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Cited by 6 publications
(11 citation statements)
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“…In Turkey, Ar–Ar isotopic ages of the metamorphic soles of the Lycian peridotites are mainly 92−90 Ma (Dilek et al 1999), an age range that is similar to the K–Ar isotopic ages on Karpathos. More recently, U–Pb ages on zircons from the metamorphic sole of the Marmaris ophiolite (Lycian Nappes) have shown that their tectonic emplacement occurred between 100.4 Ma and 93.5 Ma (Cenomanian), suggesting an Early Cretaceous age for the ophiolite and the associated sedimentary rocks (Güngör et al 2018). Unfortunately, previous geochronological studies carried out on Karpathos (Koepke et al 1985; Hatzipanagiotou, 1991; Koepke et al 2002) did not document the precise locations for the K–Ar samples or indicate whether the magmatic rocks were overlain by sedimentary strata, preventing comparative sampling of sections.…”
Section: Discussionmentioning
confidence: 99%
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“…In Turkey, Ar–Ar isotopic ages of the metamorphic soles of the Lycian peridotites are mainly 92−90 Ma (Dilek et al 1999), an age range that is similar to the K–Ar isotopic ages on Karpathos. More recently, U–Pb ages on zircons from the metamorphic sole of the Marmaris ophiolite (Lycian Nappes) have shown that their tectonic emplacement occurred between 100.4 Ma and 93.5 Ma (Cenomanian), suggesting an Early Cretaceous age for the ophiolite and the associated sedimentary rocks (Güngör et al 2018). Unfortunately, previous geochronological studies carried out on Karpathos (Koepke et al 1985; Hatzipanagiotou, 1991; Koepke et al 2002) did not document the precise locations for the K–Ar samples or indicate whether the magmatic rocks were overlain by sedimentary strata, preventing comparative sampling of sections.…”
Section: Discussionmentioning
confidence: 99%
“…Isotopic ages, Crete: Koepke et al (2002); Liati et al (2004); Karpathos and Rhodes: Koepke, Seidel & Kreuzer (2002). SW Turkey: Dilek et al (1999); Güngör et al (2018) (see references for age ranges, error margins and local distribution). Age of radiolarites, Turkey: Danelian et al (2006); Karpathos: this study.…”
Section: Eastern Mediterranean Correlations and Implications For Neotmentioning
confidence: 99%
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“…From there, east-dipping (in the west) and west-dipping (in the east) subduction segments followed the saw-toothed shape of the Greater Adriatic and Arabian continental margins (Fig. 1C) and initiated close to it: rocks of these margins already underthrusted the ophiolites within 5-15 My after SSZ ophiolite spreading 14,23,24 , and continent-derived zircons have been found in metamorphic sole rocks 25 .…”
Section: Geological Reconstruction Of Plate Boundary Formation Acrossmentioning
confidence: 96%
“…From there, east-dipping (in the west) and west-dipping (in the east) subduction segments followed the saw-toothed shape of the Greater Adriatic and Arabian continental margins (Fig. 1C) and initiated close to it: rocks of these continental margins already underthrusted the ophiolites within 5-15 My after SSZ ophiolite spreading 14,23,24 , and continent-derived zircons have been found in metamorphic sole rocks 25 . Subduction segments likely nucleated along ancient N-S and NE-SW trending fracture zones and linked through highly oblique, north-dipping subduction zones that trended parallel to and likely reactivated the pre-existing (hyper)extended passive margins (Fig.…”
Section: Geological Reconstruction Of Incipient Plate Boundarymentioning
confidence: 96%