Relative Paleointensity of Geomagnetic Field over the Past 9000 Years Estimated by the Pseudo-Thellier Method from the Bottom Sediments of Lake Shira, Northern Khakassia

• Published in: Izvestiya. Physics of the solid earth Vol. 60; no. 4; pp. 663 - 680
• Main Authors: Kuzina, D. M., Shcherbakov, V. P., Salnaia, N. V., Yusupova, A. R., Li, H.-Ch, Nurgaliev, D. K.
• Format: Journal Article
• Language: English
• Published: Moscow Pleiades Publishing 01.08.2024
• Subjects: Earth and Environmental Science; Earth Sciences; Geophysics/Geodesy; bottom sediments; pseudo-Thellier method; relative paleointensity; Lake Shira
• ISSN: 1069-3513; 1555-6506
• DOI: 10.1134/S1069351324700587

—The paper presents the results of rock magnetic studies and relative paleointensity determinations from sediments of Lake Shira, Khakassia. Carrier minerals of natural remanent magnetization (NRM) were identified through hysteresis loop parameter measurements, thermomagnetic and X-ray diffraction (XRD) analyses. The sediment age was determined by radiocarbon dating; according to age estimates, the studied sediment sequence covers approximately the past 9100 years. To obtain high-quality relative paleointensity results, the determinations were made on linear segments of the pseudo-Arai‒Nagata diagrams. The quality was assessed by the criteria of the number of points in the calculations of slope, quality criterion ( q ), NRM fraction destroyed in the paleointensity determination interval, and relative paleointensity determination error (σ). According to the rock magnetic studies and XRD analysis, the magnetic carriers are mainly single-domain (SD) and pseudo-single-domain (PSD) magnetite and hematite. The comparison of the obtained relative paleointensity data with model paleointensities calculated for the Shira coordinates from the various models (CALS10K.1b (Korte et al., 2011), PFM9k.1 (Nilsson et al., 2014), HFM.OL1.AL1, CALS10k.2 ARCH10k.1 (Constable et al., 2016)), with absolute paleointensities and with the collection of results from the studies of sedimentary and igneous rocks and archaeomagnetic objects has shown that these data are in good agreement and share common trends. This provides grounds for applying this approach to paleointensity determination from bottom sediments of modern lakes using the pseudo-Thellier method.