Standard

Calculation of the 3D density model of the earth s crust in the sea of okhotsk. / Butsenko, V.; Piskarev, A.; Poselov, V.

2010. Paper presented at 4th International Conference and Exhibition: New Discoveries through Integration of Geosciences, Saint Petersburg, Russian Federation.

Research output: Contribution to conferencePaperpeer-review

Harvard

Butsenko, V, Piskarev, A & Poselov, V 2010, 'Calculation of the 3D density model of the earth s crust in the sea of okhotsk', Paper presented at 4th International Conference and Exhibition: New Discoveries through Integration of Geosciences, Saint Petersburg, Russian Federation, 5/04/10 - 8/04/10.

APA

Butsenko, V., Piskarev, A., & Poselov, V. (2010). Calculation of the 3D density model of the earth s crust in the sea of okhotsk. Paper presented at 4th International Conference and Exhibition: New Discoveries through Integration of Geosciences, Saint Petersburg, Russian Federation.

Vancouver

Butsenko V, Piskarev A, Poselov V. Calculation of the 3D density model of the earth s crust in the sea of okhotsk. 2010. Paper presented at 4th International Conference and Exhibition: New Discoveries through Integration of Geosciences, Saint Petersburg, Russian Federation.

Author

Butsenko, V. ; Piskarev, A. ; Poselov, V. / Calculation of the 3D density model of the earth s crust in the sea of okhotsk. Paper presented at 4th International Conference and Exhibition: New Discoveries through Integration of Geosciences, Saint Petersburg, Russian Federation.

BibTeX

@conference{c0b1a6775fa7434e95e7c9fa1332fcb7,
title = "Calculation of the 3D density model of the earth s crust in the sea of okhotsk",
abstract = "The paper contains the results of combine studying of the Sea of Okhotsk continental margin. The structure of its surface, modern geodynamics, geophysical parameters and deep structure are investigated. Potential field anomalies of the Sea of Okhotsk have been analyzed. The 3D density model of the main Earth crust structures is compiled and calculated, leaning on the seismic-geological and experimental petrophysical data. The model gives a visual explanation for the observed geophysical anomalies. The schematic map of the basement tectonics is one of the investigation results. So we come nearer to the solution of the general regional problems of the Earth crust construction and the exploration prospects. Analysis of the received geophysical material helps to improve the planning of the future projects and allows to determine the Sea of Okhotsk enclave area locating outside the exclusive economic zone of the Russian Federation as the natural continuation of continental margin.",
author = "V. Butsenko and A. Piskarev and V. Poselov",
year = "2010",
month = jan,
day = "1",
language = "English",
note = "4th International Conference and Exhibition: New Discoveries through Integration of Geosciences ; Conference date: 05-04-2010 Through 08-04-2010",

}

RIS

TY - CONF

T1 - Calculation of the 3D density model of the earth s crust in the sea of okhotsk

AU - Butsenko, V.

AU - Piskarev, A.

AU - Poselov, V.

PY - 2010/1/1

Y1 - 2010/1/1

N2 - The paper contains the results of combine studying of the Sea of Okhotsk continental margin. The structure of its surface, modern geodynamics, geophysical parameters and deep structure are investigated. Potential field anomalies of the Sea of Okhotsk have been analyzed. The 3D density model of the main Earth crust structures is compiled and calculated, leaning on the seismic-geological and experimental petrophysical data. The model gives a visual explanation for the observed geophysical anomalies. The schematic map of the basement tectonics is one of the investigation results. So we come nearer to the solution of the general regional problems of the Earth crust construction and the exploration prospects. Analysis of the received geophysical material helps to improve the planning of the future projects and allows to determine the Sea of Okhotsk enclave area locating outside the exclusive economic zone of the Russian Federation as the natural continuation of continental margin.

AB - The paper contains the results of combine studying of the Sea of Okhotsk continental margin. The structure of its surface, modern geodynamics, geophysical parameters and deep structure are investigated. Potential field anomalies of the Sea of Okhotsk have been analyzed. The 3D density model of the main Earth crust structures is compiled and calculated, leaning on the seismic-geological and experimental petrophysical data. The model gives a visual explanation for the observed geophysical anomalies. The schematic map of the basement tectonics is one of the investigation results. So we come nearer to the solution of the general regional problems of the Earth crust construction and the exploration prospects. Analysis of the received geophysical material helps to improve the planning of the future projects and allows to determine the Sea of Okhotsk enclave area locating outside the exclusive economic zone of the Russian Federation as the natural continuation of continental margin.

UR - http://www.scopus.com/inward/record.url?scp=84898994335&partnerID=8YFLogxK

M3 - Paper

T2 - 4th International Conference and Exhibition: New Discoveries through Integration of Geosciences

Y2 - 5 April 2010 through 8 April 2010

ER -

ID: 36844230