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New Type of Fluidizate-Explosive Rock in Sedimentary Strata (Torgashino Limestone Deposit, Eastern Sayan Mountains, Russia)
Siberian Federal University, Svobodny pr. 79, Krasnoyarsk, Russian Federation
Siberian Federal University, Svobodny pr. 79, Krasnoyarsk, Russian Federation
Astafyev Krasnoyarsk Teachers’ Training University, Lebedevoy St. 89, Krasnoyarsk, Russian Federation
- 1 Siberian Federal University, Svobodny pr. 79, Krasnoyarsk, Russian Federation
- 2 Siberian Federal University, Svobodny pr. 79, Krasnoyarsk, Russian Federation
- 3 Astafyev Krasnoyarsk Teachers’ Training University, Lebedevoy St. 89, Krasnoyarsk, Russian Federation
Open Journal of Geology·Volume 10 (2020)·Pages 727–740·Published 16 July 2020·DOI10.4236/ojg.2020.107032
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Abstract
The paper provides the results of comprehensive studies of bodies composed of different fluidolite types (psephitic, argillizite) and hydrothermalites found in the carbonate stratum of the Torgashino suite (Eastern Sayan Mountains, Russia). These rocks are the result of post-sedimentation processes imposed on limestones. Argillizites in the carbonate stratum are referred to a new type of fluidizate-explosive rock. Their low-temperature hydrothermal origin and association with the Later Ordovician tectono-magmatic activation of the area have been identified.
KeywordsFluidolitesHydrothermalitesFluidizate-Explosive Process
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