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• W2082360769 abstract "Geochemical and Nd isotope data on granitoids of the NW part of the late Archaean eastern Dharwar craton are presented to elucidate their petrogenesis and role in crust formation. The granitoids are divided into three suites viz. trondhjemite–granodiorite gneisses, biotite monzogranites and porphyritic biotite granodiorites. The gneisses are pre- to syn-kinematic (with respect to deformation in the adjacent Hungund–Kushtagi schist belt), which show variable SiO2 and Al2O3, enriched LREE and depleted HREE with slightly negative to no Eu anomalies. They display unusual chemistry in having higher FeO(T), K2O, Ba, Cr and Ni compared to the typical Archaean tonalite–trondhjemite–granodiorite (TTG). The biotite monzogranites are mostly syn- to late-kinematic and exhibit evolved calc-alkaline compositions with high SiO2, K2O, LILE and LREE, depleted to undepleted HREE and strongly negative to no Eu anomalies. The porphyritic granodiorites show syn- to late-kinematic calc-alkaline, sanukitoid-like character with a wide range of SiO2, higher TiO2, P2O5, Sr, Ba, Cr and Ni, and lower Rb. They, however, uniquely display higher K2O, ΣREE and Th than typical sanukitoids. The trondhjemite–granodiorite gneisses are interpreted as product of melting of a subducted basaltic slab followed by slight contamination from the overlying metasomatized mantle wedge. Subsequent melting of the extremely metasomatized mantle wedge resulted in formation of the parental magma of the porphyritic granodiorites. Intrusion of the latter triggered melting of the TTG crust accreted earlier and generated the evolved monzogranites. The monzogranites occurring east of the Hungund–Kushtagi schist belt show higher εNd but lower TDM ages than those occurring to the west, indicating that terranes with different histories were juxtaposed by lateral accretion." @default.
• W2082360769 created "2016-06-24" @default.
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• W2082360769 date "2012-02-01" @default.
• W2082360769 modified "2023-10-02" @default.
• W2082360769 title "Geochemical and Nd isotope constraints on petrogenesis of granitoids from NW part of the eastern Dharwar craton: Possible implications for late Archaean crustal accretion" @default.
• W2082360769 cites W1560280583 @default.
• W2082360769 cites W1645393491 @default.
• W2082360769 cites W167668434 @default.
• W2082360769 cites W1827757642 @default.
• W2082360769 cites W1930746193 @default.
• W2082360769 cites W1970806264 @default.
• W2082360769 cites W1972607637 @default.
• W2082360769 cites W1977638370 @default.
• W2082360769 cites W1980644983 @default.
• W2082360769 cites W1985463078 @default.
• W2082360769 cites W1985485302 @default.
• W2082360769 cites W1986946192 @default.
• W2082360769 cites W1987799335 @default.
• W2082360769 cites W1988497895 @default.
• W2082360769 cites W1991730062 @default.
• W2082360769 cites W1994994114 @default.
• W2082360769 cites W2000970623 @default.
• W2082360769 cites W2002438874 @default.
• W2082360769 cites W2007774322 @default.
• W2082360769 cites W2009615347 @default.
• W2082360769 cites W2011065740 @default.
• W2082360769 cites W2018358440 @default.
• W2082360769 cites W2020324113 @default.
• W2082360769 cites W2022017333 @default.
• W2082360769 cites W2022267792 @default.
• W2082360769 cites W2027193326 @default.
• W2082360769 cites W2030316817 @default.
• W2082360769 cites W2032877876 @default.
• W2082360769 cites W2034222991 @default.
• W2082360769 cites W2034321273 @default.
• W2082360769 cites W2035670944 @default.
• W2082360769 cites W2037618727 @default.
• W2082360769 cites W2038660348 @default.
• W2082360769 cites W2040001309 @default.
• W2082360769 cites W2043407575 @default.
• W2082360769 cites W2043604832 @default.
• W2082360769 cites W2047151621 @default.
• W2082360769 cites W2048226315 @default.
• W2082360769 cites W2052839279 @default.
• W2082360769 cites W2053721096 @default.
• W2082360769 cites W2056501220 @default.
• W2082360769 cites W2056723788 @default.
• W2082360769 cites W2057366588 @default.
• W2082360769 cites W2058128109 @default.
• W2082360769 cites W2061525158 @default.
• W2082360769 cites W2066772738 @default.
• W2082360769 cites W2068692318 @default.
• W2082360769 cites W2070649406 @default.
• W2082360769 cites W2077084550 @default.
• W2082360769 cites W2080995558 @default.
• W2082360769 cites W2082582316 @default.
• W2082360769 cites W2085596423 @default.
• W2082360769 cites W2088816309 @default.
• W2082360769 cites W2092777475 @default.
• W2082360769 cites W2093377908 @default.
• W2082360769 cites W2093830186 @default.
• W2082360769 cites W2104162955 @default.
• W2082360769 cites W2113009765 @default.
• W2082360769 cites W2128624170 @default.
• W2082360769 cites W2140134802 @default.
• W2082360769 cites W2149787537 @default.
• W2082360769 cites W2155581823 @default.
• W2082360769 cites W2156661305 @default.
• W2082360769 cites W2167633604 @default.
• W2082360769 cites W2314378019 @default.
• W2082360769 cites W2332879341 @default.
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• W2082360769 doi "https://doi.org/10.1016/j.jseaes.2011.09.013" @default.
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