Tectonics of the junction region between the East European craton and West Arctic platform


Cite item

Full Text

Open Access Open Access
Restricted Access Access granted
Restricted Access Subscription Access

Abstract

The region of the junction and interaction between the East European Craton (EEC) and the West Arctic Craton (WAC) is regarded as a complexly built zone or assembly of both the volumetric and dividing linear tectonic elements: the Trollfjord–Rybachi–Kanin (TRK) Lineament, the pericratonic subsidence zone of the EEC, the Karpinskii Lineament, the Murmansk Block of the Fennoscandian (Baltic) Shield, and the Kolmozero–Voronya Zone, which are briefly characterized in this paper. Evidences of thrusting have been established not only in the TRK Suture Zone and on the Rybachi Peninsula, which represent a fragment of the Timanides fold–thrust belt, but also to the southwest, in the Upper Riphean and Vendian terrigenous sequences making up the Sredni Peninsula and related to the pericratonic trough of the VEC. Two phases of fold–thrust deformations with elements of left-lateral strike-slip offset pertaining to the activity and evolution of the lineament suture dividing the Sredni and Rybachi peninsulas have been recorded. The variously oriented fault–fold systems within this fault zone are evidence for multistage deformation and can be explained by an at least twostage change in the kinematics that control displacement along the fault. The disintegrated granitic massifs of the Archean crystalline basement tectonically squeezed out in the upper crust as protrusions are localized within TRK Fault Zone. Plagiogranitic bodies, which underwent superposed fault-fold deformations of both kinematic stages, are an evidence of the vigorous tectonic event that predated folding and two-stage strike-slip displacement along the TRK Fault—by thrusting of Riphean sequences from north to south toward the Archean craton. The nappe–thrust regional structure was formed at this stage; elements of it have been recognized in the Sredni, Rybachi, and Kanin peninsulas. The main stages of tectonic evolution in the junction zone between the EEC and the WAP have been revealed and substantiated.

About the authors

A. S. Baluev

Geological Institute

Author for correspondence.
Email: albaluev@yandex.ru
Russian Federation, Pyzhevskii per. 7, Moscow, 119017

Y. A. Morozov

Schmidt Institute of Physics of the Earth

Email: albaluev@yandex.ru
Russian Federation, ul. Bol’shaya Gruzinskaya 10, Moscow, 1213995

E. N. Terekhov

Geological Institute

Email: albaluev@yandex.ru
Russian Federation, Pyzhevskii per. 7, Moscow, 119017

T. B. Bayanova

Geological Institute, Kola Science Center

Email: albaluev@yandex.ru
Russian Federation, pr. Fersmana 14, Apatity, Murmansk oblast, 184209

S. N. Tyupanov

Geological Institute

Email: albaluev@yandex.ru
Russian Federation, Pyzhevskii per. 7, Moscow, 119017

Supplementary files

Supplementary Files
Action
1. JATS XML

Copyright (c) 2016 Pleiades Publishing, Inc.