Vol. 15, no.4, 2023
РусскийEnglish

INFORMATION TECHNOLOGIES



LOCALIZATION OF THE GEOLOGICAL LAYER BOUNDARIES USING THE REVERSE TIME MIGRATION METHOD
Alexey V. Shevchenko, Vasily I. Golubev

Moscow Institute of Physics and Technology, https://mipt.ru/
Dolgoprudny 141700, Moscow region, Russian Federation
E-mail: alexshevchenko@phystech.edu, golubev.vi@mipt.ru
Anton V. Ekimenko
Gazpromneft’s Research and Development Center, https://ntc.gazprom-neft.com/
St Petersburg 190000, Russian Federation
E-mail: ekimenko.AV@gazpromneft-ntc.ru

Received October 09, 2023, peer-reviewed October 16, 2023, accepted October 23, 2023, published December 06, 2023.


Abstract: The article is devoted to solving an important practical problem - determining the structure of the subsurface space of the geological environment based on surface seismic data. Thanks to the registration of seismic waves reflected from the boundaries of geological layers, it is possible to delineate hydrocarbon deposits, which makes it possible to effectively plan a field development scheme. Optimizing the production process makes it possible to make it profitable, including when developing unconventional hydrocarbon deposits. The paper discusses the technology of constructing a migration image using the reverse time migration method. In the general case, an analytical derivation of the calculation formulas was carried out. For the practically significant case of an acoustic environment, simplified calculation formulas are explicitly written out and implemented in the form of a software algorithm. The issue of improving the quality of the migration image without significantly increasing the computational complexity of the problem is discussed separately. The authors demonstrated the performance of this approach using the widely used Marmousi geological model.

Keywords: mathematical modeling, seismic survey, reverse-time migration

UDC 004.94

RENSIT, 2023, 15(1):433-440e DOI: 10.17725/rensit.2023.15.433

Full-text electronic version of this article - web site http://en.rensit.ru/vypuski/article/520/15(4)433-440e.pdf