Quaternary structural and paleo-environmental evolution of the Alpine Fault near Haast, New Zealand, from 2D seismic reflection and gravity data
Author:
Affiliation:
1. Department of Geology, University of Otago, Dunedin, New Zealand
Funder
New Zealand Earthquake Commission
University of Otago
Publisher
Informa UK Limited
Subject
Earth and Planetary Sciences (miscellaneous),Geology,Geophysics
Link
https://www.tandfonline.com/doi/pdf/10.1080/00288306.2018.1544153
Reference70 articles.
1. Mode of crustal shortening adjacent to the Alpine Fault, New Zealand
2. Postglacial (after 20 ka) dextral slip rate of the offshore Alpine fault, New Zealand
3. Rapid creation and destruction of sedimentary basins on mature strike-slip faults: an example from the offshore Alpine Fault, New Zealand
4. Strike-slip structure and sedimentary basins of the southern Alpine Fault, Fiordland, New Zealand
5. Barrell D. 2011. Quaternary glaciers of New Zealand. Developments in Quaternary Science. 15:1047–1064.
Cited by 3 articles. 订阅此论文施引文献 订阅此论文施引文献，注册后可以免费订阅5篇论文的施引文献，订阅后可以查看论文全部施引文献
1. Heterogeneity in Microseismicity and Stress Near Rupture‐Limiting Section Boundaries Along the Late‐Interseismic Alpine Fault;Journal of Geophysical Research: Solid Earth;2022-10
2. Seismic P Wave Velocity Model From 3‐D Surface and Borehole Seismic Data at the Alpine Fault DFDP‐2 Drill Site (Whataroa, New Zealand);Journal of Geophysical Research: Solid Earth;2020-04
3. Fault zone architecture of a large plate-bounding strike-slip fault: a case study from the Alpine Fault, New Zealand;Solid Earth;2020-01-22
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