Showing 1 - 5 results of 5 for search 'B. V. Lunev', query time: 0.01s Refine Results
  1. 1
    MODEL OF DECOMPRESSION MELTING MECHANISM IN CONVECTIVE-UNSTABLE THERMAL LITHOSPHERE (FIRST APPROXIMATION)

    MODEL OF DECOMPRESSION MELTING MECHANISM IN CONVECTIVE-UNSTABLE THERMAL LITHOSPHERE (FIRST APPROXIMATION) by B. V. Lunev, V. V. Lapkovsky

    Published 2021-09-01
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  2. 2
    The first-approximation model showing the occurrence of epicontinental sedimentary basins due to convective instability of the thermal lithosphere

    The first-approximation model showing the occurrence of epicontinental sedimentary basins due to convective instability of the thermal lithosphere by B. V. Lunev, V. V. Lapkovsky

    Published 2018-12-01
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  3. 3
    Modeling of Salt Tectogenesis in Connection With the Choice of the Main Directions for the Search For Hydrocarbon Deposits and Hydromineral Raw Materials Within the Kempendyai Depression (South-East оf the Siberian Platform)

    Modeling of Salt Tectogenesis in Connection With the Choice of the Main Directions for the Search For Hydrocarbon Deposits and Hydromineral Raw Materials Within the Kempendyai Depr... by B. V. Lunev, I. A. Gubin, V. V. Lapkovsky, R. V. Marinov

    Published 2024-12-01
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  4. 4
    Prediction of the Spatial Distribution of Petrophysical Properties of Sediment Formations Using Multidimensional Splines

    Prediction of the Spatial Distribution of Petrophysical Properties of Sediment Formations Using Multidimensional Splines by V. V. Lapkovsky, V. A. Kontorovich, K. I. Kanakova, S. E. Ponomareva, B. V. Lunev

    Published 2024-09-01
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  5. 5
    INFLUENCE OF THE EVAPORITE FORMATION STRUCTURE ON SALT TECTONICS AND HYDROCARBON TRAPS (BY THE RESULTS OF NUMERICAL SIMULATION OF HALOKINESIS IN THE PRE-CASPIAN)

    INFLUENCE OF THE EVAPORITE FORMATION STRUCTURE ON SALT TECTONICS AND HYDROCARBON TRAPS (BY THE RESULTS OF NUMERICAL SIMULATION OF HALOKINESIS IN THE PRE-CASPIAN) by B. V. Lunev, V. V. Lapkovsky, M. P. Antipov, Y. A. Volozh, I. S. Postnikova

    Published 2023-04-01
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