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- W1529124630 endingPage "n/a" @default.
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- W1529124630 abstract "[1] The distribution of oceanic domains and continental blocks in Central Anatolia remains a challenge in understanding the Alpine geodynamic evolution of the Tethys realm. The consumption of a Neotethys oceanic branch at the Mesozoic-Cenozoic boundary welded the Central Anatolian Crystalline Complex in central Turkey and the Anatolide-Tauride Block in western Turkey, with the northerly Eurasian margin. Whether those two regions constituted a single or two distinct continental masses is still matter of debate. High-pressure metamorphism has been locally evidenced in the Afyon Zone, which was, however, defined as a greenschist-facies metamorphic zone of the Anatolide-Tauride Block. Since the Afyon Zone composes a metamorphic equivalent of a continental margin exposed far south of the Izmir-Ankara suture zone, this encouraged us to reevaluate its metamorphic evolution in order to better understand the relation between western and central Turkey. Our investigations reveal that the high-pressure minerals Fe-Mg-carpholite and glaucophane are present in the entire Afyon Zone, which we reconsider as a blueschist-facies zone. We additionally present a tectonic reconstruction, stripping off the postcollisional tectonics. It reveals that today's bending of the high-pressure belt is consistent with an Eocene collision of the Anatolide-Tauride Block around the southern edge of the Central Anatolian Crystalline Complex. We argue that the Central Anatolian Crystalline Complex and the Anatolide-Tauride Block were two distinct continental masses separated by a Neotethyan oceanic stripe, the closure of which engendered subduction-related metamorphism in the latter and arc volcanism and high-grade metamorphism in the former by late Cretaceous to early Cenozoic." @default.
- W1529124630 created "2016-06-24" @default.
- W1529124630 creator A5050392120 @default.
- W1529124630 creator A5060414536 @default.
- W1529124630 creator A5060595119 @default.
- W1529124630 date "2010-09-11" @default.
- W1529124630 modified "2023-10-12" @default.
- W1529124630 title "High-pressure metasediments in central Turkey: Constraints on the Neotethyan closure history" @default.
- W1529124630 cites W1522922852 @default.
- W1529124630 cites W1584132236 @default.
- W1529124630 cites W1699154488 @default.
- W1529124630 cites W1964577448 @default.
- W1529124630 cites W1966089798 @default.
- W1529124630 cites W1967001893 @default.
- W1529124630 cites W1970532431 @default.
- W1529124630 cites W1978035290 @default.
- W1529124630 cites W1978049764 @default.
- W1529124630 cites W1979170550 @default.
- W1529124630 cites W1980767624 @default.
- W1529124630 cites W1982067367 @default.
- W1529124630 cites W1982178948 @default.
- W1529124630 cites W1982798419 @default.
- W1529124630 cites W1985959295 @default.
- W1529124630 cites W1986043684 @default.
- W1529124630 cites W1990169490 @default.
- W1529124630 cites W1990305818 @default.
- W1529124630 cites W1992489808 @default.
- W1529124630 cites W1993774984 @default.
- W1529124630 cites W1993869433 @default.
- W1529124630 cites W1997952954 @default.
- W1529124630 cites W1998598291 @default.
- W1529124630 cites W1999345020 @default.
- W1529124630 cites W2001628667 @default.
- W1529124630 cites W2003419738 @default.
- W1529124630 cites W2005912563 @default.
- W1529124630 cites W2006456164 @default.
- W1529124630 cites W2007245030 @default.
- W1529124630 cites W2007700279 @default.
- W1529124630 cites W2008748306 @default.
- W1529124630 cites W2009280852 @default.
- W1529124630 cites W2015000352 @default.
- W1529124630 cites W2017319524 @default.
- W1529124630 cites W2019228988 @default.
- W1529124630 cites W2021273178 @default.
- W1529124630 cites W2022010553 @default.
- W1529124630 cites W2022061975 @default.
- W1529124630 cites W2023216211 @default.
- W1529124630 cites W2026699431 @default.
- W1529124630 cites W2028453174 @default.
- W1529124630 cites W2031295342 @default.
- W1529124630 cites W2033825289 @default.
- W1529124630 cites W2039280992 @default.
- W1529124630 cites W2040970457 @default.
- W1529124630 cites W2043278826 @default.
- W1529124630 cites W2043832610 @default.
- W1529124630 cites W2045594539 @default.
- W1529124630 cites W2045745603 @default.
- W1529124630 cites W2047753633 @default.
- W1529124630 cites W2055817459 @default.
- W1529124630 cites W2056851271 @default.
- W1529124630 cites W2063494096 @default.
- W1529124630 cites W2063764726 @default.
- W1529124630 cites W2063992088 @default.
- W1529124630 cites W2064936022 @default.
- W1529124630 cites W2066134875 @default.
- W1529124630 cites W2067566353 @default.
- W1529124630 cites W2068239574 @default.
- W1529124630 cites W2070588971 @default.
- W1529124630 cites W2074502277 @default.
- W1529124630 cites W2075151941 @default.
- W1529124630 cites W2076927877 @default.
- W1529124630 cites W2079891283 @default.
- W1529124630 cites W2081485548 @default.
- W1529124630 cites W2081615146 @default.
- W1529124630 cites W2082196654 @default.
- W1529124630 cites W2082856486 @default.
- W1529124630 cites W2086331051 @default.
- W1529124630 cites W2089068201 @default.
- W1529124630 cites W2089790038 @default.
- W1529124630 cites W2090741958 @default.
- W1529124630 cites W2091621247 @default.
- W1529124630 cites W2091879906 @default.
- W1529124630 cites W2094825907 @default.
- W1529124630 cites W2096168179 @default.
- W1529124630 cites W2096297752 @default.
- W1529124630 cites W2096482345 @default.
- W1529124630 cites W2098447346 @default.
- W1529124630 cites W2102182867 @default.
- W1529124630 cites W2104309567 @default.
- W1529124630 cites W2107080354 @default.
- W1529124630 cites W2109100268 @default.
- W1529124630 cites W2109321804 @default.
- W1529124630 cites W2115550380 @default.
- W1529124630 cites W2116918445 @default.
- W1529124630 cites W2117088195 @default.
- W1529124630 cites W2119531507 @default.
- W1529124630 cites W2123560443 @default.
- W1529124630 cites W2123794117 @default.