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Statements

Subject Item
n2:RIV%2F00216208%3A11310%2F11%3A10118652%21RIV12-MSM-11310___
rdf:type
n11:Vysledek skos:Concept
dcterms:description
Interpretation of airborne geophysical data integrated with field structural and lithological observation was successfully employed in the creation of the litho-structural framework in a poorly exposed Paleoproterozoic granite-greenstone terrain of the West African Craton. The geophysical data portray with sufficient detail all of the lithological units and structural features present. The results suggest that the granitoid domains are formed by numerous small to medium-sized plutons. The existence of several generations of magmatic episodes has a significant impact on the development of a regional tectonic model. The magnetic data provided a better definition of the actual pluton shapes and several highly magnetic late-orogenic plutons were reliably identified. Relic F1 fold hinges were recognized in the Hounde and Boromo greenstone belts. The D1 penetrative structures are generally affected by the D2 transcurrent shear zones, which often form as well the granite-greenstone belt boundaries. Previously unreported S2 shear zones including the Bossie shear zone, transecting the Sideradougou granitoid domain and abundant small-scale shear zones affecting all of the lithologies represent prospective areas for gold exploration. Airborne gamma-ray spectrometry data aided in the mapping process in areas with less regolith cover including erosional ridges and parts of the Banfora greenstone belt. The magnetic data revealed at least three generations of doleritic dykes crosscutting the western Burkina Faso. Interpretation of airborne geophysical data integrated with field structural and lithological observation was successfully employed in the creation of the litho-structural framework in a poorly exposed Paleoproterozoic granite-greenstone terrain of the West African Craton. The geophysical data portray with sufficient detail all of the lithological units and structural features present. The results suggest that the granitoid domains are formed by numerous small to medium-sized plutons. The existence of several generations of magmatic episodes has a significant impact on the development of a regional tectonic model. The magnetic data provided a better definition of the actual pluton shapes and several highly magnetic late-orogenic plutons were reliably identified. Relic F1 fold hinges were recognized in the Hounde and Boromo greenstone belts. The D1 penetrative structures are generally affected by the D2 transcurrent shear zones, which often form as well the granite-greenstone belt boundaries. Previously unreported S2 shear zones including the Bossie shear zone, transecting the Sideradougou granitoid domain and abundant small-scale shear zones affecting all of the lithologies represent prospective areas for gold exploration. Airborne gamma-ray spectrometry data aided in the mapping process in areas with less regolith cover including erosional ridges and parts of the Banfora greenstone belt. The magnetic data revealed at least three generations of doleritic dykes crosscutting the western Burkina Faso.
dcterms:title
A geophysically constrained litho-structural analysis of the Eburnean greenstone belts and associated granitoid domains, Burkina Faso, West Africa A geophysically constrained litho-structural analysis of the Eburnean greenstone belts and associated granitoid domains, Burkina Faso, West Africa
skos:prefLabel
A geophysically constrained litho-structural analysis of the Eburnean greenstone belts and associated granitoid domains, Burkina Faso, West Africa A geophysically constrained litho-structural analysis of the Eburnean greenstone belts and associated granitoid domains, Burkina Faso, West Africa
skos:notation
RIV/00216208:11310/11:10118652!RIV12-MSM-11310___
n11:predkladatel
n19:orjk%3A11310
n4:aktivita
n7:I
n4:aktivity
I
n4:cisloPeriodika
1-4
n4:dodaniDat
n5:2012
n4:domaciTvurceVysledku
n9:2832194
n4:druhVysledku
n8:J
n4:duvernostUdaju
n18:S
n4:entitaPredkladatele
n10:predkladatel
n4:idSjednocenehoVysledku
183828
n4:idVysledku
RIV/00216208:11310/11:10118652
n4:jazykVysledku
n15:eng
n4:klicovaSlova
structural analysis; remote sensing; airborne geophysics; paleoproterozoic; Burkina Faso; West Africa
n4:klicoveSlovo
n6:remote%20sensing n6:West%20Africa n6:paleoproterozoic n6:Burkina%20Faso n6:airborne%20geophysics n6:structural%20analysis
n4:kodStatuVydavatele
NL - Nizozemsko
n4:kontrolniKodProRIV
[2D59E29A3E4E]
n4:nazevZdroje
Precambrian Research
n4:obor
n14:DB
n4:pocetDomacichTvurcuVysledku
1
n4:pocetTvurcuVysledku
4
n4:rokUplatneniVysledku
n5:2011
n4:svazekPeriodika
190
n4:tvurceVysledku
Naba, Seta Metelka, Václav Jessell, Mark W. Baratoux, Lenka
n4:wos
000296209200004
s:issn
0301-9268
s:numberOfPages
22
n16:doi
10.1016/j.precamres.2011.08.002
n12:organizacniJednotka
11310