Article (Scientific journals)
Mechanisms of active folding of the landscape (Southern Tianshan, China)
Hubert, Aurelia; Suppe, J.; Gonzales-Mieres, R.
2007In Journal of Geophysical Research, 112 (10.1029/2006JB004362)
Peer Reviewed verified by ORBi
 

Files


Full Text
JGR06_HubertFerrari.pdf
Publisher postprint (8.6 MB)
Download

All documents in ORBi are protected by a user license.

Send to



Details



Keywords :
Tianshan; shortening; seismic profiles; geomorphology
Abstract :
[en] We explore the kinematic mechanisms of active large-scale folding, based on analysis of two adjacent major anticlines in Tian Shan (central Asia) that share an acceleration of shortening rate leading to topographic emergence and folded geomorphic surfaces. Their folding mechanisms are fundamentally different. Yakeng anticline is a gentle pure shear detachment fold with 1200 m of shortening and a well-constrained history of growth beginning at 5.5 Ma with an order-of-magnitude increase in shortening rate from 0.16 to 1.2–1.6 mm/yr at 0.16–0.21 Ma. The shape of the deformed topographic surface and of subsurface horizons deposited during deformation is a linearly proportional image at reduced amplitude of the deeper structure, which shows that instantaneous uplift rates have been pointwise linearly proportional to the current finite fold amplitude. In contrast, Quilitak anticline is a complex fault bend fold with uplift rates proportional to the sine of the fault dip, showing discontinuities in uplift rate across active axial surfaces. The 10- to 20-km-wide anticline is topographically emergent only in a central 5- to 7-km-wide mountainous uplift, the abrupt southern edge of which is marked by 600- to 700-m-high triangular facets that result from active folding of a pediment across an active axial surface. The giant facets are shown to form by kink band migration and record postemergence deformation since an order-of-magnitude acceleration in shortening rate from 0.6 t 4–5 mm/yr, apparently contemporaneous with Yakeng. Sections logged across the active 115-m-wide hinge zone show that recent strata provide a bed- by-bed record of fold scarp growth, which is quantitatively deciphered by fitting bed shapes to a finite width kink band migration model.
Disciplines :
Earth sciences & physical geography
Author, co-author :
Hubert, Aurelia  ;  Université de Liège - ULiège > Département de géographie > Géomorphologie
Suppe, J.
Gonzales-Mieres, R.
Language :
English
Title :
Mechanisms of active folding of the landscape (Southern Tianshan, China)
Publication date :
2007
Journal title :
Journal of Geophysical Research
ISSN :
0148-0227
eISSN :
2156-2202
Publisher :
American Geophysical Union (AGU), Washington, United States - District of Columbia
Special issue title :
Issue B3
Volume :
112
Issue :
10.1029/2006JB004362
Peer reviewed :
Peer Reviewed verified by ORBi
Available on ORBi :
since 26 November 2010

Statistics


Number of views
97 (10 by ULiège)
Number of downloads
314 (2 by ULiège)

Scopus citations®
 
196
Scopus citations®
without self-citations
180
OpenCitations
 
111

Bibliography


Similar publications



Contact ORBi