TWO-STAGE MODEL OF DEVONIAN BASIC MAGMATISM IN THE VILYUI PALEORIFT (Siberian Platform)
O.P. Polyansky1, V.A. Simonov1, O.V. Koroleva2, A.V. Prokopiev2, A.V. Babichev1, A.V. Kotlyarov1, A.N. Semenov1
1V.S. Sobolev Institute of Geology and Mineralogy, Siberian Branch of the Russian Academy of Sciences, Novosibirsk, Russia
2Diamond and Precious Metal Geology Institute, Siberian Branch of the Russian Academy of Sciences, Yakutsk, Russia
Keywords: Dike swarm, melt inclusions, thermobarometry, geochemistry, basic magmatism, 40Ar/39Ar age, numerical modeling, Siberian Platform, Vilyui paleorift
Abstract
We report study results of basic intrusive bodies in the middle Paleozoic Vilyui paleorift (eastern Siberian Platform). Geochemical data for basic sills penetrated by boreholes in the rift’s dike swarms are presented, as well as our data on the time of formation of sills and dikes. We also studied mineral-hosted melt inclusions from a dolerite dike of the Vilyui-Markha dike swarm on the northwestern flank of the Vilyui paleorift. Data on the compositions of homogenous glasses of mineral-hosted melt inclusions yielded the P-T parameters of mantle sources of basic melts responsible for the formation of the Vilyui paleorift gabbro-dolerites. Two depth levels of basic melt generation have been established: 95-65 km at 1480-1400 °C and 55-45 km at 1360-1320 °C. Crystallization of the melts occurred at a shallow depth of 12-4 km with a decrease in temperature from 1185 to 1125 °С. This occurrence of basic melt sources at two different depths, as well as the heterogeneity of the chemical composition of melt inclusions and their host minerals explains the presence of two pulses of Devonian basic magmatism. Our new numerical thermomechanical model of magma rise during melting of the lithospheric mantle above a mantle plume supports the existence of two chambers at the spinel-garnet peridotite boundary and under the base of the crust, as well as the two-stage nature of Devonian magmatism.
|
