期刊
GEOPHYSICAL RESEARCH LETTERS
卷 35, 期 5, 页码 -出版社
AMER GEOPHYSICAL UNION
DOI: 10.1029/2007GL033073
关键词
-
The use of displaced fluvial terrace risers to determine slip rates along strike-slip faults depends on knowing when risers become passive markers. Typically, chronologic constraints from terrace deposits only place bounds on this age; consequent slip rates may be highly uncertain. Along the Kunlun fault, in northeastern Tibet, we demonstrate that consideration of riser degradation can augment terrace chronology and improve the precision of slip-rate estimates. Multiple offset risers and C-14 age determinations from terrace treads yield a narrow range of slip rates of 4.5 +/- 0.5 m/kyr at one site, but permit a wide range of allowable rates (3 - 10 m/kyr) in an adjacent drainage. Using a locally calibrated sediment transport rate of 3.2-5.4 m(2)/ka, we show that riser morphology at this latter site is consistent with degradation since abandonment of the upper terrace tread. Our analysis indicates that slip rates at this site are similar to 5 +/- 2 m/kyr.
作者
我是这篇论文的作者
点击您的名字以认领此论文并将其添加到您的个人资料中。
推荐
暂无数据