Выявление признаков дифференциации глинисто-кремнистых и карбонатных пород в крутопадающих пластах доюрского фундамента Западной Сибири по данным сейсморазведки

Translated title of the contribution: Identification of signs of differentiation of clay-siliceous and carbonate rocks in steeply dipping beds of the pre-Jurassic basement of Western Siberia according to the seismic data

A. Volkova, V. Merkulov

Research output: Chapter in Book/Report/Conference proceedingConference contribution

Abstract

The paper proposes an approach to the study of Paleozoic sediments by direct seismic modeling in combination with the analysis of real seismic data and the results of core studies for one of the fields in the Tomsk region. The regularities of the dynamics of the wave pattern of the upper part of the Paleozoic section with the lithological composition of rocks are revealed.

Translated title of the contributionIdentification of signs of differentiation of clay-siliceous and carbonate rocks in steeply dipping beds of the pre-Jurassic basement of Western Siberia according to the seismic data
Original languageRussian
Title of host publicationTyumen 2019
Subtitle of host publication6th Conference
PublisherEuropean Association of Geoscientists and Engineers, EAGE
ISBN (Electronic)9789462822801
DOIs
Publication statusPublished - 1 Jan 2019
Event6th Scientific Conference - Tyumen 2019 - Tyumen, Russian Federation
Duration: 25 Mar 201929 Mar 2019

Publication series

NameTyumen 2019: 6th Conference

Conference

Conference6th Scientific Conference - Tyumen 2019
CountryRussian Federation
CityTyumen
Period25.3.1929.3.19

ASJC Scopus subject areas

  • Electrical and Electronic Engineering
  • Fuel Technology
  • Renewable Energy, Sustainability and the Environment

Fingerprint Dive into the research topics of 'Identification of signs of differentiation of clay-siliceous and carbonate rocks in steeply dipping beds of the pre-Jurassic basement of Western Siberia according to the seismic data'. Together they form a unique fingerprint.

Cite this