FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2064017554> ?p ?o ?g. }

• W2064017554 endingPage "38" @default.
• W2064017554 startingPage "21" @default.
• W2064017554 abstract "The Miocene volcanic rocks along the İzmir-Balıkesir Transfer Zone along the western margin of the Menderes Core Complex (MCC) in western Anatolian Volcanic Province (WAVP), where strike–slip deformation is dominant, comprise: (Group 1) early-middle Miocene high-K to shoshonitic rocks with high-Mg# and relatively low SiO2, (Group 2) middle Miocene phonolitic rocks with low-Mg# and intermediate SiO2, (Group 3) early-middle Miocene medium- to high-K series from andesites to rhyolites, (Group 4) middle Miocene rhyolites with distinct trace element compositions; and (Group 5) late Miocene high-MgO basalts, K-trachybasalts and (Group 6) late Miocene high-MgO basaltic andesites. The geochemical features of these rocks are comparable with the other Oligocene to Miocene volcanic rocks, but differ from the Eocene volcanic rocks in WAVP. The geochemical features of the most primitive early-middle Miocene Group 1 rocks indicate that they were derived from an anomalously metasomatized lithospheric mantle. The mineralogical and geochemical properties of garnet–amphibole peridotite from the Ulten Zone (UZP), Eastern Alps, which is thought to represent a fossil metasomatic mantle wedge contaminated by continental subduction, is similar to the model mantle composition previously proposed for the genesis of the mafic rocks. Together with the presence of Eocene to early Miocene continental subduction beneath the Aegean-west Anatolia region, this strongly suggests that continental subduction was an important factor in the genesis of the high-MgO shoshonitic to ultrapotassic volcanism in this post-collisional area. The origin of the Group 3 andesitic to rhyolitic rocks includes; (1) lower crustal melting, (2) mixing between lower crustally-derived and mantle-derived melts, and (3) FC-AFC processes. The late Miocene Group 5 and 6 rocks, however, derived from a more depleted mantle source, indicating that the mantle became depleted over time. The rhyolites of Group 4 are most probably crustally-derived. OIB-type Quaternary Kula volcanics (QKV) were emplaced near the centre of the MCC. Among the late Miocene basalts in the region, only the basalts located close to the QKV show transitional geochemistry between the Miocene volcanic rocks and QKV, indicating that asthenospheric contribution to lavas in the region occurred only near the centre of the MCC." @default.
• W2064017554 created "2016-06-24" @default.
• W2064017554 creator A5001368310 @default.
• W2064017554 creator A5020163715 @default.
• W2064017554 creator A5049115819 @default.
• W2064017554 creator A5062646834 @default.
• W2064017554 creator A5066610200 @default.
• W2064017554 creator A5072894480 @default.
• W2064017554 date "2012-10-01" @default.
• W2064017554 modified "2023-10-18" @default.
• W2064017554 title "Petrogenesis of the Miocene volcanism along the İzmir-Balıkesir Transfer Zone in western Anatolia, Turkey: Implications for origin and evolution of potassic volcanism in post-collisional areas" @default.
• W2064017554 cites W1556036204 @default.
• W2064017554 cites W1850526270 @default.
• W2064017554 cites W1877095307 @default.
• W2064017554 cites W1969030586 @default.
• W2064017554 cites W1969859799 @default.
• W2064017554 cites W1978456585 @default.
• W2064017554 cites W1978658483 @default.
• W2064017554 cites W1978809752 @default.
• W2064017554 cites W1980330690 @default.
• W2064017554 cites W1981685718 @default.
• W2064017554 cites W1997952954 @default.
• W2064017554 cites W1998004859 @default.
• W2064017554 cites W2002232892 @default.
• W2064017554 cites W2003279842 @default.
• W2064017554 cites W2005679595 @default.
• W2064017554 cites W2009900924 @default.
• W2064017554 cites W2011607179 @default.
• W2064017554 cites W2014482258 @default.
• W2064017554 cites W2018946474 @default.
• W2064017554 cites W2023216211 @default.
• W2064017554 cites W2023691463 @default.
• W2064017554 cites W2024888719 @default.
• W2064017554 cites W2029929222 @default.
• W2064017554 cites W2030145420 @default.
• W2064017554 cites W2030870291 @default.
• W2064017554 cites W2032912062 @default.
• W2064017554 cites W2038213437 @default.
• W2064017554 cites W2039781072 @default.
• W2064017554 cites W2042692134 @default.
• W2064017554 cites W2043433441 @default.
• W2064017554 cites W2045582465 @default.
• W2064017554 cites W2045594539 @default.
• W2064017554 cites W2049660991 @default.
• W2064017554 cites W2050189782 @default.
• W2064017554 cites W2052280670 @default.
• W2064017554 cites W2052473341 @default.
• W2064017554 cites W2060394838 @default.
• W2064017554 cites W2064373110 @default.
• W2064017554 cites W2065581078 @default.
• W2064017554 cites W2065850166 @default.
• W2064017554 cites W2067336738 @default.
• W2064017554 cites W2067875518 @default.
• W2064017554 cites W2072307823 @default.
• W2064017554 cites W2074324100 @default.
• W2064017554 cites W2076289118 @default.
• W2064017554 cites W2077810916 @default.
• W2064017554 cites W2078840355 @default.
• W2064017554 cites W2080380118 @default.
• W2064017554 cites W2081673195 @default.
• W2064017554 cites W2081865852 @default.
• W2064017554 cites W2087662765 @default.
• W2064017554 cites W2094857760 @default.
• W2064017554 cites W2095601024 @default.
• W2064017554 cites W2096663118 @default.
• W2064017554 cites W2096707152 @default.
• W2064017554 cites W2113349757 @default.
• W2064017554 cites W2119438235 @default.
• W2064017554 cites W2120577061 @default.
• W2064017554 cites W2121394503 @default.
• W2064017554 cites W2131973381 @default.
• W2064017554 cites W2132271592 @default.
• W2064017554 cites W2140149446 @default.
• W2064017554 cites W2143481796 @default.
• W2064017554 cites W2149517976 @default.
• W2064017554 cites W2149683715 @default.
• W2064017554 cites W2152928205 @default.
• W2064017554 cites W2155413836 @default.
• W2064017554 cites W2157184090 @default.
• W2064017554 cites W2169326720 @default.
• W2064017554 cites W2169673818 @default.
• W2064017554 cites W2317233249 @default.
• W2064017554 cites W2319930653 @default.
• W2064017554 cites W4242272598 @default.
• W2064017554 cites W845906037 @default.
• W2064017554 doi "https://doi.org/10.1016/j.jvolgeores.2012.05.022" @default.
• W2064017554 hasPublicationYear "2012" @default.
• W2064017554 type Work @default.
• W2064017554 sameAs 2064017554 @default.
• W2064017554 citedByCount "46" @default.
• W2064017554 countsByYear W20640175542013 @default.
• W2064017554 countsByYear W20640175542014 @default.
• W2064017554 countsByYear W20640175542015 @default.
• W2064017554 countsByYear W20640175542016 @default.
• W2064017554 countsByYear W20640175542017 @default.
• W2064017554 countsByYear W20640175542018 @default.
• W2064017554 countsByYear W20640175542019 @default.
• W2064017554 countsByYear W20640175542020 @default.

• next