Introduction to the volume, and definition and use of the term ‘tectono-sedimentary element’

The present volume is rooted in a map of sedimentary successions of the Arctic Region by Grantz et al. (2011), and contains a brief, but comprehensive compilation of geological and geophysical data characterizing all significant sedimentary successions in the Arctic, which cover 57% of the polar are...

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Bibliographic Details
Published in:Geological Society, London, Memoirs
Main Authors: Drachev, Sergey, Brekke, Harald, Henriksen, Erik, Moore, Thomas
Format: Article in Journal/Newspaper
Language:English
Published: Geological Society 2021
Subjects:
Online Access:https://hdl.handle.net/10037/24580
https://doi.org/10.1144/M57-2021-30
Description
Summary:The present volume is rooted in a map of sedimentary successions of the Arctic Region by Grantz et al. (2011), and contains a brief, but comprehensive compilation of geological and geophysical data characterizing all significant sedimentary successions in the Arctic, which cover 57% of the polar area north of 64°N. Two main goals have been designated: (i) to provide, based on the present-day knowledge and data, a characterization of all Arctic sedimentary successions (or sedimentary accumulations), and (ii) to supply a snapshot of hydrocarbon-related exploration in the Arctic at the end of the second decade of this millennium. To achieve these goals, we represent sedimentary successions as consisting of one or several “Tectono-Sedimentary Elements” (TSE). This concept allows delineation, mapping, and characterization of 9 categories of TSEs based of main tectonic regimes that formed accommodation space. A TSE characterization template has been developed as an efficient method of organising and presenting the most important information about stratigraphy, structure, and petroleum geology of a TSE, including most significant exploration facts. This organizationa architecture is the backbone of the volume and is a key feature that distinguishes it from other similar works about the sedimentary basins.