A copy of this work was available on the public web and has been preserved in the Wayback Machine. The capture dates from 2020; you can also visit the original URL.
The file type is application/pdf.
The first petrological evidence of subduction at the western margin of the Siberian сraton
2019
Doklady Akademii Nauk
Preserved Fulltext
The discovery of relics of glaucophane schist in high-pressure tectonites of the suture zone of Yenisei Ridge has provided evidence for a Cordillera-type convergent boundary controlled by subduction of the oceanic crust beneath the continental margin on the western side of the Siberian Craton. According to the microtextural patterns of rocks and the results of geothermobarometry, two stages of metamorphism were distinguished. The formation of high-pressure tectonites indicates the early stage
doi:10.31857/s0869-56524842209-214
fatcat:ma3z4wyx3rd3fgi5mxse36ac3a