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The tectonic evolution of the Chuya-Kurai zone (Siberian Altai mountains) by means of multi-method chronology

Willem Vandoorne UGent, Johan De Grave UGent, Stijn Glorie UGent and Peter Van den haute UGent (2011) GEOLOGICA BELGICA. 14(3-4). p.289-292
abstract
The Phanerozoic tectonic evolution of the Chuya-Kurai zone was studied by means of zircon U/Pb-dating, apatite fission track (AFT) and apatite (U-Th)/He (AHe) thermochronology performed on basement rocks. Our results suggest that multiple magmatic episodes during the Paleozoic, related to the accretion-collision tectonics in Central Asia, affected our study area. Mesozoic and Cenozoic basement cooling events are interpreted as periods of tectonic reactivation. A new tectonic model for Late Cenozoic evolution of the Chuya-Kurai zone is proposed.
Please use this url to cite or link to this publication:
author
organization
year
type
journalArticle (original)
publication status
published
subject
keyword
intracontinental reactivation, tectonic denudation, thermal history, geochronology, Central Asian Orogenic Belt, FISSION-TRACK THERMOCHRONOLOGY, ASIAN OROGENIC BELT, ZIRCON U-PB, CHINESE ALTAI, APATITE, GEODYNAMICS, KAZAKSTAN, HISTORY, SYSTEM, REGION
journal title
GEOLOGICA BELGICA
Geol. Belg.
volume
14
issue
3-4
pages
289 - 292
Web of Science type
Article
Web of Science id
000297182400012
JCR category
GEOLOGY
JCR impact factor
0.773 (2011)
JCR rank
28/46 (2011)
JCR quartile
3 (2011)
ISSN
1374-8505
language
English
UGent publication?
yes
classification
A1
copyright statement
I have retained and own the full copyright for this publication
id
1960683
handle
http://hdl.handle.net/1854/LU-1960683
alternative location
http://popups.ulg.ac.be/Geol/docannexe.php?id=3458
date created
2011-12-06 13:15:47
date last changed
2012-10-19 14:26:34
@article{1960683,
  abstract     = {The Phanerozoic tectonic evolution of the Chuya-Kurai zone was studied by means of zircon U/Pb-dating, apatite fission track (AFT) and apatite (U-Th)/He (AHe) thermochronology performed on basement rocks. Our results suggest that multiple magmatic episodes during the Paleozoic, related to the accretion-collision tectonics in Central Asia, affected our study area. Mesozoic and Cenozoic basement cooling events are interpreted as periods of tectonic reactivation. A new tectonic model for Late Cenozoic evolution of the Chuya-Kurai zone is proposed.},
  author       = {Vandoorne, Willem and De Grave, Johan and Glorie, Stijn and Van den haute, Peter},
  issn         = {1374-8505},
  journal      = {GEOLOGICA BELGICA},
  keyword      = {intracontinental reactivation,tectonic denudation,thermal history,geochronology,Central Asian Orogenic Belt,FISSION-TRACK THERMOCHRONOLOGY,ASIAN OROGENIC BELT,ZIRCON U-PB,CHINESE ALTAI,APATITE,GEODYNAMICS,KAZAKSTAN,HISTORY,SYSTEM,REGION},
  language     = {eng},
  number       = {3-4},
  pages        = {289--292},
  title        = {The tectonic evolution of the Chuya-Kurai zone (Siberian Altai mountains) by means of multi-method chronology},
  url          = {http://popups.ulg.ac.be/Geol/docannexe.php?id=3458},
  volume       = {14},
  year         = {2011},
}

Chicago
Vandoorne, Willem, Johan De Grave, Stijn Glorie, and Peter Van den haute. 2011. “The Tectonic Evolution of the Chuya-Kurai Zone (Siberian Altai Mountains) by Means of Multi-method Chronology.” Geologica Belgica 14 (3-4): 289–292.
APA
Vandoorne, W., De Grave, J., Glorie, S., & Van den haute, P. (2011). The tectonic evolution of the Chuya-Kurai zone (Siberian Altai mountains) by means of multi-method chronology. GEOLOGICA BELGICA, 14(3-4), 289–292.
Vancouver
1.
Vandoorne W, De Grave J, Glorie S, Van den haute P. The tectonic evolution of the Chuya-Kurai zone (Siberian Altai mountains) by means of multi-method chronology. GEOLOGICA BELGICA. 2011;14(3-4):289–92.
MLA
Vandoorne, Willem, Johan De Grave, Stijn Glorie, et al. “The Tectonic Evolution of the Chuya-Kurai Zone (Siberian Altai Mountains) by Means of Multi-method Chronology.” GEOLOGICA BELGICA 14.3-4 (2011): 289–292. Print.