Mobility, Thickness, and Hydraulic Diffusivity of the Slow‐Moving Monroe Landslide in California Revealed by L‐Band Satellite Radar Interferometry-Reference-Cited by-同舟云学术

Mobility, Thickness, and Hydraulic Diffusivity of the Slow‐Moving Monroe Landslide in California Revealed by L‐Band Satellite Radar Interferometry

Author:

Hu Xie¹²³^ORCID,Bürgmann Roland²³^ORCID,Lu Zhong¹^ORCID,Handwerger Alexander L.⁴^ORCID,Wang Teng⁵⁶^ORCID,Miao Runze³

Affiliation:

1. Roy M. Huffington Department of Earth Sciences Southern Methodist University Dallas CA USA

2. Berkeley Seismological Laboratory University of California Berkeley CA USA

3. Department of Earth and Planetary Science University of California Berkeley CA USA

4. Jet Propulsion Laboratory California Institute of Technology Pasadena CA USA

5. Earth Observatory of Singapore Nanyang Technological University Singapore

6. Now at School of Earth and Space Sciences, Peking University Beijing China

Funder

U.S. Forest Service

National Aeronautics and Space Administration

Publisher

American Geophysical Union (AGU)

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Link

Reference49 articles.

3. California Geological Survey(2010).Geologic map of California California Department of Conservation.

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