MESOZOIC INTRACONTINENTAL OROGENY IN THE TECTONIC HISTORY OF THE KOLYVAN’-TOMSK FOLDED ZONE (southern Siberia): A SYNTHESIS OF GEOLOGICAL DATA AND RESULTS OF APATITE FISSION TRACK ANALYSIS
F.I. Zhimulev1, E.V. Vetrov1, I.S. Novikov1, G. Van Ranst2, S. Nachtergaele2, S.A. Dokashenko1, J. De Grave2
1V.S. Sobolev Institute of Geology and Mineralogy, Siberian Вrаnch of the Russian Academy of Sciences, Novosibirsk, Russia
2Department of Geology, Ghent University, Gent, Belgium
Keywords: Intracontinental orogeny, Mesozoic, apatite fission track thermochronology, planation surface, molasse, granites, Central Asian Orogenic Belt, West Siberia
Abstract
The Kolyvan’-Tomsk folded zone (KTFZ) is a late Permian collisional orogen in the northwestern section of the Central Asian Orogenic Belt. The Mesozoic history of the KTFZ area includes Late Triassic-Early Jurassic and Late Jurassic-Early Cretaceous orogenic events. The earlier event produced narrow deep half-ramp basins filled with Early-Middle Jurassic molasse south of the KTFZ, and the later activity rejuvenated the Tomsk thrust fault, whereby the KTFZ Paleozoic rocks were thrust over the Early-Middle Jurassic basin sediments. The Mesozoic orogenic events induced erosion and the ensuing exposure of granitoids (Barlak complex) that were emplaced in a within-plate context after the Permian collisional orogeny. Both events were most likely associated with ocean closure, i.e., the Paleothetys Ocean in the Late Triassic-Early Jurassic and the Mongol-Okhotsk Ocean in the Late Jurassic-Early Cretaceous. The apatite fission track (AFT) ages of granitoids from the Ob’ complex in the KTFZ range between ~120 and 100 Ma (the Aptian and the Albian). The rocks with Early Cretaceous AFT ages were exhumed as a result of denudation and peneplanation of the Early Cretaceous orogen, which produced a vast Late Cretaceous-Paleogene planation surface. The tectonic pattern of the two orogenic events, although being different in details, generally inherited the late Paleozoic primary collisional structure of the Kolyvan’-Tomsk zone.
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