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• W1966887645 abstract "Radiogenic isotope data (initial Nd, Pb) and elemental concentrations for the Mooselookmeguntic igneous complex, a suite of mainly granitic intrusions in New Hampshire and western Maine, are used to evaluate petrogenesis and crustal variations across a mid-Paleozoic suture zone. The complex comprises an areally subordinate monzodiorite suite [377±2 Ma; εNd (at 370 Ma)=−2.7 to −0.7; initial 207Pb/204Pb=15.56–15.58] and an areally dominant granite [370±2 Ma; εNd (at 370 Ma)=−7.0 to −0.6; initial 207Pb/204Pb=15.55–15.63]. The granite contains meter-scale enclaves of monzodiorite, petrographically similar to but older than that of the rest of the complex [389±2 Ma; εNd (at 370 Ma)=−2.6 to +0.3; initial 207Pb/204Pb ∼15.58, with one exception]. Other granite complexes in western Maine and New Hampshire are ∼30 Ma older than the Mooselookmeguntic igneous complex granite, but possess similar isotopic signatures. Derivation of the monzodioritic rocks of the Mooselookmeguntic igneous complex most likely occurred by melting of Bronson Hill belt crust of mafic to intermediate composition. The Mooselookmeguntic igneous complex granites show limited correlation of isotopic variations with elemental concentrations, precluding any significant presence of mafic source components. Given overlap of initial Nd and Pb isotopic compositions with data for Central Maine belt metasedimentary rocks, the isotopic heterogeneity of the granites may have been produced by melting of rocks in this crustal package or through a mixture of metasedimentary rocks with magmas derived from Bronson Hill belt crust. New data from other granites in western Maine include Pb isotope data for the Phillips pluton, which permit a previous interpretation that leucogranites were derived from melting heterogeneous metasedimentary rocks of the Central Maine belt, but suggest that granodiorites were extracted from sources more similar to Bronson Hill belt crust. Data for the Redington pluton are best satisfied by generation from sources in either the Bronson Hill belt or Laurentian basement. Based on these data, we infer that Bronson Hill belt crust was more extensive beneath the Central Maine belt than previously recognized and that mafic melts from the mantle were not important to genesis of Devonian granite magma." @default.
• W1966887645 created "2016-06-24" @default.
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• W1966887645 date "2005-03-01" @default.
• W1966887645 modified "2023-10-01" @default.
• W1966887645 title "Source contributions to Devonian granite magmatism near the Laurentian border, New Hampshire and Western Maine, USA" @default.
• W1966887645 cites W1482624593 @default.
• W1966887645 cites W1484019883 @default.
• W1966887645 cites W155872667 @default.
• W1966887645 cites W1640907558 @default.
• W1966887645 cites W1675648967 @default.
• W1966887645 cites W1679875884 @default.
• W1966887645 cites W1820659196 @default.
• W1966887645 cites W1964211524 @default.
• W1966887645 cites W1966191878 @default.
• W1966887645 cites W1969859799 @default.
• W1966887645 cites W1970621049 @default.
• W1966887645 cites W1973012528 @default.
• W1966887645 cites W1974912772 @default.
• W1966887645 cites W1977181360 @default.
• W1966887645 cites W1977795491 @default.
• W1966887645 cites W1987021146 @default.
• W1966887645 cites W1990728952 @default.
• W1966887645 cites W1993307882 @default.
• W1966887645 cites W1993810260 @default.
• W1966887645 cites W2003564352 @default.
• W1966887645 cites W2007105153 @default.
• W1966887645 cites W2011016972 @default.
• W1966887645 cites W2012161753 @default.
• W1966887645 cites W2014346120 @default.
• W1966887645 cites W2014473780 @default.
• W1966887645 cites W2014795256 @default.
• W1966887645 cites W2018376581 @default.
• W1966887645 cites W2019317659 @default.
• W1966887645 cites W2023563727 @default.
• W1966887645 cites W2025214997 @default.
• W1966887645 cites W2026408144 @default.
• W1966887645 cites W2030635509 @default.
• W1966887645 cites W2031794243 @default.
• W1966887645 cites W2032901453 @default.
• W1966887645 cites W2037090281 @default.
• W1966887645 cites W2037278837 @default.
• W1966887645 cites W2039704788 @default.
• W1966887645 cites W2044358950 @default.
• W1966887645 cites W2044490939 @default.
• W1966887645 cites W2045278405 @default.
• W1966887645 cites W2047383465 @default.
• W1966887645 cites W2048320205 @default.
• W1966887645 cites W2048990277 @default.
• W1966887645 cites W2054683576 @default.
• W1966887645 cites W2055770229 @default.
• W1966887645 cites W2061972658 @default.
• W1966887645 cites W2062761453 @default.
• W1966887645 cites W2063938104 @default.
• W1966887645 cites W2064675727 @default.
• W1966887645 cites W2065365058 @default.
• W1966887645 cites W2070031251 @default.
• W1966887645 cites W2073671350 @default.
• W1966887645 cites W2084682037 @default.
• W1966887645 cites W2085289476 @default.
• W1966887645 cites W2088341998 @default.
• W1966887645 cites W2089625409 @default.
• W1966887645 cites W2090475924 @default.
• W1966887645 cites W2091983134 @default.
• W1966887645 cites W2093845350 @default.
• W1966887645 cites W2120208585 @default.
• W1966887645 cites W2134502130 @default.
• W1966887645 cites W2138522501 @default.
• W1966887645 cites W2146559072 @default.
• W1966887645 cites W2148242120 @default.
• W1966887645 cites W2150455561 @default.
• W1966887645 cites W2156869463 @default.
• W1966887645 cites W2178842697 @default.
• W1966887645 cites W2307257090 @default.
• W1966887645 cites W2325119656 @default.
• W1966887645 cites W2493596588 @default.
• W1966887645 cites W3045930534 @default.
• W1966887645 cites W642057463 @default.
• W1966887645 cites W2036258406 @default.
• W1966887645 doi "https://doi.org/10.1016/j.lithos.2004.04.059" @default.
• W1966887645 hasPublicationYear "2005" @default.
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