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DOI10.1126/science.1213778
Near-field deformation from the El Mayor-Cucapah earthquake revealed by differential LIDAR
Oskin M.E.; Arrowsmith J.R.; Corona A.H.; Elliott A.J.; Fletcher J.M.; Fielding E.J.; Gold P.O.; Garcia J.J.G.; Hudnut K.W.; Liu-Zeng J.; Teran O.J.
发表日期2012
ISSN0036-8075
起始页码702
结束页码705
卷号335期号:6069
英文摘要Large [moment magnitude (Mw) ≥ 7] continental earthquakes often generate complex, multifault ruptures linked by enigmatic zones of distributed deformation. Here, we report the collection and results of a high-resolution (≥nine returns per square meter) airborne light detection and ranging (LIDAR) topographic survey of the 2010 Mw 7.2 El Mayor-Cucapah earthquake that produced a 120-kilometer-long multifault rupture through northernmost Baja California, Mexico. This differential LIDAR survey completely captures an earthquake surface rupture in a sparsely vegetated region with pre-earthquake lower-resolution (5-meter-pixel) LIDAR data. The postevent survey reveals numerous surface ruptures, including previously undocumented blind faults within thick sediments of the Colorado River delta. Differential elevation changes show distributed, kilometer-scale bending strains as large as ∼103 microstrains in response to slip along discontinuous faults cutting crystalline bedrock of the Sierra Cucapah.
英文关键词bedrock; bending; crystalline rock; data set; deformation; deltaic deposit; earthquake event; earthquake rupture; geological survey; lidar; pixel; slip; topographic mapping; vegetation structure; article; differential light detection and ranging; earthquake; ellipsometry; Mexico; priority journal; sediment; topography; United States; Baja California [(STT) Mexico]; Colorado Delta; Mexico [North America]
语种英语
来源期刊Science
文献类型期刊论文
条目标识符http://gcip.llas.ac.cn/handle/2XKMVOVA/244958
作者单位Department of Geology, University of California, Davis, 1 Shields Avenue, Davis, CA 95618, United States; School of Earth and Space Exploration, Arizona State University, Tempe, AZ 85287-1404, United States; Centro de Investigación Científica Y de Educación Superior de Ensenada, Carretera Ensenada-Tijuana no. 3918, Zona Playitas, C.P. 22860, Ensenada, Baja California, Mexico; Jet Propulsion Laboratory, California Institute of Technology, 4800 Oak Grove Drive, Pasadena, CA 91109, United States; United States Geological Survey, 525 South Wilson Avenue, Pasadena, CA 91106, United States; National Key Laboratory of Earthquake Dynamics, Institute of Geology, China Earthquake Administration, 1# Huayanli, Dewai Avenue, Beijing 100029, China
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Oskin M.E.,Arrowsmith J.R.,Corona A.H.,et al. Near-field deformation from the El Mayor-Cucapah earthquake revealed by differential LIDAR[J],2012,335(6069).
APA Oskin M.E..,Arrowsmith J.R..,Corona A.H..,Elliott A.J..,Fletcher J.M..,...&Teran O.J..(2012).Near-field deformation from the El Mayor-Cucapah earthquake revealed by differential LIDAR.Science,335(6069).
MLA Oskin M.E.,et al."Near-field deformation from the El Mayor-Cucapah earthquake revealed by differential LIDAR".Science 335.6069(2012).
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