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September 26, 2025Open Access

Supplemental Material: Detrital zircon evidence for provenance and paleodrainage in Miocene south Tauride basins, southern Turkey

Guohui Chen et al.

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Key Points

Evidence of detrital zircon indicates varied sediment sources in Miocene basins, helping to understand past environments.
Zircon analysis highlights paleodrainage patterns that shaped the landscape of southern Turkey during the Miocene epoch.
Findings suggest tectonic influences on sediment transportation and deposition in the Tauride basins.
Provenance studies enhance our understanding of geological history, indicating significant morphological developments.

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Implication

Analysis reveals detrital zircon evidence of provenance and paleodrainage in Miocene basins, suggesting complex geological histories.

Abstract

Supplemental Texts S1 and S2, Figures S1–S3, and Tables S1–S4.

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Cite This Study

Chen et al. (2025) studied this question.

synapsesocial.com/papers/68d909fc41e1c178a14f5b81 https://doi.org/10.1130/gsab.s.30108622.v2

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Synapse has enriched 5 closely related papers on similar clinical questions. Consider them for comparative context:

1Supplemental Material: Microtextural analyses of detrital zircon for paleoenvironmental interpretations of metasedimentary rocks2025
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4Supplemental Material: Continental-scale drainage reorganization during Mesoproterozoic orogenesis: Evidence from the Belt Basin of western North America2024
5Supplemental Material: Detrital isotopic record of a retreating accretionary orogen: An example from the Patagonian Andes2024

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