Abstract
The paper presents the results of paleomagnetic and geochronological studies on the Lower Cretaceous sandstones of the Silasa and Kema Formations (Kiselevka-Manoma and Kema terranes, respectively). Source areas of rocks are determined and paleolatitudes at which they formed are constrained. The fact that ages of zircons from sandstones of the studied formations differ essentially suggests that the material from a source area in continental Eurasia was not transported to the deposition area of the Silasa Formation. The reason is that sediments of the Silasa Formation accumulated in the outer island arc zone separated by the fore-arc basin from the inner island arc zone where the material from the continent was transported to the deposition area of the Kema Formation.
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The study was supported by the Russian Foundation for Basic Research (project no. 18-05-00117) and as part of the State Assignment to the ITiG FEB RAS.
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Arkhipov, M.V. et al. (2019). Results of Paleomagnetic and Geochronological Studies of Sedimentary Rocks from Kema and Silasa Formations of the Sikhote-Alin Orogen. In: Nurgaliev, D., Shcherbakov, V., Kosterov, A., Spassov, S. (eds) Recent Advances in Rock Magnetism, Environmental Magnetism and Paleomagnetism. Springer Geophysics. Springer, Cham. https://doi.org/10.1007/978-3-319-90437-5_1
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