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Craig earthquake 2013

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Journal Article
Published: 14 April 2015
Bulletin of the Seismological Society of America (2015) 105 (2B): 1153-1164.
..., up. On 5 January 2013 at 08:58 UTC, the Craig M w  7.5 earthquake occurred off the coast of Alaska about 113 km west of Craig and 114 km south of Port Alexander, as located by the Alaska Earthquake Center. The mainshock initiated at 10 km depth and was accompanied by a sequence of adjacent...
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Journal Article
Published: 07 April 2015
Bulletin of the Seismological Society of America (2015) 105 (2B): 1143-1152.
...Stephen Holtkamp; Natalia Ruppert AbstractThe Mw 7.5 Craig, Alaska, earthquake on 5 January 2013 was the second largest earthquake on the Queen Charlotte fault (QCF) in 40 yrs, representing the transform plate boundary between the Pacific and North American plates. Earthquake hazard along the QCF...
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Journal Article
Published: 14 April 2015
Bulletin of the Seismological Society of America (2015) 105 (2B): 1165-1177.
... broadband stations in the Canadian National Seismograph Network and find that the 2012 Mw 7.8 Haida Gwaii and 2013 Mw 7.5 Craig, Alaska, earthquakes triggered long duration (>10  s), emergent tremor‐like signals near the southeastern portion of the EDF. In both cases, tremor coincides with the peak...
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Journal Article
Published: 14 April 2015
Bulletin of the Seismological Society of America (2015) 105 (2B): 1053-1057.
...Thomas S. James; John F. Cassidy; Garry C. Rogers; Peter J. Haeussler The 27 October 2012 M w  7.8 Haida Gwaii thrust earthquake and the 5 January 2013 M w  7.5 Craig strike‐slip earthquake are the focus of this special issue. They occurred along the transform boundary between the Pacific...
FIGURES
Image
Finite‐fault models for the <b>2013</b> <b>Craig</b> <b>earthquake</b> representing the preferre...
Published: 14 April 2015
Figure 7. Finite‐fault models for the 2013 Craig earthquake representing the preferred model with the least constrained (top) and the most constrained (bottom) fault geometry. Both models have a centered hypocenter of 15 km, with a rupture velocity of 4  km/s along the positive 333° strike and 1
Journal Article
Published: 16 May 2018
Seismological Research Letters (2018) 89 (4): 1345-1353.
... and the 2013 M w  6.7 Lushan earthquakes, resulting in three destructive earthquakes to hit Sichuan Province in the last decade. The Wenchuan earthquake was a complex event, with just under a 240‐km‐long rupture trace along the base of the Longmen Shan, with predominantly reverse slip...
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Journal Article
Published: 14 April 2015
Bulletin of the Seismological Society of America (2015) 105 (2B): 1129-1142.
...Figure 7. Finite‐fault models for the 2013 Craig earthquake representing the preferred model with the least constrained (top) and the most constrained (bottom) fault geometry. Both models have a centered hypocenter of 15 km, with a rupture velocity of 4  km/s along the positive 333° strike and 1...
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Image
Location map for the 2012  M  w  7.8 Haida Gwaii and <b>2013</b>  M  w  7.5 <b>Craig</b> ...
Published: 14 April 2015
Figure 1. Location map for the 2012 M w  7.8 Haida Gwaii and 2013 M w  7.5 Craig earthquakes, which occurred on the Pacific–North American plate boundary. Approximate rupture zones for the two events are shown in yellow, whereas other significant events on the plate boundary are depicted
Image
Stations used in the finite‐fault slip inversion of the <b>2013</b> <b>Craig</b> earthqua...
Published: 14 April 2015
Figure 6. Stations used in the finite‐fault slip inversion of the 2013 Craig earthquake. The map has the location of each station relative to the NEIC hypocenter, showing the good azimuthal coverage. The seismograms show P waves (left) and SH waves (right) with solid lines for the recorded
Image
Stations used in the finite‐fault slip inversion of the <b>2013</b> <b>Craig</b> earthqua...
Published: 14 April 2015
Figure 6. Stations used in the finite‐fault slip inversion of the 2013 Craig earthquake. The map has the location of each station relative to the NEIC hypocenter, showing the good azimuthal coverage. The seismograms show P waves (left) and SH waves (right) with solid lines for the recorded
Journal Article
Published: 07 April 2015
Bulletin of the Seismological Society of America (2015) 105 (2B): 1219-1230.
