Zobrazeno 1 - 10
of 25
pro vyhledávání: '"J. Ramon Arrowsmith"'
Autor:
Chelsea Scott, Albert Kottke, Christopher Madugo, J. Ramon Arrowsmith, Rachel Adam, Malinda Zuckerman
Publikováno v:
Geophysical Research Letters, Vol 51, Iss 16, Pp n/a-n/a (2024)
Abstract Tectonic landforms and surficial lithologic age are essential data for producing quality late Quaternary fault maps and predicting coseismic fault rupture location before an earthquake. However, we lack a clear understanding of the relations
Externí odkaz:
https://doaj.org/article/08ae501502944a57bc3689b66b285660
Autor:
Alessandro Gattuso, Costanza Bonadonna, Corine Frischknecht, Sabatino Cuomo, Valérie Baumann, Marco Pistolesi, Sebastien Biass, J. Ramon Arrowsmith, Mariagiovanna Moscariello, Mauro Rosi
Publikováno v:
Journal of Applied Volcanology, Vol 10, Iss 1, Pp 1-23 (2021)
Abstract Lahars are rapid flows composed of water and volcaniclastic sediments, which have the potential to impact residential buildings and critical infrastructure as well as to disrupt critical services, especially in the absence of hazard-based la
Externí odkaz:
https://doaj.org/article/2efb443ab56e4d008c46462a2550a7f7
Autor:
Simone Bello, Carlo Andrenacci, Daniele Cirillo, Chelsea P. Scott, Francesco Brozzetti, J Ramon Arrowsmith, Giusy Lavecchia
Publikováno v:
Lithosphere. 2022
Following observations made in a survey campaign along the Lost River Fault (Idaho, USA) in 2019, we integrate both original and previously published data to obtain a detailed segmentation of the fault sections that failed in the 1983 Borah Peak eart
Autor:
Chelsea P. Scott, Tiziano Giampietro, Cassandra Brigham, Frédérique Leclerc, Isabelle Manighetti, J Ramon Arrowsmith, Daniel A. Laó-Dávila, Lionel Mattéo
Publikováno v:
Lithosphere
Lithosphere, In press, 2021 (Special 2), pp.9031662. ⟨10.2113/2021/9031662⟩
Lithosphere, In press, 2021 (Special 2), pp.9031662. ⟨10.2113/2021/9031662⟩
Observations of fault geometry and cumulative slip distribution serve as critical constraints on fault behavior over temporal scales ranging from a single earthquake to a fault’s complete history. The increasing availability of high-resolution topo
Autor:
Magda Patyniak, Angela Landgraf, Atyrgul Dzhumabaeva, Alana M. Williams, Sultan Baikulov, J Ramon Arrowsmith, Kanatbek Abdrakhmatov, Mnfred R. Strecker
The Pamir Frontal Thrust (PFT) constitutes the northernmost boundary of the Pamir mountain range at the NW edge of the India-Eurasia collision zone. Due to the ongoing collision this active system propagates into and overthrusts the Quaternary deposi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::56e38e68cc50e4dff34b1480a48d80dd
https://doi.org/10.5194/egusphere-egu2020-4599
https://doi.org/10.5194/egusphere-egu2020-4599
Autor:
Emily E. Zawacki, J. Ramon Arrowsmith, Craig S. Feibel, Manfred R. Strecker, Arjun M. Heimsath, Christopher J. Campisano
Publikováno v:
Geological Society of America Abstracts with Programs.
Autor:
Matthijs C. van Soest, J. Ramon Arrowsmith, Christopher J. Campisano, Frank Schaebitz, Kip V. Hodges, Manfred R. Strecker, Emily E. Zawacki, Craig S. Feibel
Publikováno v:
Geological Society of America Abstracts with Programs.
Autor:
Craig S. Feibel, Emily E. Zawacki, Alan L. Deino, Christopher J. Campisano, J. Ramon Arrowsmith, John D. Kingston, Team Members Hspdp, Helen M. Roberts, Manfred R. Strecker
Publikováno v:
Geological Society of America Abstracts with Programs.
Autor:
Brian, Villmoare, William H, Kimbel, Chalachew, Seyoum, Christopher J, Campisano, Erin, DiMaggio, John, Rowan, David R, Braun, J Ramon, Arrowsmith, Kaye E, Reed
Publikováno v:
Science (New York, N.Y.). 348(6241)
Hawks et al. argue that our analysis of Australopithecus sediba mandibles is flawed and that specimen LD 350-1 cannot be distinguished from this, or any other, Australopithecus species. Our reexamination of the evidence confirms that LD 350-1 falls o
Publikováno v:
Geophysical Research Letters. 28:3777-3780
Fault slip and geomorphic surface processes create and modify bedrock normal fault scarps. Our field studies and numerical models show that mechanical interaction between near-surface fractures and active faults may diminish scarp slopes and broaden