Results of Studying the Material Composition and U-Pb (LA-ICP-MS) Age of Detrital Zircons From Terrigenous Rocks of the Vanavara and Oskobinskaya Formations of the Kamov Arch of the Baikit Antelise

The paper presents the results of studies on sandstones from the Vanavara and Oskobinskaya formations, which are part of the Nepa and Torskiy regional stratigraphic horizons, respectively. These formations were studied using the core from the Yur-92 deep well, located within the Kamov Arch of the Ba...

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Egile Nagusiak:	A. V. Plusnin, Z. L. Motova, I. V. Afonin, E. M. Tomilina, D. A. Staroselets, E. E. Belozerov, I. R. Khalikov, M. V. Shaldybin, I. A. Yashin, V. A. Fomin
Formatua:	Artigo
Hizkuntza:	Inglês
Argitaratua:	Georesursy Ltd. 2025-04-01
Saila:	Georesursy
Gaiak:	siberian platform baikit anteclise vanavara formation oskoba formation vendian lithogeochemistry detrital zircons paleogeodynamics
Sarrera elektronikoa:	https://www.geors.ru/jour/article/view/479
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