Assessing the activity of faults in continental interiors: Palaeoseismic insights from SE Kazakhstan

Grützner, C. and Carson, E. and Walker, R.T. and Rhodes, E.J. and Mukambayev, A. and Mackenzie, D. and Elliott, J.R. and Campbell, G. E. and Abdrakhmatov, K. (2017) Assessing the activity of faults in continental interiors: Palaeoseismic insights from SE Kazakhstan. Earth and Planetary Science Letters, 459. pp. 93-104. ISSN 0012821X DOI 10.1016/j.epsl.2016.11.025

Preview	Text 1-s2.0-S0012821X16306598-main.pdf - Published Version Available under License Creative Commons Attribution. Download (6MB) | Preview
Preview	Image 1-s2.0-S0012821X16306598-mmc1.jpg - Supplemental Material Download (62kB) | Preview
Preview	Image 1-s2.0-S0012821X16306598-mmc2.jpg - Supplemental Material Download (59kB) | Preview
Preview	Image 1-s2.0-S0012821X16306598-mmc3.jpg - Supplemental Material Download (56kB) | Preview
Preview	Image 1-s2.0-S0012821X16306598-mmc4.jpg - Supplemental Material Download (58kB) | Preview
Preview	Image 1-s2.0-S0012821X16306598-mmc5.jpg - Published Version Download (229kB) | Preview
Preview	Image 1-s2.0-S0012821X16306598-mmc6.jpg - Supplemental Material Download (157kB) | Preview
Preview	Image 1-s2.0-S0012821X16306598-mmc7.jpg - Supplemental Material Download (164kB) | Preview
Preview	Image 1-s2.0-S0012821X16306598-mmc8.jpg - Updated Version Download (176kB) | Preview
Preview	Image 1-s2.0-S0012821X16306598-mmc9.jpg - Supplemental Material Download (180kB) | Preview
Preview	Image 1-s2.0-S0012821X16306598-mmc10.jpg - Supplemental Material Download (135kB) | Preview
	Text mmc11.docx - Supplemental Material Download (20kB)
	Other (GoogleEarth kml file) mmc12.kml - Supplemental Material Download (4MB)

Abstract

The presence of fault scarps is a first-order criterion for identifying active faults. Yet the preservation of these features depends on the recurrence interval between surface rupturing events, combined with the rates of erosional and depositional processes that act on the landscape. Within arid continental interiors single earthquake scarps can be preserved for thousands of years, and yet the interval between surface ruptures on faults in these regions may be much longer, such that the lack of evidence for surface faulting in the morphology may not preclude activity on those faults. In this study we investigate the 50 km-long ‘Toraigyr’ thrust fault in the northern Tien Shan. From palaeoseismological trenching we show that two surface rupturing earthquakes occurred in the last 39.9±2.7 ka39.9±2.7 ka BP, but only the most recent event (3.15–3.6 ka BP) has a clear morphological expression. We conclude that a landscape reset took place in between the two events, likely as a consequence of the climatic change at the end of the last glacial maximum. These findings illustrate that in the Tien Shan evidence for the most recent active faulting can be easily obliterated by climatic processes due to the long earthquake recurrence intervals. Our results illustrate the problems related to the assessment of active tectonic deformation and seismic hazard assessments in continental interior settings.

Item Type:	Article
Uncontrolled Keywords:	2016AREP; IA72; bull
Subjects:	02 - Geodynamics, Geophysics and Tectonics
Divisions:	02 - Geodynamics, Geophysics and Tectonics 07 - Gold Open Access
Journal or Publication Title:	Earth and Planetary Science Letters
Volume:	459
Page Range:	pp. 93-104
Identification Number:	10.1016/j.epsl.2016.11.025
Depositing User:	Sarah Humbert
Date Deposited:	17 Feb 2017 17:09
Last Modified:	03 Mar 2017 11:47
URI:	http://eprints.esc.cam.ac.uk/id/eprint/3823

Actions (login required)

View Item