Articles | Volume 12, issue 12
https://doi.org/10.5194/se-12-2773-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/se-12-2773-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Sedimentary basins of the eastern Asia Arctic zone: new details on their structure revealed by decompensative gravity anomalies
Geophysical Center of the Russian Academy of Sciences (GC RAS),
Moscow, Russia
Mikhail K. Kaban
Geophysical Center of the Russian Academy of Sciences (GC RAS),
Moscow, Russia
German Research Center for Geosciences (GFZ), Potsdam, Germany
Schmidt Institute of Physics of the Earth of the Russian Academy of
Sciences (IPE RAS), Moscow, Russia
Anatoly A. Soloviev
Geophysical Center of the Russian Academy of Sciences (GC RAS),
Moscow, Russia
Schmidt Institute of Physics of the Earth of the Russian Academy of
Sciences (IPE RAS), Moscow, Russia
Alexei G. Petrunin
Geophysical Center of the Russian Academy of Sciences (GC RAS),
Moscow, Russia
German Research Center for Geosciences (GFZ), Potsdam, Germany
Schmidt Institute of Physics of the Earth of the Russian Academy of
Sciences (IPE RAS), Moscow, Russia
Alexei D. Gvishiani
Geophysical Center of the Russian Academy of Sciences (GC RAS),
Moscow, Russia
Schmidt Institute of Physics of the Earth of the Russian Academy of
Sciences (IPE RAS), Moscow, Russia
Alexei A. Oshchenko
Geophysical Center of the Russian Academy of Sciences (GC RAS),
Moscow, Russia
Anton B. Popov
Geophysical Center of the Russian Academy of Sciences (GC RAS),
Moscow, Russia
Roman I. Krasnoperov
Geophysical Center of the Russian Academy of Sciences (GC RAS),
Moscow, Russia
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Subject area: Crustal structure and composition | Editorial team: Geodesy, gravity, and geomagnetism | Discipline: Remote sensing
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One motivation for this study is to develop a workflow that enables the integration of geophysical datasets with different coverages that are quite common in exploration geophysics. We have utilized a level set approach to achieve this goal. The utilized technique parameterizes the subsurface in the same fashion as geological models. Our results indicate that the approach is capable of integrating information from seismic data in 2D to guide the 3D inversion results of the gravity data.
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Short summary
In the present study, the structure of sedimentary basins in the eastern Asia Arctic zone is analysed by employing the approach based on decompensative gravity anomalies. Two obtained models of thickness and density of sediments in the study area display significant changes in the thickness and distribution of sedimentary rocks revealed for some particular basins. The new results improve our knowledge about the region, providing a better understanding of the evolution of the sedimentary basins.
In the present study, the structure of sedimentary basins in the eastern Asia Arctic zone is...