... and Smith. This is Natural Resources Canada Earth Science Sector Contribution Number 20140187. Interestingly, just two months after the Haida Gwaii earthquake, the M w  7.5 strike‐slip event near Craig, Alaska, ruptured a more northerly section of the QCF ( Gomberg, 2013 ; Lay et al. , 2013...
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Journal Article
Published: 14 April 2015
Bulletin of the Seismological Society of America (2015) 105 (2B): 1090-1105.
... the entirety of its strike. The structure and dip of the QCF at depth, however, remain uncertain. For instance, we map a vertical QCF ∼1  km beneath the seafloor near the rupture of the 2013 Craig earthquake, though the earthquake ruptured a fault plane dipping at 63°, with a hypocenter at 10 km depth...
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Series: Geological Society, London, Special Publications
Published: 01 January 2017
DOI: 10.1144/SP441.4
EISBN: 9781862399709
... earthquake situational awareness tools. The use of the new strong-motion network is demonstrated for two recent earthquakes in northern Sumatra: the 2 July 2013 M w 6.1 Bener Meriah, Sumatra and the 10 October 2013 M w 5.4 Aceh Besar earthquakes. The former earthquake resulted in 35 fatalities...
Journal Article
Published: 06 December 2017
Seismological Research Letters (2017) 89 (1): 13-21.
... . Aftershock observation and analysis of the 2013 M s  7.0 Lushan earthquake , Seismol. Res. Lett. 86 , 1 – 8 , doi: 10.1785/0220140186 . Feng X. Y. Deng Q. D. , and Shi J. B. 1991 . Active tectonics of the southern and northern Tianshan and its tectonic evolution...
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Journal Article
Journal: Geosphere
Published: 01 December 2014
Geosphere (2014) 10 (6): 1255-1282.
... may be accommodated by internal deformation within the plateau and regional clockwise rotation of the Kunlun fault ( Harkins et al., 2010 ; Kirby and Harkins, 2013 ), and/or that displacement is transferred northward, across the interior of northeastern Tibet, to the Haiyuan fault ( Duvall and Clark...
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Journal Article
Journal: Interpretation
Published: 13 October 2016
Interpretation (2016) 4 (4): SQ59-SQ69.
... (Figure  1 ; Field, 2013 ). Effects from the 1906 and 1989 earthquakes were especially pronounced in areas composed of soft sediments and artificial fill. Sites along the margins of the bay with late Quaternary sediments and artificial fill combined with a shallow water table are likely to experience...
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Journal Article
Journal: GSA Bulletin
Published: 01 March 2013
GSA Bulletin (2013) 125 (3-4): 420-431.
...Brendan Duffy; Mark Quigley; David J.A. Barrell; Russ Van Dissen; Timothy Stahl; Sébastien Leprince; Craig McInnes; Eric Bilderback AbstractDextral slip at the western end of the east-west–striking Greendale fault during the 2010 MW 7.1 Darfield earthquake transferred onto a northwest-trending...
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Journal Article
Published: 07 April 2015
Bulletin of the Seismological Society of America (2015) 105 (2B): 1253-1264.
... as it accommodates elements of both convergence and margin‐parallel motion in the restraining bend between the complicated Queen Charlotte triple junction to the south and the purely strike‐slip region to the north ( Rohr and Furlong, 1995 ; Smith et al. , 2003 ; Szeliga, 2013 ). Prior to the 2012 earthquake...
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Journal Article
Journal: GSA Bulletin
Published: 30 June 2017
GSA Bulletin (2017) 129 (11-12): 1450-1471.
... studies have hypothesized that the Tajik fold-and-thrust belt may have initiated in the Miocene as a result of gravitational collapse of the Pamir ( Stübner et al., 2013 ; Rutte et al., 2017b ). The Tajik fold-and-thrust belt is still active today, and GPS measurements indicate ∼5–10 mm/yr convergence...
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Journal Article
Published: 29 January 2016
Canadian Journal of Earth Sciences (2016) 53 (2): 129-139.
... of this earthquake (and the 5 January 2013 M W 7.5 Craig strike-slip earthquake). James et al. (2015) provided the introduction to this special issue. The full moment tensor inversion for the Haida Gwaii earthquake was performed using the method outlined earlier. As the Haida Gwaii earthquake was very large...
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