Deep Structure Model › Научные исследования в СПбГУ

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Deep Structure Model. / Kashubin, S. N.; Petrov, O. V.; Milshtein, E. D.; Androsov, E. A.; Vinokurov, I. Y.; Erinchek, Y. M.; Litvinova, T. P.; Mukhin, V. N.; Golysheva, Y. S.; Kashubina, T. V.; Krupnova, N. A.; Sakulina, T. S.; Suslova, S. V.; Tarasova, O. A.; Yavarova, T. M.; Vyatkina, D. V.

Tectonics of Asia (Northern, Central and Eastern Asia). ред. / O.V. Petrov; S. Dong. Springer Nature, 2021. стр. 33-61 (Springer Geology).

Результаты исследований: Публикации в книгах, отчётах, сборниках, трудах конференций › глава/раздел › научная › Рецензирование

Harvard

Kashubin, SN, Petrov, OV, Milshtein, ED, Androsov, EA, Vinokurov, IY, Erinchek, YM, Litvinova, TP, Mukhin, VN, Golysheva, YS, Kashubina, TV, Krupnova, NA, Sakulina, TS, Suslova, SV, Tarasova, OA, Yavarova, TM & Vyatkina, DV 2021, Deep Structure Model. в OV Petrov & S Dong (ред.), Tectonics of Asia (Northern, Central and Eastern Asia). Springer Geology, Springer Nature, стр. 33-61. https://doi.org/10.1007/978-3-030-62001-1_2

APA

Kashubin, S. N., Petrov, O. V., Milshtein, E. D., Androsov, E. A., Vinokurov, I. Y., Erinchek, Y. M., Litvinova, T. P., Mukhin, V. N., Golysheva, Y. S., Kashubina, T. V., Krupnova, N. A., Sakulina, T. S., Suslova, S. V., Tarasova, O. A., Yavarova, T. M., & Vyatkina, D. V. (2021). Deep Structure Model. в O. V. Petrov, & S. Dong (Ред.), Tectonics of Asia (Northern, Central and Eastern Asia) (стр. 33-61). (Springer Geology). Springer Nature. https://doi.org/10.1007/978-3-030-62001-1_2

Vancouver

Kashubin SN, Petrov OV, Milshtein ED, Androsov EA, Vinokurov IY, Erinchek YM и пр. Deep Structure Model. в Petrov OV, Dong S, Редакторы, Tectonics of Asia (Northern, Central and Eastern Asia). Springer Nature. 2021. стр. 33-61. (Springer Geology). https://doi.org/10.1007/978-3-030-62001-1_2

Author

Kashubin, S. N. ; Petrov, O. V. ; Milshtein, E. D. ; Androsov, E. A. ; Vinokurov, I. Y. ; Erinchek, Y. M. ; Litvinova, T. P. ; Mukhin, V. N. ; Golysheva, Y. S. ; Kashubina, T. V. ; Krupnova, N. A. ; Sakulina, T. S. ; Suslova, S. V. ; Tarasova, O. A. ; Yavarova, T. M. ; Vyatkina, D. V. / Deep Structure Model. Tectonics of Asia (Northern, Central and Eastern Asia). Редактор / O.V. Petrov ; S. Dong. Springer Nature, 2021. стр. 33-61 (Springer Geology).

BibTeX

@inbook{95fd26a1d539418d860dcf62b3bdfa7a,

title = "Deep Structure Model",

abstract = "The chapter provides results of the generalization and interpretation of deep geophysical studies. The model of the deep crustal structure is represented by a set of maps, showing the crustal thickness, and a 5400 km-long Geotransect, crossing major tectonic areas of northeastern Eurasia. A set of digital maps covering an area of 50,000,000 km2 is compiled in a single projection and includes the following maps: the Moho depth; the thickness of main crustal units (sedimentary cover and consolidated crust); the anomalous gravity field and anomalous magnetic field used for zoning of the area; crustal types. The Geotransect crosses North-Eastern Eurasia and characterizes the vertical section of the earth{\textquoteright}s crust and upper mantle in the passive margin of the Eurasian continent (including submarine elevations of the Arctic Ocean and its shelf part), the active eastern continental margin and extends into the Pacific Plate.",

