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Lab team

The Laboratory of Fission-Track Analysis and Isotope Geochronology was established in 2024 as a structural subdivision of the Schmidt Institute of Physics of the Earth of the Russian Academy of Sciences (IPE RAS). Our Laboratory realizes the full cycle of Apatite and Zircon Fission-Track analysis/dating (AFT, ZFT), as well as U-Th-Pb LA-Q-ICP-MS dating of detrital zircon. The scope of our fundamental research encompasses the Siberia, the Kola Peninsula and Karelia regions. In recent years, our team has obtained new data on the tectono-thermal evolution of the Siberian Traps Large Igneous Province and the basement of the East European Platform. We engage in active collaboration with companies in the oil and gas sector, offering services in fission-track dating of apatite and zircon, as well as U-Pb dating of clastic (detrital) zircon.

  1. Analysis of nanocarp tracks
  2. Cathodoluminescent survey of zircon
  3. Laser ablation
  4. Inductively coupled plasma mass spectrometry
  5. Petrography
  6. Scanning electron microscopy (SEM)
  7. Raman spectroscopy
  8. Track dating
  9. U-Pb dating of zircon
Roman Veselovskiy 🥼 🤝
Head of Laboratory

Research directions

Geochronology and thermochronology

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Track analysis (fission-track dating) of apatite and zircon, U-Pb dating of zircon and apatite, electron and optical microscopy, Raman spectroscopy and much more.

Analytical studies of rocks and materials

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The X-ray method for determining the elemental composition of rocks and substances using the Olympus Vanta M portable X-ray fluorescence (XRF) analyzer is an express determination of the qualitative chemical composition of minerals, rocks, ores, metals, soils, soils, wastewater, oil and other substances with the possibility of visiting the research facility. Scanning electron microscopy. Optical microscopy, petrography.

Publications and patents

Found 

Partners

Lab address

Москва, пос. Мосрентген, 41, стр. 1
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