GSTDTAP  > 地球科学
DOI10.1130/B31907.1
Millennial-scale denudation rates of the Santa Lucia Mountains, California: Implications for landscape evolution in steep, high-relief, coastal mountain ranges
Young, Holly H.; Hilley, George E.
2018-11-01
发表期刊GEOLOGICAL SOCIETY OF AMERICA BULLETIN
ISSN0016-7606
EISSN1943-2674
出版年2018
卷号130页码:1809-1824
文章类型Article
语种英语
国家USA
英文摘要

We used a suite of topographic metrics and cosmogenic Be-10-derived catchment-averaged denudation rates from 18 watersheds to evaluate patterns of millennial-scale erosion of the Santa Lucia Mountains and test the explanatory power of the power-law incision rule for this landscape. Catchment-averaged denudation rates in the study area vary between similar to 0.07 and 0.4 mm/yr, with a single drainage yielding a rate >0.45 mm/yr. Channel steepness ranges from similar to 90 to 390 m for these catchments. We used these observations to test two forms of the power-law incision rule, one incorporating multiple, lithologically dependent erodibilities, and one containing a single erodibility term. Statistical analyses indicated the power-law incision rule provides an improved fit relative to a model that does not relate erosion rate to channel steepness. However, tests comparing both model forms indicate no significant improvement in model fit when using unique erodibility and channel steepness terms for each lithology. Estimates of erodibility coefficients were similar to 10(-6)-10(-5) m(0.2)/yr for all rock types evaluated. Where range asymmetry was most pronounced, watershed divides were identified as mobile by the chi landscape metric, yet we resolved no cross-divide change in erosion rate. Conversely, divides predicted by chi to be close to an equilibrium configuration showed markedly different erosion rates in adjoining basins. These conflicting data sets, considered in conjunction with geomorphic indicators of river capture, may suggest that divide migration occurs in abrupt, punctuated episodes, rather than by gradual migration of divides. Finally, erosion rates measured here are broadly consistent with late Pleistocene uplift rates recorded by geomorphic markers and are a factor of 2-6 lower than previously reported rates of exhumation gauged by apatite helium thermochronology. This suggests that there has been a secular slowing of erosion, and perhaps rock uplift rates, between the Pliocene and today.


领域地球科学
收录类别SCI-E
WOS记录号WOS:000449028300004
WOS关键词SITU-PRODUCED BE-10 ; EROSION RATES ; RIVER INCISION ; COSMOGENIC NUCLIDES ; ANDREAS FAULT ; UPLIFT RATES ; SEDIMENT ; BEDROCK ; NORTHERN ; AL-26
WOS类目Geosciences, Multidisciplinary
WOS研究方向Geology
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文献类型期刊论文
条目标识符http://119.78.100.173/C666/handle/2XK7JSWQ/24557
专题地球科学
作者单位Stanford Univ, Dept Geol Sci, Braun Hall,Bldg 320,450 Serra Mall, Stanford, CA 94305 USA
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Young, Holly H.,Hilley, George E.. Millennial-scale denudation rates of the Santa Lucia Mountains, California: Implications for landscape evolution in steep, high-relief, coastal mountain ranges[J]. GEOLOGICAL SOCIETY OF AMERICA BULLETIN,2018,130:1809-1824.
APA Young, Holly H.,&Hilley, George E..(2018).Millennial-scale denudation rates of the Santa Lucia Mountains, California: Implications for landscape evolution in steep, high-relief, coastal mountain ranges.GEOLOGICAL SOCIETY OF AMERICA BULLETIN,130,1809-1824.
MLA Young, Holly H.,et al."Millennial-scale denudation rates of the Santa Lucia Mountains, California: Implications for landscape evolution in steep, high-relief, coastal mountain ranges".GEOLOGICAL SOCIETY OF AMERICA BULLETIN 130(2018):1809-1824.
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