Schmidt hammer and terrestrial laser scanning (TLS) used to detect single‐event displacements on the Pleasant Valley fault (Nevada, USA)-Reference-Cited by-同舟云学术

Schmidt hammer and terrestrial laser scanning (TLS) used to detect single‐event displacements on the Pleasant Valley fault (Nevada, USA)

Published:2019-12-22 Issue:2 Volume:45 Page:473-483
ISSN:0197-9337
Container-title:Earth Surface Processes and Landforms
language:en
Short-container-title:Earth Surf. Process. Landforms

Author:

Stahl Timothy¹^ORCID,Tye Alexander²^ORCID

Affiliation:

1. Department of Geological Sciences University of Canterbury Christchurch New Zealand

2. Department of Earth and Environmental Sciences University of Michigan Ann Arbor Michigan USA

Funder

Division of Earth Sciences

Publisher

Wiley

Subject

Earth and Planetary Sciences (miscellaneous),Earth-Surface Processes,Geography, Planning and Development

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1002/esp.4748

Reference49 articles.

1. AndersonRE MachetteMN.2000.Fault number 1136c Pleasant Valley fault zone Pearce section. InQuaternary Fault and Fold Database of the United States. US Geological Survey: Reston VA. Available:https://earthquakes.usgs.gov/hazards/qfaults(last accessed 2 November 2018).

3. Post-glacial slip history of the Sparta fault (Greece) determined by36Cl cosmogenic dating: Evidence for non-periodic earthquakes

4. Cosmogenic Nuclide Dating of Earthquakes, Faults, and Toppled Blocks

5. BenedictJB.1985.Arapaho Pass: glacial geology and archaeology at the crest of the Colorado Front Range.Research Report No. 3. Center for Mountain Arachaeology: Ward CO.

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