Standard

First results and prospects of a new approach to the study of active geologic processes by space and ground instrumental measurements (By the example of kamchatka and the central asian orogenic belt). / Dobretsov, N. L.; Buslov; Vasilevskiy, N. и др.

в: Russian Geology and Geophysics, Том 62, № 1, 4, 01.2021, стр. 44-67.

Результаты исследований: Научные публикации в периодических изданияхстатьяРецензирование

Harvard

APA

Vancouver

Dobretsov NL, Buslov, Vasilevskiy N, Zhmodik S, Kotlyarov V. First results and prospects of a new approach to the study of active geologic processes by space and ground instrumental measurements (By the example of kamchatka and the central asian orogenic belt). Russian Geology and Geophysics. 2021 янв.;62(1):44-67. 4. doi: 10.2113/RGG20204227

Author

BibTeX

@article{88ea0dcea01441ce977a1ed8550a7e7d,
title = "First results and prospects of a new approach to the study of active geologic processes by space and ground instrumental measurements (By the example of kamchatka and the central asian orogenic belt)",
abstract = "The use of satellite-geological information permits generalization of studies of various active geologic processes in a new way. As reference examples, we consider geologic regions extensively covered by research with our contribution. The joint use of satellite images, maps of gravity anomalies, and seismic-tomography data for Kamchatka made it possible to construct 3D models of surficial and deep-seated (depths from 10–50 to 650 km) volcanic structures. For young volcanosedimentary structures of Kamchatka, it is possible to trace the interaction of various processes, from crystallization of magmas in magma chambers to ore and oil formation in calderas. Ancient tectonic structures and superposed Cenozoic deformations in the Tien Shan, Altai, and Baikal regions are clearly displayed in satellite images and on maps of gravity anomalies. The long-range impact of the Indo-Eurasian collision on the Tien Shan, Altai, and Baikal regions was expressed as shearing, which resulted in the most contrasting structures in the zones of junction of regional faults and along the framing of cratonal structures. The active structures of Gorny Altai contain numerous travertines, whose abundance is correlated with seismic activity. The mass formation of methane and gas hydrates in Lake Baikal might be related to mantle plume fluids.",
keywords = "Correlation of geological and geophysical data, Gas hydrates, Gravity maps, Interdisciplinary research, Long-range impact of the Indo-Eurasian collision, Mantle plumes, Paleotravertines, Remote sensing",
author = "Dobretsov, {N. L.} and Buslov and N. Vasilevskiy and S. Zhmodik and V. Kotlyarov",
note = "Funding Information: The work was carried out according to the state tasks of IPGG SB RAS and IGM SB RAS, with the support of the Ministry of science and higher education of the Russian Federation, agreement No. 14.Y26.31.0029, and with the support of RFBR grant No. 18-05-70109. Publisher Copyright: {\textcopyright} 2021, V.S. Sobolev IGM, Siberian Branch of the RAS.",
year = "2021",
month = jan,
doi = "10.2113/RGG20204227",
language = "English",
volume = "62",
pages = "44--67",
journal = "Russian Geology and Geophysics",
issn = "1068-7971",
publisher = "Elsevier Science B.V.",
number = "1",

}

RIS

TY - JOUR

T1 - First results and prospects of a new approach to the study of active geologic processes by space and ground instrumental measurements (By the example of kamchatka and the central asian orogenic belt)

AU - Dobretsov, N. L.

AU - Buslov, null

AU - Vasilevskiy, N.

AU - Zhmodik, S.

AU - Kotlyarov, V.

N1 - Funding Information: The work was carried out according to the state tasks of IPGG SB RAS and IGM SB RAS, with the support of the Ministry of science and higher education of the Russian Federation, agreement No. 14.Y26.31.0029, and with the support of RFBR grant No. 18-05-70109. Publisher Copyright: © 2021, V.S. Sobolev IGM, Siberian Branch of the RAS.

PY - 2021/1

Y1 - 2021/1

N2 - The use of satellite-geological information permits generalization of studies of various active geologic processes in a new way. As reference examples, we consider geologic regions extensively covered by research with our contribution. The joint use of satellite images, maps of gravity anomalies, and seismic-tomography data for Kamchatka made it possible to construct 3D models of surficial and deep-seated (depths from 10–50 to 650 km) volcanic structures. For young volcanosedimentary structures of Kamchatka, it is possible to trace the interaction of various processes, from crystallization of magmas in magma chambers to ore and oil formation in calderas. Ancient tectonic structures and superposed Cenozoic deformations in the Tien Shan, Altai, and Baikal regions are clearly displayed in satellite images and on maps of gravity anomalies. The long-range impact of the Indo-Eurasian collision on the Tien Shan, Altai, and Baikal regions was expressed as shearing, which resulted in the most contrasting structures in the zones of junction of regional faults and along the framing of cratonal structures. The active structures of Gorny Altai contain numerous travertines, whose abundance is correlated with seismic activity. The mass formation of methane and gas hydrates in Lake Baikal might be related to mantle plume fluids.

AB - The use of satellite-geological information permits generalization of studies of various active geologic processes in a new way. As reference examples, we consider geologic regions extensively covered by research with our contribution. The joint use of satellite images, maps of gravity anomalies, and seismic-tomography data for Kamchatka made it possible to construct 3D models of surficial and deep-seated (depths from 10–50 to 650 km) volcanic structures. For young volcanosedimentary structures of Kamchatka, it is possible to trace the interaction of various processes, from crystallization of magmas in magma chambers to ore and oil formation in calderas. Ancient tectonic structures and superposed Cenozoic deformations in the Tien Shan, Altai, and Baikal regions are clearly displayed in satellite images and on maps of gravity anomalies. The long-range impact of the Indo-Eurasian collision on the Tien Shan, Altai, and Baikal regions was expressed as shearing, which resulted in the most contrasting structures in the zones of junction of regional faults and along the framing of cratonal structures. The active structures of Gorny Altai contain numerous travertines, whose abundance is correlated with seismic activity. The mass formation of methane and gas hydrates in Lake Baikal might be related to mantle plume fluids.

KW - Correlation of geological and geophysical data

KW - Gas hydrates

KW - Gravity maps

KW - Interdisciplinary research

KW - Long-range impact of the Indo-Eurasian collision

KW - Mantle plumes

KW - Paleotravertines

KW - Remote sensing

UR - http://www.scopus.com/inward/record.url?scp=85106306585&partnerID=8YFLogxK

UR - https://www.elibrary.ru/item.asp?id=46102010

U2 - 10.2113/RGG20204227

DO - 10.2113/RGG20204227

M3 - Article

AN - SCOPUS:85106306585

VL - 62

SP - 44

EP - 67

JO - Russian Geology and Geophysics

JF - Russian Geology and Geophysics

SN - 1068-7971

IS - 1

M1 - 4

ER -

ID: 34225851