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Tectonic evolution of the northern Verkhoyansk Fold-and-Thrust Belt: insights from palaeostress analysis and U–Pb calcite dating

Published online by Cambridge University Press:  21 July 2022

Elena A Pavlovskaia Open the ORCID record for Elena A Pavlovskaia [Opens in a new window] ,
Andrey K Khudoley ,
Jonas B Ruh ,
Artem N Moskalenko ,
Marcel Guillong  and
Sergey V Malyshev
Elena A Pavlovskaia*
Affiliation:
Institute of Earth Sciences, St Petersburg State University, 7/9 University Nab., St Petersburg, 199034, Russia
Andrey K Khudoley
Affiliation:
Institute of Earth Sciences, St Petersburg State University, 7/9 University Nab., St Petersburg, 199034, Russia Institute of the Earth’s Crust, Siberian Branch of the Russian Academy of Sciences, Lermontova st. 128, Irkutsk, 664033, Russia
Jonas B Ruh
Affiliation:
Department of Earth Sciences, Structural Geology and Tectonics Group, Geological Institute, ETH Zürich, Zürich, Switzerland
Artem N Moskalenko
Affiliation:
Institute of Earth Sciences, St Petersburg State University, 7/9 University Nab., St Petersburg, 199034, Russia
Marcel Guillong
Affiliation:
Department of Earth Sciences, Structural Geology and Tectonics Group, Geological Institute, ETH Zürich, Zürich, Switzerland
Sergey V Malyshev
Affiliation:
Institute of Earth Sciences, St Petersburg State University, 7/9 University Nab., St Petersburg, 199034, Russia Institute of the Earth’s Crust, Siberian Branch of the Russian Academy of Sciences, Lermontova st. 128, Irkutsk, 664033, Russia
*
Author for correspondence: Elena A Pavlovskaia, Email: pavlovskaia.elena@gmail.com
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Abstract

A combined structural and geochronological study was carried out to identify the tectonic evolution of the northern Verkhoyansk Fold-and-Thrust Belt, formed on the east margin of the Siberian Craton during late Mesozoic collision. Fault and fold geometries and kinematics were used for palaeostress reconstruction along the Danil and Neleger rivers cross-cutting the central and western parts of the Kharaulakh segment of the northern Verkhoyansk. Three different stress fields (thrust, normal and strike-slip faulting) were identified after separation from heterogeneous fault-slip data. Thrust and normal faulting stress fields were found in both areas, whereas a strike-slip faulting stress field was only found in Neoproterozoic rocks of the Neleger River area. U–Pb laser ablation – inductively coupled plasma – mass spectrometry (LA-ICP-MS) dating of calcite slickenside samples reveals the following succession of major deformation events across the northern Verkhoyansk: (i) The oldest tectonic event corresponding to the strike-slip faulting stress field with NE–SW-trending compression axis is Early Permian (Cisuralian, 284 ± 7 Ma) and likely represents a far-field response to the late Palaeozoic collision of the Kara terrane with the northern margin of the Siberian Craton. (ii) A slickenfibrous calcite age of 125 ± 4 Ma is attributed to the Early Cretaceous compression event, when the fold-and-thrust structure was formed. (iii) U–Pb slickenfibre calcite ages of 76–60 Ma estimate the age of a Late Cretaceous – Palaeocene compression event, when thrusts were reactivated. Slickensides related to both (ii) and (iii) compressional tectonic events formed by similar stress fields with W–E-trending compression axes. (iv) From the Palaeocene onwards, extensional tectonics with approximately W–E extension predominated.

Keywords

Verkhoyansk Fold-and-Thrust BeltpalaeostressU-Pb calcite datingnortheast Asia
Type
ABSOLUTE DATING OF FAULTS AND FRACTURES
Information
Geological Magazine , Volume 159 , Issue 11-12: THEMATIC ISSUE: Faults and fractures in rocks: mechanics, occurrence, dating, stress history and fluid flow , November 2022 , pp. 2132 - 2156
Copyright
© The Author(s), 2022. Published by Cambridge University Press

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