Publication 143
Crustal structure and rheology of the Longmenshan and Wenchuan
Mw 7.9 earthquake epicentral area from magnetotelluric data
Guoze Zhao, Martyn J. Unsworth, Yan Zhan, Lifeng Wang, Xiaobin Chen, Alan G. Jones, Ji Tang, Qibin Xiao,
Jijun Wang, Juntao Cai, Tao Li, Yanzhao Wang, and Jihong Zhang
Abstract
The Longmenshan forms the eastern margin of the Tibetan Plateau adjacent to the Sichuan
Basin. This range is anomalous because it formed despite low convergence and slip rates and
without the development of a foreland basin. The devastating A.D. 2008 Wenchuan earthquake
(Mw = 7.9) has renewed debate about the tectonics of the Longmenshan. A magnetotelluric
(MT) study was undertaken subsequent to the earthquake to investigate the crustal structure
of the Longmenshan, and inversion of the data reveals a low-resistivity (high-conductivity)
layer at a depth of ~20 km beneath the eastern Tibetan Plateau that terminates ~25 km west
of the Wenchuan-Maoxian fault. Its electrical properties are consistent with it being fl uid-rich
and mechanically weak. Beneath the Longmenshan and Sichuan Basin, a high-resistivity zone
extends through the entire crust, but with a zone of low resistivity in the vicinity of the Wenchuan
hypocenter. We show that the MT data, combined with other geological and geophysical
observations, support geodynamic models for the uplift of eastern Tibet being caused by southeast-
directed crustal fl ow that is blocked by stable lithosphere beneath the Sichuan Basin and
Longmenshan, leading to infl ation of the Songpan-Ganzi terrane. This rigid high-resistivity
backstop not only provided a block to fl ow, but also may have accumulated stress prior to the
earthquake. The MT observations provide new insights into the generation of the Wenchuan
earthquake, which occurred in a region with low convergence rates prior to the earthquake.
Source
Geology, , in press, doi:10.1130/G33703.1. [PDF]
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Alan G Jones / 08 November 2012 /
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