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Chapter 6.4 The Oldest Rock Assemblages of the Siberian Craton
2007Publisher Summary This chapter elaborates the oldest rock assemblages of the Siberian Craton. The Siberian Craton that occupies an area of approximately 4 × 10 6 km 2 is overlain largely by Mesoproterozoic to Phanerozoic sedimentary rocks, whose thickness ranges between 1 and 8 km, averaging approximately 4 km.
Oleg M. Rosen, O.M. Turkina
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Phanerozoic mafic magmatism in the southern Siberian craton: geodynamic implications
Russian Geology and Geophysics, 2010Abstract The Phanerozoic history of mafic magmatism in the southern Siberian craton included three major events. The earliest event (∼500 Ma) recorded in dolerite dikes occurred during accretion and collision at the early stage of the Central Asian orogen.
Gladkochub, D. +6 more
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Evidence of Eoarchean crust beneath the Yakutian kimberlite province in the Siberian craton
Precambrian Research, 2022Qin Wang
exaly

