Highly Variable Latest Pleistocene‐Holocene Incremental Slip Rates on the Awatere Fault at Saxton River, South Island, New Zealand, Revealed by Lidar Mapping and Luminescence Dating-Reference-Cited by-同舟云学术

Highly Variable Latest Pleistocene‐Holocene Incremental Slip Rates on the Awatere Fault at Saxton River, South Island, New Zealand, Revealed by Lidar Mapping and Luminescence Dating

Published:2017-11-18 Issue:22 Volume:44 Page:
ISSN:0094-8276
Container-title:Geophysical Research Letters
language:en
Short-container-title:Geophys. Res. Lett.

Author:

Zinke Robert¹^ORCID,Dolan James F.¹^ORCID,Rhodes Edward J.²^ORCID,Van Dissen Russ³^ORCID,McGuire Christopher P.⁴^ORCID

Affiliation:

1. Department of Earth Sciences University of Southern California Los Angeles CA USA

2. Department of Geography University of Sheffield Western Bank UK

3. GNS Science Lower Hutt New Zealand

4. Department of Earth, Planetary, and Space Sciences University of California Los Angeles CA USA

Funder

National Science Foundation

Georgian National Science Foundation

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1002/2017GL075048

Reference45 articles.

1. Accelerated Plate Tectonics

2. Accelerating slip rates on the Puente Hills blind thrust fault system beneath metropolitan Los Angeles, California, USA

3. Development of the Radiocarbon Calibration Program

4. Adjustments by the Charwell River, New Zealand, to uplift and climatic changes

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