2021
DOI: 10.1002/essoar.10508546.1
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Sedimentary provenance from the evolving forearc-to-foreland Central Sakarya Basin, western Anatolia reveals multi-phase intercontinental collision

Abstract:  Multi-phase intercontinental collision is identified in western Anatolia by sedimentary basin changes  Sedimentary provenance change indicate collision was at 76 Ma, but significant thickskinned deformation was delayed until 54 Ma  The 20 Myr duration of initial collision can be explained by three multi-stage mechanisms involving changes in plate coupling manuscript submitted to Geochemistry, Geophysics, Geosystems

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Cited by 1 publication
(5 citation statements)
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“…(2018) and compared to detrital zircon maximum depositional ages from samples published by Mueller et al. (2019, 2022). To remain as objective as possible, we used a stochastic approach to calculating zircon maximum depositional ages based on a software provided by Keller et al.…”
Section: Hf Analytical Proceduresmentioning
confidence: 99%
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“…(2018) and compared to detrital zircon maximum depositional ages from samples published by Mueller et al. (2019, 2022). To remain as objective as possible, we used a stochastic approach to calculating zircon maximum depositional ages based on a software provided by Keller et al.…”
Section: Hf Analytical Proceduresmentioning
confidence: 99%
“…Closure of the ∼1,000 km wide İzmir‐Ankara Ocean in Western Anatolia (van Hinsbergen et al., 2016) was followed by collision between 80 and 60 Ma (e.g., Ballato et al., 2011; Cavazza et al., 2012; Gülyüz, 2020; Gülyüz et al., 2019; Mueller et al., 2022; Okay et al., 2020). At this juncture in the region's geodynamic evolution, both the single and double subduction zone models are more or less identical.…”
Section: Single Versus Double Subduction Modelsmentioning
confidence: 99%
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