2D Reverse Tectonic Modelling along the DOBRE-2000 deep seismic reflection profile and its northern continuation in the Donbas Foldbelt, Ukraine

Y. Maystrenko; U. Bayer; S. Stovba; R. Stephenson; A. Saintot

doi:10.3997/2214-4609-pdb.38.F003

2D Reverse Tectonic Modelling along the DOBRE-2000 deep seismic reflection profile and its northern continuation in the Donbas Foldbelt, Ukraine
By Y. Maystrenko, U. Bayer, S. Stovba, R. Stephenson and A. Saintot
Publisher: European Association of Geoscientists & Engineers
Source: Conference Proceedings, Geophysics of the 21st Century - The Leap into the Future, Sep 2003, cp-38-00057
DOI: https://doi.org/10.3997/2214-4609-pdb.38.F003

Abstract

2D reverse tectonic modelling was carried out to examine the results of the DOBRE-2000 deep seismic reflection profile and its northern continuation. The results of the palinspastic reconstruction show that a crustal-scale pop-up structure provides a reasonable interpretation. In addition, we present the evolution of the Donbas Foldbelt (DF) through time by 2D reverse tectonic modelling. Tectonic modelling from the Late Devonian rifting to the Pre-Triassic uplift was done taking into account two phases of salt tectonics which occurred during Early Carboniferous.

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2003-09-01

2024-04-27

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2D Reverse Tectonic Modelling along the DOBRE-2000 deep seismic reflection profile and its northern continuation in the Donbas Foldbelt, Ukraine

Abstract

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The natural combination of full and image‐based waveform inversion

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Characterizing the effect of elastic interactions on the effective elastic properties of porous, cracked rocks

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Laboratory measurements of guided‐wave propagation within a fluid‐saturated fracture