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<p>The island of Donousa consists of a variegated metasedimentary sequence cut by arc-type granitoid dykes. Detrital zircon U–Pb ages and the presence of volcanic and ultramafic detritus suggest that the protoliths of the metasedimentary rocks were deposited in a Campanian forearc basin later than 76&#xa0;Ma. D1 stacking of the forearc deposits occurred at upper crustal levels (P<sub>max</sub> = 0.4&#xa0;GPa) with staurolite present as a stable phase. The subsequent isobaric heating led to growth of andalusite followed by D2 extension in the stability field of sillimanite, K-feldspar and high-quartz (<i>P</i> = 0.3 GPa, <i>T</i> = 660&#xa0;°C). Based on U–Pb ages of garnet (74.6 + 2.3/ − 2.5 Ma) and zircon (74.0 ± 0.8 Ma), separated from an early monzogranite dyke, the timing of forearc deposition, Buchan metamorphism, D2 extension and dyke emplacement is constrained to a maximum period of 2.6&#xa0;m.y. in the late Campanian. Cooling below T = ca. 600&#xa0;°C occurred during the Maastrichtian (71.3 + 0.6/ − 1.3&#xa0;Ma, U–Pb on titanite) and was followed by D3 folding under greenschist facies conditions. A younger generation of Danian granitoid dykes (64.1 + 0.9/ − 1.4&#xa0;Ma, U–Pb on titanite; 60 ± 4&#xa0;Ma, Rb–Sr on muscovite) intruded at higher structural levels and was associated with a pervasive fluid-assisted overprint. The sequence of forearc deposition, burying, Buchan metamorphism, extension, and igneous dyking within &lt; 2.6&#xa0;m.y. is strong evidence for fast (ca. 4&#xa0;cm a<sup>−1</sup>) trenchward arc retreat that was probably related to late Campanian subduction accretion and magmatic flare-up.</p> Graphical abstract <p></p>

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Fast arc retreat in the eastern Mediterranean: constraints from late Campanian forearc deposits (Donousa, Greece)

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  • 发表日期：

    2025年6月13日

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  • S. O. Martha,
  • P. Xypolias,
  • C. Cheng,
  • W. Dörr,
  • A. Gerdes,
  • D. C. Hezel,
  • M. Kutzschbach,
  • L. Millonig,
  • H. Schmeling,
  • H. R. Marschall,
  • W. Müller,
  • G. Zulauf

摘要

The island of Donousa consists of a variegated metasedimentary sequence cut by arc-type granitoid dykes. Detrital zircon U–Pb ages and the presence of volcanic and ultramafic detritus suggest that the protoliths of the metasedimentary rocks were deposited in a Campanian forearc basin later than 76 Ma. D1 stacking of the forearc deposits occurred at upper crustal levels (Pmax = 0.4 GPa) with staurolite present as a stable phase. The subsequent isobaric heating led to growth of andalusite followed by D2 extension in the stability field of sillimanite, K-feldspar and high-quartz (P = 0.3 GPa, T = 660 °C). Based on U–Pb ages of garnet (74.6 + 2.3/ − 2.5 Ma) and zircon (74.0 ± 0.8 Ma), separated from an early monzogranite dyke, the timing of forearc deposition, Buchan metamorphism, D2 extension and dyke emplacement is constrained to a maximum period of 2.6 m.y. in the late Campanian. Cooling below T = ca. 600 °C occurred during the Maastrichtian (71.3 + 0.6/ − 1.3 Ma, U–Pb on titanite) and was followed by D3 folding under greenschist facies conditions. A younger generation of Danian granitoid dykes (64.1 + 0.9/ − 1.4 Ma, U–Pb on titanite; 60 ± 4 Ma, Rb–Sr on muscovite) intruded at higher structural levels and was associated with a pervasive fluid-assisted overprint. The sequence of forearc deposition, burying, Buchan metamorphism, extension, and igneous dyking within < 2.6 m.y. is strong evidence for fast (ca. 4 cm a−1) trenchward arc retreat that was probably related to late Campanian subduction accretion and magmatic flare-up.

Graphical abstract