Russian Journal of Earth Sciences Russian Journal of Earth Sciences Russian Journal of Earth Sciences 1681-1208 100528 10.2205/2025ES001022 iljgbb ОРИГИНАЛЬНЫЕ СТАТЬИ ORIGINAL ARTICLES ОРИГИНАЛЬНЫЕ СТАТЬИ Petrophysical Properties of Rocks of the Northern Ladoga Petrophysical Properties of Rocks of the Northern Ladoga https://orcid.org/0009-0004-5862-7428 Таран Я. В. Taran Ya. V. https://orcid.org/0000-0001-7489-2951 Алёшин Игорь Михайлович Aleshin Igor Mikhaylovich ima@ifz.ru Институт физики Земли им. О.Ю. Шмидта Российской академии наук Moscow Россия Schmidt Institute of Physics of the Earth of the Russian Academy of Sciences Moscow Russian Federation Геофизический центр РАН Москва Россия Geophysical Center of the Russian Academy of Sciences Moscow Russian Federation 30 06 2025 30 06 2025 25 4 ES4003 19 05 2025 20 06 2025 https://rjes.ru/en/nauka/article/100528/view

Northern Ladoga is a region of Southeastern Fennoscandia with complex geological and tectonic structure. It is crossed by the Raakhe–Ladoga junction zone of the Karelian craton and the Svecofennian orogen. Analysis of existing data on the petrophysical properties of rocks in the region was carried out as part of a complex geophysical modelling of Northern Ladoga. Based on these data, a summary table of the properties of the rocks of the Northern Ladoga region was compiled using modern geological maps.

Northern Ladoga is a region of Southeastern Fennoscandia with complex geological and tectonic structure. It is crossed by the Raakhe–Ladoga junction zone of the Karelian craton and the Svecofennian orogen. Analysis of existing data on the petrophysical properties of rocks in the region was carried out as part of a complex geophysical modelling of Northern Ladoga. Based on these data, a summary table of the properties of the rocks of the Northern Ladoga region was compiled using modern geological maps.

 Fennoscandia Northern Ladoga petrophysical properties Raakhe–Ladoga zone Fennoscandia Northern Ladoga petrophysical properties Raakhe–Ladoga zone This work was conducted in the framework of budgetary funding of the Geophysical Center of RAS and Schmidt Institute of Physics of the Earth RAS, adopted by the Ministry of Science and Higher Education of the Russian Federation. This work was conducted in the framework of budgetary funding of the Geophysical Center of RAS and Schmidt Institute of Physics of the Earth RAS, adopted by the Ministry of Science and Higher Education of the Russian Federation.

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