Knowledge Resource Center for Ecological Environment in Arid Area
DOI | 10.1130/B26123.1 |
Slip rate of the western Garlock fault, at Clark Wash, near Lone Tree Canyon, Mojave Desert, California | |
McGill, Sally F.1; Wells, Stephen G.2; Fortner, Sarah K.4; Kuzma, Heidi Anderson1; Mcgij, John D.3 | |
通讯作者 | McGill, Sally F. |
来源期刊 | GEOLOGICAL SOCIETY OF AMERICA BULLETIN
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ISSN | 0016-7606 |
EISSN | 1943-2674 |
出版年 | 2009 |
卷号 | 121期号:3-4页码:536-554 |
英文摘要 | The precise tectonic role of the left-lateral Garlock fault in southern California has been controversial. Three proposed tectonic models yield significantly different predictions for the slip rate, history, orientation, and total bedrock offset as a function of distance along strike. In an effort to test these models, we present the first slip-rate estimate for the western Garlock fault that is constrained by radiocarbon dating. A channel (referred to here as Clark Wash) incised into a Latest Pleistocene alluvial fan has been left-laterally offset at least 66 +/- 6 m and no more than 100 m across the western Garlock fault, indicating a left-lateral slip rate of 7.6 mm/yr (95% confidence interval of 5.3-10.7 mm/yr) using dendrochronologically calibrated radiocarbon dates. The timing of aggradational events on the Clark Wash fan corresponds closely to what has been documented elsewhere in the Mojave Desert, suggesting that much of this activity has been climatically controlled. The range-front fault, located a few hundred meters northwest of the Garlock fault, has probably acted primarily as a normal fault, with a Holocene rate of dip-slip of 0.4-0.7 mm/yr. The record of prehistoric earthquakes on the Garlock fault at this site, though quite possibly incomplete, suggests a longer interseismic interval (1200-2700 yr) for the western Garlock fault than for the central Garlock fault. The relatively high slip rate determined here indicates that the western and central segments of the Garlock fault show similar rates of movement that are somewhat faster than rates inferred from geodetic data. The high rate of motion on the western Garlock fault is most consistent with a model in which the western Garlock fault acts as a conjugate shear to the San Andreas fault. Other mechanisms, involving extension north of the Garlock fault and block rotation at the eastern end of the fault may be relevant to the central and eastern sections of the fault, but they cannot explain a high rate of slip on the western Garlock fault. |
类型 | Article |
语种 | 英语 |
国家 | USA |
收录类别 | SCI-E |
WOS记录号 | WOS:000262964700013 |
WOS关键词 | TRANSIENT STRAIN ACCUMULATION ; EASTERN CALIFORNIA ; SHEAR ZONE ; SOUTHERN-CALIFORNIA ; SIERRA-NEVADA ; UNITED-STATES ; EXTENSIONAL TECTONICS ; AGE CALIBRATION ; NORTH-AMERICA ; OWENS-VALLEY |
WOS类目 | Geosciences, Multidisciplinary |
WOS研究方向 | Geology |
来源机构 | Desert Research Institute |
资源类型 | 期刊论文 |
条目标识符 | http://119.78.100.177/qdio/handle/2XILL650/160767 |
作者单位 | 1.Calif State Univ San Bernardino, Dept Geol Sci, San Bernardino, CA 92407 USA; 2.Univ Nevada, Desert Res Inst, Reno, NV 89506 USA; 3.Calif State Univ San Bernardino, Dept Phys, San Bernardino, CA 92407 USA; 4.Univ Wisconsin, Dept Geol & Geophys, Madison, WI 53706 USA |
推荐引用方式 GB/T 7714 | McGill, Sally F.,Wells, Stephen G.,Fortner, Sarah K.,et al. Slip rate of the western Garlock fault, at Clark Wash, near Lone Tree Canyon, Mojave Desert, California[J]. Desert Research Institute,2009,121(3-4):536-554. |
APA | McGill, Sally F.,Wells, Stephen G.,Fortner, Sarah K.,Kuzma, Heidi Anderson,&Mcgij, John D..(2009).Slip rate of the western Garlock fault, at Clark Wash, near Lone Tree Canyon, Mojave Desert, California.GEOLOGICAL SOCIETY OF AMERICA BULLETIN,121(3-4),536-554. |
MLA | McGill, Sally F.,et al."Slip rate of the western Garlock fault, at Clark Wash, near Lone Tree Canyon, Mojave Desert, California".GEOLOGICAL SOCIETY OF AMERICA BULLETIN 121.3-4(2009):536-554. |
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