Abstracts - faqs.org

Abstracts

Earth sciences

Search abstracts:
Abstracts » Earth sciences

Structure and evolution of the Magnitogorsk forearc basin: identifying upper crustal processes during arc-continent collision in the southern Urals

Article Abstract:

Research into the structure and evolution of the Magnitogorsk forearc in the southern Urals is presented. This volcanic arc can be divided into the Irendyk and east Magnitogorsk volcanic fronts. These were active during intraoceanic island arc creation and during arc-continent collision respectively.

Author: Brown, D., Alvarez-Marron, J., Perez-Estaun, A., Puchkov, V., Gorozhanina, Y., Ayarza, P.
Publisher: American Geophysical Union
Publication Name: Tectonics
Subject: Earth sciences
ISSN: 0278-7407
Year: 2001
Island arcs, Magnitogorsk, Russia

User Contributions:

Comment about this article or add new information about this topic:

CAPTCHA


Geometric and kinematic evolution of the foreland thrust and fold belt in the southern Urals

Article Abstract:

New structural mapping the southern Urals of bashkortostan is presented. The first balanced and restored cross section through the foreland thrust and fold belt from the allochthonous Zilair Nappe over the paleozoic platform provides information on the structure and kinematic evolution and gives quantitative estimates of fault displacement and shortening.

Author: Brown, D., Perez-Estaun, A., Puchkov, V., Gorozhanina, Y., Alverez-Marron, J., Baryshev, V.
Publisher: American Geophysical Union
Publication Name: Tectonics
Subject: Earth sciences
ISSN: 0278-7407
Year: 1997
Thrust faults (Geology), Thrust faults

User Contributions:

Comment about this article or add new information about this topic:

CAPTCHA


Crustal-scale structure and evolution of an arc-continent collision zone in the southern Urals, Russia

Article Abstract:

Three reflection seismic profiles have been combined with outcropping field geology to examine the crustal-scale structure and evolution of an arc-continent collision zone in southern Urals, Russia. Results reveal that the accretionary complex is very reflective and that it is a thrust stack made of subducted continental shelf and rise material. Results also show that arc erosion, uplift and collision is associated with Late Devonian volcaniclastic sediment deposits of the Zilair formation.

Author: Brown, D., Alvarez-Marron, J., Perez-Estaun, A., Juhlin, C., Oslianski, A.
Publisher: American Geophysical Union
Publication Name: Tectonics
Subject: Earth sciences
ISSN: 0278-7407
Year: 1998
Usage, Earth, Crust (Geology), Seismic reflection method, Seismic reflection surveying, Continents

User Contributions:

Comment about this article or add new information about this topic:

CAPTCHA


Subjects list: Research, Natural history, Ural Mountains region
Similar abstracts:
  • Abstracts: Evolution of the late Paleozoic accretionary complex and overlying forearc-magmatic arc, south central Chile (38 degrees-41 degrees S): Constraints for the tectonic setting along the southwestern margin of Gondwana
  • Abstracts: Cenozoic transtension along the Transantarctic Mountains-west Antarctic rift boundary, southern Victoria Land, Antarctica
  • Abstracts: Rheology predictions across the western Carpathians, Bohemian massif, and the Pannonian basin: Implications for tectonic scenarios
This website is not affiliated with document authors or copyright owners. This page is provided for informational purposes only. Unintentional errors are possible.
Some parts © 2025 Advameg, Inc.