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Cenozoic history of topography in southeastern Gorny Altai : thermochronology and resistivity and gravity records. / Dobretsov, N. L.; Buslov, M. M.; Vasilevsky, A. N. et al.

In: Russian Geology and Geophysics, Vol. 57, No. 11, 01.11.2016, p. 1525-1534.

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

Harvard

Dobretsov, NL, Buslov, MM, Vasilevsky, AN, Vetrov, EV & Nevedrova, NN 2016, 'Cenozoic history of topography in southeastern Gorny Altai: thermochronology and resistivity and gravity records', Russian Geology and Geophysics, vol. 57, no. 11, pp. 1525-1534. https://doi.org/10.1016/j.rgg.2016.10.001

APA

Dobretsov, N. L., Buslov, M. M., Vasilevsky, A. N., Vetrov, E. V., & Nevedrova, N. N. (2016). Cenozoic history of topography in southeastern Gorny Altai: thermochronology and resistivity and gravity records. Russian Geology and Geophysics, 57(11), 1525-1534. https://doi.org/10.1016/j.rgg.2016.10.001

Vancouver

Dobretsov NL, Buslov MM, Vasilevsky AN, Vetrov EV, Nevedrova NN. Cenozoic history of topography in southeastern Gorny Altai: thermochronology and resistivity and gravity records. Russian Geology and Geophysics. 2016 Nov 1;57(11):1525-1534. doi: 10.1016/j.rgg.2016.10.001

Author

Dobretsov, N. L. ; Buslov, M. M. ; Vasilevsky, A. N. et al. / Cenozoic history of topography in southeastern Gorny Altai : thermochronology and resistivity and gravity records. In: Russian Geology and Geophysics. 2016 ; Vol. 57, No. 11. pp. 1525-1534.

BibTeX

@article{6a8e4b75eb3b4278b80be17d78ebdf3d,
title = "Cenozoic history of topography in southeastern Gorny Altai: thermochronology and resistivity and gravity records",
abstract = "The Central Asian Orogen was reactivated in the Cenozoic, which gave rise to mountain systems and sedimentary basins, strike-slip and thrust faults, ramps, and rift basins under the far-field effect of the India-Eurasia collision. Pre-Cenozoic structures, as well as the superposed Cenozoic deformation, are traceable in the gravity pattern. Analysis and correlation of stratigraphic, tectonic, geomorphological, and geophysical (resistivity and gravity) data from Gorny Altai and tectonic modeling on the basis of apatite fission-track thermochronology show that vertical motions have been the most active for the past 5 Ma. The uplift and subsidence produced, respectively, the Chulyshman and Ukok Plateaus with high mountains around and the the Kurai-Chuya basin between them. Gravity data suggest the existence of Late Carboniferous, Jurassic, and Cretaceous rocks found in tectonic wedges around the basin at the base of its sedimentary fill.",
keywords = "Gorny Altai, neotectonics, plateau, rampfission-track thermochronology, resistivity and gravity fields, strike-slip fault, thrust",
author = "Dobretsov, {N. L.} and Buslov, {M. M.} and Vasilevsky, {A. N.} and Vetrov, {E. V.} and Nevedrova, {N. N.}",
year = "2016",
month = nov,
day = "1",
doi = "10.1016/j.rgg.2016.10.001",
language = "English",
volume = "57",
pages = "1525--1534",
journal = "Russian Geology and Geophysics",
issn = "1068-7971",
publisher = "Elsevier Science B.V.",
number = "11",

}

RIS

TY - JOUR

T1 - Cenozoic history of topography in southeastern Gorny Altai

T2 - thermochronology and resistivity and gravity records

AU - Dobretsov, N. L.

AU - Buslov, M. M.

AU - Vasilevsky, A. N.

AU - Vetrov, E. V.

AU - Nevedrova, N. N.

PY - 2016/11/1

Y1 - 2016/11/1

N2 - The Central Asian Orogen was reactivated in the Cenozoic, which gave rise to mountain systems and sedimentary basins, strike-slip and thrust faults, ramps, and rift basins under the far-field effect of the India-Eurasia collision. Pre-Cenozoic structures, as well as the superposed Cenozoic deformation, are traceable in the gravity pattern. Analysis and correlation of stratigraphic, tectonic, geomorphological, and geophysical (resistivity and gravity) data from Gorny Altai and tectonic modeling on the basis of apatite fission-track thermochronology show that vertical motions have been the most active for the past 5 Ma. The uplift and subsidence produced, respectively, the Chulyshman and Ukok Plateaus with high mountains around and the the Kurai-Chuya basin between them. Gravity data suggest the existence of Late Carboniferous, Jurassic, and Cretaceous rocks found in tectonic wedges around the basin at the base of its sedimentary fill.

AB - The Central Asian Orogen was reactivated in the Cenozoic, which gave rise to mountain systems and sedimentary basins, strike-slip and thrust faults, ramps, and rift basins under the far-field effect of the India-Eurasia collision. Pre-Cenozoic structures, as well as the superposed Cenozoic deformation, are traceable in the gravity pattern. Analysis and correlation of stratigraphic, tectonic, geomorphological, and geophysical (resistivity and gravity) data from Gorny Altai and tectonic modeling on the basis of apatite fission-track thermochronology show that vertical motions have been the most active for the past 5 Ma. The uplift and subsidence produced, respectively, the Chulyshman and Ukok Plateaus with high mountains around and the the Kurai-Chuya basin between them. Gravity data suggest the existence of Late Carboniferous, Jurassic, and Cretaceous rocks found in tectonic wedges around the basin at the base of its sedimentary fill.

KW - Gorny Altai

KW - neotectonics

KW - plateau

KW - rampfission-track thermochronology

KW - resistivity and gravity fields

KW - strike-slip fault

KW - thrust

UR - http://www.scopus.com/inward/record.url?scp=84995767723&partnerID=8YFLogxK

U2 - 10.1016/j.rgg.2016.10.001

DO - 10.1016/j.rgg.2016.10.001

M3 - Article

AN - SCOPUS:84995767723

VL - 57

SP - 1525

EP - 1534

JO - Russian Geology and Geophysics

JF - Russian Geology and Geophysics

SN - 1068-7971

IS - 11

ER -

ID: 25480277