Zobrazeno 1 - 10
of 268
pro vyhledávání: '"Walker RT"'
We use satellite‐derived high‐resolution topography and ortho‐images, namely pre‐earthquake Advanced Land Observing Satellite World 3D data and post‐earthquake Pleiades data, to retrieve 3D displacements in the 2013 Balochistan, Pakistan ea
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::07f55ffc0626d3ff88d49c1e1b67c7b5
https://ora.ox.ac.uk/objects/uuid:1bd8bbf3-976a-4340-8f1a-b9c3ba647b5b
https://ora.ox.ac.uk/objects/uuid:1bd8bbf3-976a-4340-8f1a-b9c3ba647b5b
Publikováno v:
Journal of geophysical research. Earth surface, vol 123, iss 4
Dow, CF; Werder, MA; Babonis, G; Nowicki, S; Walker, RT; Csatho, B; et al.(2018). Dynamics of Active Subglacial Lakes in Recovery Ice Stream. JOURNAL OF GEOPHYSICAL RESEARCH-EARTH SURFACE, 123(4), 837-850. doi: 10.1002/2017JF004409. UC Irvine: Retrieved from: http://www.escholarship.org/uc/item/8nb5g9kd
Dow, CF; Werder, MA; Babonis, G; Nowicki, S; Walker, RT; Csatho, B; et al.(2018). Dynamics of Active Subglacial Lakes in Recovery Ice Stream. JOURNAL OF GEOPHYSICAL RESEARCH-EARTH SURFACE, 123(4), 837-850. doi: 10.1002/2017JF004409. UC Irvine: Retrieved from: http://www.escholarship.org/uc/item/8nb5g9kd
Recovery Ice Stream has a substantial number of active subglacial lakes that are observed, with satellite altimetry, to grow and drain over multiple years. These lakes store and release water that could be important for controlling the velocity of th
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https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::773abc5155062c90bc3685fd0a0639d0
https://escholarship.org/uc/item/8nb5g9kd
https://escholarship.org/uc/item/8nb5g9kd
The relationship between individual earthquakes and the longer-term growth of topography and of geological structures is not fully understood, but is key to our ability to make use of topographic and geological datasets in the contexts of seismic haz
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https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::a222bb009ec6584064cadd915c866722
https://doi.org/10.1002/2017jb014268
https://doi.org/10.1002/2017jb014268
This is the author accepted manuscript. The final version is available from Wiley via http://onlinelibrary.wiley.com/doi/10.1002/2017TC004657/abstract
The Zailisky Alatau is a >250-km-long mountain range in Southern Kazakhstan. Its northern rang
The Zailisky Alatau is a >250-km-long mountain range in Southern Kazakhstan. Its northern rang
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::c79ab4641c3aaf618d0c6215221d6da5
https://doi.org/10.1002/2017tc004657
https://doi.org/10.1002/2017tc004657
Autor:
Middleton, TA, Walker, RT, Rood, DH, Rhodes, EJ, Parsons, B, Lei, Q, Elliott, JR, Ren, Z, Zhou, Y
Publikováno v:
Tectonics. 35(11)
Analysis of the locus, style, and rate of faulting is fundamental to understanding the kinematics of continental deformation. The Ordos Plateau lies to the northeast of Tibet, within the India-Eurasia collision zone. Previous studies have suggested t
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https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::da20d09fbc7adc03e483c0dda02b3695
http://ora.ox.ac.uk/objects/uuid:
http://ora.ox.ac.uk/objects/uuid:
The seismic hazard in the immediate vicinity of an earthquake is usually assumed to be reduced after rupture of a continental fault, with along-strike portions being brought closer to failure and aftershocks being significantly smaller. This period o
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::c00cdbc7769028917219a956c56ec073
https://doi.org/10.1029/2011gl046897
https://doi.org/10.1029/2011gl046897
The 2013 Balochistan earthquake, a predominantly strike-slip event, occurred on the arcuate Hoshab fault in the eastern Makran linking an area of mainly left-lateral shear in the east to one of shortening in the west. The difficulty of reconciling pr
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https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::515454fe04adfde280b2ac5181cfb79e
https://doi.org/10.1002/2015gl065096
https://doi.org/10.1002/2015gl065096
Autor:
Walker, RT, Khatib, MM
[1] We use satellite imagery and field observations to investigate the distribution of active faults around Birjand in eastern Iran to determine how the transition between conjugate zones of faulting can be accommodated by diffuse active faulting. In
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https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::f94935faa4b11b3aaab15aa25caed917
https://doi.org/10.1029/2005tc001871
https://doi.org/10.1029/2005tc001871
The sequence of seismicity in the Dasht-e-Bayaz and Zirkuh region of northeastern Iran, which includes 11 destructive earthquakes within a period of only 30 years, forms one of the most outstanding examples of clustered large and intermediate-magnitu
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https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::cde135848f8d51a503ed60596bde574b
https://doi.org/10.1111/j.1365-246x.2011.05213.x
https://doi.org/10.1111/j.1365-246x.2011.05213.x
A large continental normal‐faulting earthquake occurred in the Yinchuan Graben in northern China on 3 January 1739. This event is of significant interest for two reasons. First, it has been suggested on the basis of historical records of shaking th
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https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::702c6d93145d339400fd1ebc327995b8
https://ora.ox.ac.uk/objects/uuid:51d1a15e-53c6-46d9-bce0-7c32ad0ac9a2
https://ora.ox.ac.uk/objects/uuid:51d1a15e-53c6-46d9-bce0-7c32ad0ac9a2