In:
Tectonics, American Geophysical Union (AGU), Vol. 40, No. 12 ( 2021-12)
Abstract:
The Xigeda fault is active in the Holocene and slips left‐laterally at a rate of 0.8–1.6 mm/yr with a thrust component The Xigeda fault is the seismogenic structure of the 1732 CE earthquake whose magnitude is reevaluated to range from 7.0 to 7.5 The Xigeda‐Yuanmou fault absorbs some slip on the boundary fault of the Sichuan‐Yunnan block and accommodates the intra‐block deformation
Type of Medium:
Online Resource
ISSN:
0278-7407
,
1944-9194
DOI:
10.1029/2021TC007056
Language:
English
Publisher:
American Geophysical Union (AGU)
Publication Date:
2021
detail.hit.zdb_id:
2013221-9
detail.hit.zdb_id:
780264-X
SSG:
16,13
SSG:
13
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