions and analysis of planar deformations for the basal and marly units of the Crow Creek Member.
Book ChapterDOI
Occurrence and Origin of Scapolite in the Neoproterozoic Lufilian-Zambezi Belt, Zambia: Evidence/Role of Brine-Rich Fluid Infiltration During Regional Metamorphism
TL;DR: In this paper, the authors show that scapolite is an important mineral in the metamorphism of calc-silicates, marbles, amphibolites, and metagabbros in the Lufilian-Zambezi belt of Zambia.
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Remote sensing, field studies, petrography, and geochemistry of rocks in central Zambia: no evidence of a meteoritic impact in the area of the Lukanga Swamp
TL;DR: The Lukanga Swamp in central Zambia has previously been proposed as the site of a large (52 km diameter) impact structure on the basis of alleged observation of shock-diagnostic planar deformation features (PDFs) in quartz of breccia from the southern margin of the swamp as mentioned in this paper.