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Abstract <p>The paper presents the reconstructed thermal history of the Slyudyanka crystalline complex, southern margin of the Siberian Craton, from the Late Ordovician to the Cenozoic. The reconstructions were done by using medium- and low-temperature thermochronology methods. The cooling stages of the rocks from the peak temperatures of granulite-facies metamorphism (~800°C in the Ordovician) to their exhumation to the surface in the Cenozoic, associated with the Baikal rifting, have been reconstructed.</p>

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Slyudyanka Crystalline Complex: From Ordovician Granulite-Facies Metamorphism to Late Cenozoic Exhumation

  • 期刊论文

  • 发表日期：

    2026年7月22日

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  • A. V. Ivanov,
  • E. A. Gladkochub,
  • L. P. Kasatkina,
  • L. Z. Reznitskii,
  • E. I. Demonterova,
  • N. V. Bryansky,
  • A. A. Karimov,
  • A. S. Maltsev,
  • K. G. Erofeeva,
  • A. S. Dubensky,
  • S. V. Malyshev

摘要

Abstract

The paper presents the reconstructed thermal history of the Slyudyanka crystalline complex, southern margin of the Siberian Craton, from the Late Ordovician to the Cenozoic. The reconstructions were done by using medium- and low-temperature thermochronology methods. The cooling stages of the rocks from the peak temperatures of granulite-facies metamorphism (~800°C in the Ordovician) to their exhumation to the surface in the Cenozoic, associated with the Baikal rifting, have been reconstructed.