FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2169171804> ?p ?o ?g. }

• W2169171804 endingPage "299" @default.
• W2169171804 startingPage "283" @default.
• W2169171804 abstract "Abstract The Kızıldağ (Hatay) ophiolite in Turkey represents remnants of the southern Neotethyan ocean and is characterized by a complete ocean lithospheric section. It formed in a fore-arc setting above a N-dipping intraoceanic subduction zone, and represents the undeformed, more northerly part of the same thrust sheet that also forms the Baer–Bassit ophiolite to the south. The ophiolite was emplaced southwards from the southerly Neotethyan ocean in Maastrichtian time. U–Pb and Sm–Nd dates are used to constrain the crystallization age and duration of magmatic activity of the Kızıldağ ophiolite. U–Pb dating yielded ages of 91.7 ± 1.9 Ma for a plagiogranite and 91.6 ± 3.8 Ma for a cumulate gabbro. The cumulate gabbro also yielded a Sm–Nd isochron age of 95.3 ± 6.9 Ma. The measured ages suggest that the oceanic crust of the Kızıldağ ophiolite formed in a maximum time period of 6 Ma, and that the plagiogranite may have formed later than the gabbroic section. The U–Pb zircon ages from the Kızıldağ ophiolite and the cooling age of a metamorphic sole beneath the Baer–Bassit ophiolite are indistinguishable within the analytical uncertainties. This indicates the presence of young and hot oceanic lithosphere at the time of intraoceanic subduction/thrusting in the southern Neotethys. The U–Pb zircon ages from the Kızıldağ, the Troodos and the Semail ophiolites overlap within analytical uncertainties, suggesting that these ophiolites are contemporaneous and genetically and tectonically related within the same Late Cretaceous southern Neotethyan ocean." @default.
• W2169171804 created "2016-06-24" @default.
• W2169171804 creator A5000132936 @default.
• W2169171804 creator A5012276973 @default.
• W2169171804 creator A5067433260 @default.
• W2169171804 creator A5072089806 @default.
• W2169171804 creator A5089404412 @default.
• W2169171804 date "2012-10-23" @default.
• W2169171804 modified "2023-10-05" @default.
• W2169171804 title "U–Pb and Sm–Nd geochronology of the Kızıldağ (Hatay, Turkey) ophiolite: implications for the timing and duration of suprasubduction zone type oceanic crust formation in the southern Neotethys" @default.
• W2169171804 cites W105717235 @default.
• W2169171804 cites W1529124630 @default.
• W2169171804 cites W1963963600 @default.
• W2169171804 cites W1965596457 @default.
• W2169171804 cites W1965808859 @default.
• W2169171804 cites W1968053622 @default.
• W2169171804 cites W1969845853 @default.
• W2169171804 cites W1972401026 @default.
• W2169171804 cites W1972603973 @default.
• W2169171804 cites W1973051634 @default.
• W2169171804 cites W1974149250 @default.
• W2169171804 cites W1975368712 @default.
• W2169171804 cites W1978188291 @default.
• W2169171804 cites W1979170550 @default.
• W2169171804 cites W1980767624 @default.
• W2169171804 cites W1981145264 @default.
• W2169171804 cites W1986127271 @default.
• W2169171804 cites W1986786935 @default.
• W2169171804 cites W1988251519 @default.
• W2169171804 cites W1994181046 @default.
• W2169171804 cites W1994935654 @default.
• W2169171804 cites W2001146770 @default.
• W2169171804 cites W2004053289 @default.
• W2169171804 cites W2006550061 @default.
• W2169171804 cites W2008531647 @default.
• W2169171804 cites W2009280852 @default.
• W2169171804 cites W2009463051 @default.
• W2169171804 cites W2017840788 @default.
• W2169171804 cites W2027547935 @default.
• W2169171804 cites W2028764239 @default.
• W2169171804 cites W2028890485 @default.
• W2169171804 cites W2031295342 @default.
• W2169171804 cites W2036174339 @default.
• W2169171804 cites W2040605013 @default.
• W2169171804 cites W2043858545 @default.
• W2169171804 cites W2045594539 @default.
• W2169171804 cites W2045745603 @default.
• W2169171804 cites W2045778373 @default.
• W2169171804 cites W2047399789 @default.
• W2169171804 cites W2048539408 @default.
• W2169171804 cites W2050092460 @default.
• W2169171804 cites W2052455551 @default.
• W2169171804 cites W2061951984 @default.
• W2169171804 cites W2062055128 @default.
• W2169171804 cites W2065542151 @default.
• W2169171804 cites W2067897492 @default.
• W2169171804 cites W2068921463 @default.
• W2169171804 cites W2070287079 @default.
• W2169171804 cites W2070363219 @default.
• W2169171804 cites W2071520274 @default.
• W2169171804 cites W2076373269 @default.
• W2169171804 cites W2076927877 @default.
• W2169171804 cites W2079290545 @default.
• W2169171804 cites W2082524079 @default.
• W2169171804 cites W2083293993 @default.
• W2169171804 cites W2083912349 @default.
• W2169171804 cites W2086331051 @default.
• W2169171804 cites W2086977494 @default.
• W2169171804 cites W2090421737 @default.
• W2169171804 cites W2091654878 @default.
• W2169171804 cites W2093743417 @default.
• W2169171804 cites W2093786999 @default.
• W2169171804 cites W2094002101 @default.
• W2169171804 cites W2095788906 @default.
• W2169171804 cites W2096297752 @default.
• W2169171804 cites W2101934152 @default.
• W2169171804 cites W2104447927 @default.
• W2169171804 cites W2104959535 @default.
• W2169171804 cites W2106548275 @default.
• W2169171804 cites W2112329577 @default.
• W2169171804 cites W2124767937 @default.
• W2169171804 cites W2133308748 @default.
• W2169171804 cites W2133461735 @default.
• W2169171804 cites W2135651322 @default.
• W2169171804 cites W2137159697 @default.
• W2169171804 cites W2140054472 @default.
• W2169171804 cites W2147961046 @default.
• W2169171804 cites W2151792848 @default.
• W2169171804 cites W2153044652 @default.
• W2169171804 cites W2154745739 @default.
• W2169171804 cites W2160427881 @default.
• W2169171804 cites W2160856860 @default.
• W2169171804 cites W2161493148 @default.
• W2169171804 cites W2168482363 @default.
• W2169171804 cites W2169766597 @default.
• W2169171804 cites W2259645488 @default.
• W2169171804 cites W2299704767 @default.
• W2169171804 cites W2387543009 @default.

• next