Zobrazeno 1 - 10
of 49
pro vyhledávání: '"G. Ian Alsop"'
Publikováno v:
Frontiers in Earth Science, Vol 10 (2022)
Thrust collision zones with low slip rates along the plate boundary are significant areas of stress accumulation and prone to develop more destructive earthquakes with longer recurrence intervals. Such regions are often classified as low seismic risk
Externí odkaz:
https://doaj.org/article/15d9a4285b2f410a9df16c89e4964332
Autor:
Yin Lu, Nicolas Waldmann, Nadav Wetzler, Jasper Moernaut, Revital Bookman, Glenn P. Biasi, Michael Strasser, Xiaomin Fang, Aurélia Hubert-Ferrari, G. Ian Alsop, Amotz Agnon, Shmuel Marco
Sharp changes in lithology and increases in grain size and sedimentation rate of sedimentary sequences from tectonically active basins are often used to indicate regional neotectonic activity. However, these conventional methods have been challenged
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::928c4aa3aeee77e7e710e7b0ab15a600
https://doi.org/10.5194/egusphere-egu22-1439
https://doi.org/10.5194/egusphere-egu22-1439
Publikováno v:
Geological Society, London, Special Publications. 493:273-286
We are very grateful to companies sponsoring Phase 3 of the Sand InjectionResearch Group (SIRG). We acknowledge the continuing help provided by the Bureau of Land Management (BLM) in California.
Autor:
Robert W. H. Butler, G. Ian Alsop
Publikováno v:
Journal of the Geological Society. 177:443-446
The interpretation of the Stac Fada Member of the Stoer Group of NW Scotland as a proximal ejecta blanket of late Mesoproterozoic age (Amor et al. 2008) has led to the search for the impact crater from which it originated. One prominent suggestion ha
Autor:
Benjamin Charles Kneller, G. Ian Alsop, Matheus S. Sobiesiak, Victoria Valdez Buso, Juan Pablo Milana
Publikováno v:
Submarine Landslides
Autor:
Shmuel Marco, Yin Lu, Revital Bookman, Michael Strasser, Nicolas Waldmann, Amotz Agnon, Aurélia Hubert-Ferrari, Jasper Moernaut, G. Ian Alsop
Publikováno v:
Geophysical Research Letters. 48
Acknowledgments The authors appreciate the editor L. Flesch for handling our manuscript, Ed Pope and Sebastian Cardona for constructive reviews. This research was supported by the Austrian Science Fund (FWF): M 2817 to Y. Lu and P30285-N34 to J. Moer
Publikováno v:
Marine and Petroleum Geology. 98:629-639
Erosion of the seafloor is often interpreted to be the result of turbidity currents and reflects their frictional and non-cohesive nature. However, evidence of the interaction between sediment gravity-flows and the substrate forming the sea floor has
Publikováno v:
Geophysical Research Letters. 48
Acknowledgments This research was inspired by Prof. Lin Ding's comments on the doctoral thesis proposal of Yin Lu in May 2014 at the Institute of Tibetan Plateau Research, China. We thank Profs. Todd Ehlers, Erwin Appel, and Oliver Friedrich for frui
Autor:
Amotz Agnon, Shmuel Marco, Nadav Wetzler, Jasper Moernaut, Nicolas Waldmann, Aurélia Hubert-Ferrari, G. Ian Alsop, Michael Strasser, Yin Lu, Revital Bookman
Seismogenic turbidites are widely used for geohazard assessment. The use of turbidites as an earthquake indicator requires a clear demonstration that an earthquake, rather than non-seismic factors, is the most plausible trigger. The seismic origin is
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::fb180682d13ba975909c0685c6c3320b
https://doi.org/10.5194/egusphere-egu21-11057
https://doi.org/10.5194/egusphere-egu21-11057