author = "Kashubin, {S. N.} and Petrov, {O. V.} and Milshtein, {E. D.} and Androsov, {E. A.} and Vinokurov, {I. Y.} and Erinchek, {Y. M.} and Litvinova, {T. P.} and Mukhin, {V. N.} and Golysheva, {Y. S.} and Kashubina, {T. V.} and Krupnova, {N. A.} and Sakulina, {T. S.} and Suslova, {S. V.} and Tarasova, {O. A.} and Yavarova, {T. M.} and Vyatkina, {D. V.}",

year = "2021",

month = mar,

day = "4",

doi = "10.1007/978-3-030-62001-1_2",

language = "English",

series = "Springer Geology",

publisher = "Springer Nature",

pages = "33--61",

editor = "O.V. Petrov and S. Dong",

booktitle = "Tectonics of Asia (Northern, Central and Eastern Asia)",

address = "Germany",

}

RIS

TY - CHAP

T1 - Deep Structure Model

AU - Kashubin, S. N.

AU - Petrov, O. V.

AU - Milshtein, E. D.

AU - Androsov, E. A.

AU - Vinokurov, I. Y.

AU - Erinchek, Y. M.

AU - Litvinova, T. P.

AU - Mukhin, V. N.

AU - Golysheva, Y. S.

AU - Kashubina, T. V.

AU - Krupnova, N. A.

AU - Sakulina, T. S.

AU - Suslova, S. V.

AU - Tarasova, O. A.

AU - Yavarova, T. M.

AU - Vyatkina, D. V.

PY - 2021/3/4

Y1 - 2021/3/4

N2 - The chapter provides results of the generalization and interpretation of deep geophysical studies. The model of the deep crustal structure is represented by a set of maps, showing the crustal thickness, and a 5400 km-long Geotransect, crossing major tectonic areas of northeastern Eurasia. A set of digital maps covering an area of 50,000,000 km2 is compiled in a single projection and includes the following maps: the Moho depth; the thickness of main crustal units (sedimentary cover and consolidated crust); the anomalous gravity field and anomalous magnetic field used for zoning of the area; crustal types. The Geotransect crosses North-Eastern Eurasia and characterizes the vertical section of the earth’s crust and upper mantle in the passive margin of the Eurasian continent (including submarine elevations of the Arctic Ocean and its shelf part), the active eastern continental margin and extends into the Pacific Plate.

AB - The chapter provides results of the generalization and interpretation of deep geophysical studies. The model of the deep crustal structure is represented by a set of maps, showing the crustal thickness, and a 5400 km-long Geotransect, crossing major tectonic areas of northeastern Eurasia. A set of digital maps covering an area of 50,000,000 km2 is compiled in a single projection and includes the following maps: the Moho depth; the thickness of main crustal units (sedimentary cover and consolidated crust); the anomalous gravity field and anomalous magnetic field used for zoning of the area; crustal types. The Geotransect crosses North-Eastern Eurasia and characterizes the vertical section of the earth’s crust and upper mantle in the passive margin of the Eurasian continent (including submarine elevations of the Arctic Ocean and its shelf part), the active eastern continental margin and extends into the Pacific Plate.

UR - http://www.scopus.com/inward/record.url?scp=85102193738&partnerID=8YFLogxK

U2 - 10.1007/978-3-030-62001-1_2

DO - 10.1007/978-3-030-62001-1_2

M3 - Chapter

AN - SCOPUS:85102193738

T3 - Springer Geology

SP - 33

EP - 61

BT - Tectonics of Asia (Northern, Central and Eastern Asia)

A2 - Petrov, O.V.

A2 - Dong, S.

PB - Springer Nature

ER -

ID: 78301655