- journal_title：Geology
- Contributor：Zachary Washburn ; J Ramón Arrowsmith ; Steven L. Forman ; Eric Cowgill ; Wang Xiaofeng ; Zhang Yueqiao ; Chen Zhengle
- Publisher：Geological Society of America
- Date：2001-
- Format：text/html
- Language：en
- Identifier：10.1130/0091-7613(2001)029<1051:LHEHOT>2.0.CO;2
- journal_abbrev：Geology
- issn：0091-7613
- volume：29
- issue：11
- firstpage：1051
The Altyn Tagh fault accommodates sinistral motion between the Tibetan Plateau and the Tarim block within the India-Eurasia collision zone. We used well-preserved evidence for surface-rupturing earthquakes to reconstruct the earthquake history for the central Altyn Tagh fault. We identified three geometric fault segments bounded by left steps and a bend. Geomorphic offsets indicate that the most recent event had maximum surface displacement of ∼5.5 m in the west (38.5°N, 90.0°E), ∼7 m in the central part of our study area, and ∼4 m in the east (38.8°N, 91.5°E). The 14C dates and trench logs of disrupted sediments indicate that these offsets occurred either in a single earthquake with a surface- rupture length >240 km dated as 680 ± 108 yr B.P. or as two events. If there were two events, the westernmost recent event occurred 518 ± 268 yr ago, whereas the eastern event occurred 650 ± 80 yr ago and had a surface rupture length >155 km. We find two events in the past 0.8–2.2 k.y. in the west and two or three events in the east, yielding recurrence intervals of 0.7 ± 0.4 k.y. and 1.1 ± 0.3 k.y., respectively. These recurrence rates for major earthquakes are lower than expected if the long-term fault slip rate is >20 mm/yr. Explanations for the discrepancy include an overdue major earthquake, or accelerated deformation elsewhere in the India-Eurasia orogen.