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- W2767393704 abstract "Outcrops of the Late Ordovician glacio-marine deposits in Tauride Anatolide Platform contain rare rounded/sub-rounded glacially transported granitic pebbles. Recently determined crystallization ages of the granitic fragments by LA-ICP-MS U-Pb zircon dating fall in two groups, 575 to 600 Ma and 700 to 965 Ma. Crystallization ages are in the range of juvenile magmatic rocks in the Arabian Nubian Shield except one sample implying pre-0.87 Ga magmatic activity. All dated granitic pebbles geochemically show arc-related compositions and juvenile isotopic systematics (whole rock ƐNd(T), Pb-Pb and zircon ƐHf(T) isotopic data). Marginal arc type sources fit well with the geochemical and isotopic data of the granitic pebbles of 700 and 800 Ma that have juvenile Hf-TDM and older Nd-TCR modal ages. However, A-type affinity of three samples, ranging from 575 to 600 Ma show that they might have been derived from mixing of juvenile mantle and older crustal sources having older Hf-TDM and Nd-TCR modal ages. A 965 Ma granitic fragment has the oldest Hf-TDM and Nd-TCR model age(s) implying involvement of pre-Neoproterozoic crustal source(s) in its genesis. These results collectively suggest that the glacio-marine successions in the Tauride Anatolide Platform were eroded from Neoproterozoic granitic/meta-granitic/meta-granodioritic rocks in the northern Nubian Shield (Egypt) and were then transported to the Tauride-Anatolide Platform by the glacial sheets during Late Ordovician time." @default.
- W2767393704 created "2017-11-17" @default.
- W2767393704 creator A5020826469 @default.
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- W2767393704 creator A5057709836 @default.
- W2767393704 creator A5060640853 @default.
- W2767393704 creator A5070748465 @default.
- W2767393704 creator A5078084168 @default.
- W2767393704 creator A5083229170 @default.
- W2767393704 date "2018-02-01" @default.
- W2767393704 modified "2023-10-16" @default.
- W2767393704 title "Nd, Pb, Hf isotope characteristics and provenance of glacial granitic pebbles from Late Ordovician diamictites in the Taurides, S Turkey" @default.
- W2767393704 cites W1183603216 @default.
- W2767393704 cites W1499677798 @default.
- W2767393704 cites W1578122124 @default.
- W2767393704 cites W1589729536 @default.
- W2767393704 cites W1949116197 @default.
- W2767393704 cites W1963592120 @default.
- W2767393704 cites W1964094851 @default.
- W2767393704 cites W1964591197 @default.
- W2767393704 cites W1964909252 @default.
- W2767393704 cites W1967307262 @default.
- W2767393704 cites W1970621049 @default.
- W2767393704 cites W1971376046 @default.
- W2767393704 cites W1972021591 @default.
- W2767393704 cites W1979473511 @default.
- W2767393704 cites W1980070520 @default.
- W2767393704 cites W1983330130 @default.
- W2767393704 cites W1984003364 @default.
- W2767393704 cites W1991076595 @default.
- W2767393704 cites W1992407057 @default.
- W2767393704 cites W1993090420 @default.
- W2767393704 cites W1995884346 @default.
- W2767393704 cites W1996303120 @default.
- W2767393704 cites W1997132358 @default.
- W2767393704 cites W1999473536 @default.
- W2767393704 cites W2000030712 @default.
- W2767393704 cites W2002898265 @default.
- W2767393704 cites W2003703699 @default.
- W2767393704 cites W2009295375 @default.
- W2767393704 cites W2016025369 @default.
- W2767393704 cites W2026704077 @default.
- W2767393704 cites W2027334351 @default.
- W2767393704 cites W2030009697 @default.
- W2767393704 cites W2031423471 @default.
- W2767393704 cites W2032401976 @default.
- W2767393704 cites W2033718063 @default.
- W2767393704 cites W2034345935 @default.
- W2767393704 cites W2035751836 @default.
- W2767393704 cites W2043043810 @default.
- W2767393704 cites W2043858545 @default.
- W2767393704 cites W2046688920 @default.
- W2767393704 cites W2048464517 @default.
- W2767393704 cites W2048857036 @default.
- W2767393704 cites W2051797790 @default.
- W2767393704 cites W2055274306 @default.
- W2767393704 cites W2056065853 @default.
- W2767393704 cites W2059198663 @default.
- W2767393704 cites W2063574742 @default.
- W2767393704 cites W2064300797 @default.
- W2767393704 cites W2064612127 @default.
- W2767393704 cites W2065369930 @default.
- W2767393704 cites W2067787424 @default.
- W2767393704 cites W2069615839 @default.
- W2767393704 cites W2076340378 @default.
- W2767393704 cites W2079472735 @default.
- W2767393704 cites W2079727754 @default.
- W2767393704 cites W2079855816 @default.
- W2767393704 cites W2082538997 @default.
- W2767393704 cites W2083110591 @default.
- W2767393704 cites W2085033737 @default.
- W2767393704 cites W2089609821 @default.
- W2767393704 cites W2091796504 @default.
- W2767393704 cites W2092901514 @default.
- W2767393704 cites W2094801005 @default.
- W2767393704 cites W2094876925 @default.
- W2767393704 cites W2094886494 @default.
- W2767393704 cites W2104121056 @default.
- W2767393704 cites W2117069434 @default.
- W2767393704 cites W2126029945 @default.
- W2767393704 cites W2142319922 @default.
- W2767393704 cites W2151118378 @default.
- W2767393704 cites W2151802570 @default.
- W2767393704 cites W2167933124 @default.
- W2767393704 cites W2168077883 @default.
- W2767393704 cites W2169334036 @default.
- W2767393704 cites W2169616158 @default.
- W2767393704 cites W2174216460 @default.
- W2767393704 cites W2238656530 @default.
- W2767393704 cites W2318056206 @default.
- W2767393704 cites W2342508973 @default.
- W2767393704 cites W2583478527 @default.
- W2767393704 cites W2974207299 @default.
- W2767393704 cites W2974796042 @default.
- W2767393704 cites W396911382 @default.
- W2767393704 cites W607831913 @default.
- W2767393704 doi "https://doi.org/10.1016/j.gr.2017.11.003" @default.
- W2767393704 hasPublicationYear "2018" @default.