Standard

Magnetotelluric sounding in the Western Transbaikalia segment of the Central Asian fold belt. / Pospeeva, E. V.; Potapov, V. V.; Vitte, L. V.

In: Russian Geology and Geophysics, Vol. 58, No. 1, 01.01.2017, p. 133-147.

Research output: Contribution to journal › Article › peer-review

Harvard

Pospeeva, EV, Potapov, VV & Vitte, LV 2017, 'Magnetotelluric sounding in the Western Transbaikalia segment of the Central Asian fold belt', Russian Geology and Geophysics, vol. 58, no. 1, pp. 133-147. https://doi.org/10.1016/j.rgg.2016.03.014

APA

Pospeeva, E. V., Potapov, V. V., & Vitte, L. V. (2017). Magnetotelluric sounding in the Western Transbaikalia segment of the Central Asian fold belt. Russian Geology and Geophysics, 58(1), 133-147. https://doi.org/10.1016/j.rgg.2016.03.014

Vancouver

Pospeeva EV, Potapov VV, Vitte LV. Magnetotelluric sounding in the Western Transbaikalia segment of the Central Asian fold belt. Russian Geology and Geophysics. 2017 Jan 1;58(1):133-147. doi: 10.1016/j.rgg.2016.03.014

Author

Pospeeva, E. V. ; Potapov, V. V. ; Vitte, L. V. / Magnetotelluric sounding in the Western Transbaikalia segment of the Central Asian fold belt. In: Russian Geology and Geophysics. 2017 ; Vol. 58, No. 1. pp. 133-147.

BibTeX

@article{a04a32c61d4246119c5286e27517f4d1,
title = "Magnetotelluric sounding in the Western Transbaikalia segment of the Central Asian fold belt",
abstract = "This paper presents the results of magnetotelluric (MT) studies performed within the Western Transbaikalia segment of the Central Asian fold belt along the Selenga River delta-Krasnyi Chikoi Village profile. The data are interpreted using the results of recent geological, petrological, geothermal, tectonic, and geochronological studies of the Mongolia-Transbaikalian part of the Central Asian fold belt, including large heterochronous igneous provinces and zones. The studies have shown that the investigated area has a complex geologic and tectonic structure produced by extensive rifting leading to the formation of large crustal blocks and by intense magmatic fluid activity along deep fault zones. The investigated profile is characterized by a combination of blocks with different types of geoelectric section—mountain ranges and intermontane basins separated by long-lived deep fault zones.",
keywords = "deep rift, Earth's crust, electrical resistivity, geoelectric section, granitoids, magmatism, magnetotelluric sounding, mountain range, rift trough, rift zone, Western Transbaikalia, GEODYNAMICS, ZONE, BAIKAL REGION, CRUST",
author = "Pospeeva, {E. V.} and Potapov, {V. V.} and Vitte, {L. V.}",
year = "2017",
month = jan,
day = "1",
doi = "10.1016/j.rgg.2016.03.014",
language = "English",
volume = "58",
pages = "133--147",
journal = "Russian Geology and Geophysics",
issn = "1068-7971",
publisher = "Elsevier Science B.V.",
number = "1",

}

RIS

TY - JOUR

T1 - Magnetotelluric sounding in the Western Transbaikalia segment of the Central Asian fold belt

AU - Pospeeva, E. V.

AU - Potapov, V. V.

AU - Vitte, L. V.

PY - 2017/1/1

Y1 - 2017/1/1

N2 - This paper presents the results of magnetotelluric (MT) studies performed within the Western Transbaikalia segment of the Central Asian fold belt along the Selenga River delta-Krasnyi Chikoi Village profile. The data are interpreted using the results of recent geological, petrological, geothermal, tectonic, and geochronological studies of the Mongolia-Transbaikalian part of the Central Asian fold belt, including large heterochronous igneous provinces and zones. The studies have shown that the investigated area has a complex geologic and tectonic structure produced by extensive rifting leading to the formation of large crustal blocks and by intense magmatic fluid activity along deep fault zones. The investigated profile is characterized by a combination of blocks with different types of geoelectric section—mountain ranges and intermontane basins separated by long-lived deep fault zones.

AB - This paper presents the results of magnetotelluric (MT) studies performed within the Western Transbaikalia segment of the Central Asian fold belt along the Selenga River delta-Krasnyi Chikoi Village profile. The data are interpreted using the results of recent geological, petrological, geothermal, tectonic, and geochronological studies of the Mongolia-Transbaikalian part of the Central Asian fold belt, including large heterochronous igneous provinces and zones. The studies have shown that the investigated area has a complex geologic and tectonic structure produced by extensive rifting leading to the formation of large crustal blocks and by intense magmatic fluid activity along deep fault zones. The investigated profile is characterized by a combination of blocks with different types of geoelectric section—mountain ranges and intermontane basins separated by long-lived deep fault zones.

KW - deep rift

KW - Earth's crust

KW - electrical resistivity

KW - geoelectric section

KW - granitoids

KW - magmatism

KW - magnetotelluric sounding

KW - mountain range

KW - rift trough

KW - rift zone

KW - Western Transbaikalia

KW - GEODYNAMICS

KW - ZONE

KW - BAIKAL REGION

KW - CRUST

UR - http://www.scopus.com/inward/record.url?scp=85013200744&partnerID=8YFLogxK

U2 - 10.1016/j.rgg.2016.03.014

DO - 10.1016/j.rgg.2016.03.014

M3 - Article

AN - SCOPUS:85013200744

VL - 58

SP - 133

EP - 147

JO - Russian Geology and Geophysics

JF - Russian Geology and Geophysics

SN - 1068-7971

IS - 1

ER -

ID: 10309937