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• W2023684105 abstract "This study focuses on the East Serbian latest Cretaceous to Palaeocene Mafic Alkaline Rocks (hereafter, ES-MAR). This alkaline magmatism developed along the Eurasian border after the closure of the Mesozoic Tethys in the Balkan sector. Olivine(± clinopyroxene)-phyric and olivine- and nepheline-normative basanite, tephrite and theralite rocks are studied using Ar/Ar ages and major elements, trace elements and Sr–Nd–Pb isotopes. The ES-MAR are geochemically similar to other alkaline rocks of the Circum-Mediterranean Anorogenic Cenozoic Igneous (CiMACI) province, showing elevated contents of high field strength elements (HFSE) (e.g., Nb = 50–100 ppm) and high HFSE/LILE (large ion lithophile elements) ratios coupled with relatively low 87Sr/86Sri (mostly 0.7028–0.7040) and high 143Nd/144Ndi (mostly > 0.5127). In contrast to the majority of CiMACI rocks, the ES-MAR exhibit low 206Pb/204Pbi (< 18.5) ratios, similar to those displayed by Plio-Pleistocene volcanics of Sardinia. The Pb-unradiogenic signature of the ES-MAR is explained as the involvement of either an enriched mantle I-like source or highly depleted mantle. However, Sr–Nd–Pb and trace element variations (U/Nb, Ce/Pb, Th/Nb, and Th/La ratios and K2O and Th contents) suggest that mixing between an asthenospheric magma (similar to the average primitive CiMACI) and a lamproite-like melt also played a significant role in the ES-MAR petrogenesis. It is assumed that the lamproite-like magma originated by the melting of crustally modified lithosphere. A similar mantle is believed to be the source of primitive Serbian Oligocene lamproites. The model fails to explain the elevated K2O contents shown by samples that have low Th/Nb, Th/La and U/Nb and low Ce/Pb ratios. This subset of ES-MAR samples probably implies that there was an additional, presumably ‘anorogenic’ source of potassium." @default.
• W2023684105 created "2016-06-24" @default.
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• W2023684105 date "2013-11-01" @default.
• W2023684105 modified "2023-10-17" @default.
• W2023684105 title "An anorogenic pulse in a typical orogenic setting: The geochemical and geochronological record in the East Serbian latest Cretaceous to Palaeocene alkaline rocks" @default.
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• W2023684105 cites W1534749586 @default.
• W2023684105 cites W1544284413 @default.
• W2023684105 cites W1582044678 @default.
• W2023684105 cites W1877095307 @default.
• W2023684105 cites W1907935558 @default.
• W2023684105 cites W1914890451 @default.
• W2023684105 cites W1966653801 @default.
• W2023684105 cites W1967248360 @default.
• W2023684105 cites W1967390329 @default.
• W2023684105 cites W1968646608 @default.
• W2023684105 cites W1969859799 @default.
• W2023684105 cites W1974626411 @default.
• W2023684105 cites W1974767465 @default.
• W2023684105 cites W1978658483 @default.
• W2023684105 cites W1980544584 @default.
• W2023684105 cites W1980932812 @default.
• W2023684105 cites W1988369251 @default.
• W2023684105 cites W2006396228 @default.
• W2023684105 cites W2006510273 @default.
• W2023684105 cites W2008564598 @default.
• W2023684105 cites W2008584387 @default.
• W2023684105 cites W2009544440 @default.
• W2023684105 cites W2018282154 @default.
• W2023684105 cites W2018991138 @default.
• W2023684105 cites W2019920565 @default.
• W2023684105 cites W2020726550 @default.
• W2023684105 cites W2035044185 @default.
• W2023684105 cites W2035642076 @default.
• W2023684105 cites W2038600837 @default.
• W2023684105 cites W2039583716 @default.
• W2023684105 cites W2039616419 @default.
• W2023684105 cites W2041193569 @default.
• W2023684105 cites W2041627403 @default.
• W2023684105 cites W2045778373 @default.
• W2023684105 cites W2046735978 @default.
• W2023684105 cites W2047128953 @default.
• W2023684105 cites W2050651392 @default.
• W2023684105 cites W2051336362 @default.
• W2023684105 cites W2052504895 @default.
• W2023684105 cites W2055179278 @default.
• W2023684105 cites W2055812626 @default.
• W2023684105 cites W2057588685 @default.
• W2023684105 cites W2059933032 @default.
• W2023684105 cites W2060433213 @default.
• W2023684105 cites W2061405256 @default.
• W2023684105 cites W2063091092 @default.
• W2023684105 cites W2064414364 @default.
• W2023684105 cites W2065581078 @default.
• W2023684105 cites W2067512185 @default.
• W2023684105 cites W2067997488 @default.
• W2023684105 cites W2069663972 @default.
• W2023684105 cites W2079110505 @default.
• W2023684105 cites W2081865852 @default.
• W2023684105 cites W2082270291 @default.
• W2023684105 cites W2082962229 @default.
• W2023684105 cites W2083456023 @default.
• W2023684105 cites W2090448899 @default.
• W2023684105 cites W2090570612 @default.
• W2023684105 cites W2096663118 @default.
• W2023684105 cites W2100287838 @default.
• W2023684105 cites W2123536410 @default.
• W2023684105 cites W2126674782 @default.
• W2023684105 cites W2129909679 @default.
• W2023684105 cites W2135064030 @default.
• W2023684105 cites W2135251040 @default.
• W2023684105 cites W2140149446 @default.
• W2023684105 cites W2143863579 @default.
• W2023684105 cites W2145604970 @default.
• W2023684105 cites W2147184766 @default.
• W2023684105 cites W2154488736 @default.
• W2023684105 cites W2158261040 @default.
• W2023684105 cites W2162462477 @default.
• W2023684105 cites W2166626396 @default.
• W2023684105 cites W2171246880 @default.
• W2023684105 cites W2335340266 @default.
• W2023684105 cites W4245638129 @default.
• W2023684105 cites W4315748992 @default.
• W2023684105 doi "https://doi.org/10.1016/j.lithos.2013.08.013" @default.
• W2023684105 hasPublicationYear "2013" @default.
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