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Journal Article
Published: 22 May 2018
Bulletin of the Seismological Society of America (2018) 108 (3B): 1746–1756.
..., emergency observations were made promptly and frequently by ALOS‐2. In this study, we used data acquired in both a high‐resolution stripmap mode ( 10 × 5    m resolution in ground range and azimuth, respectively, and 70‐km swath width) and wide swath Scan SAR (ScanSAR) mode ( 20 × 25    m...
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Journal Article
Published: 01 May 2018
Bulletin of the Seismological Society of America (2018) 108 (3A): 1489.
..., S9, and S10, and captions in the electronic supplement. Reference Morishita Y. Kobayashi T. Fujiwara S. , and Yarai H. 2017 . Complex crustal deformation of the 2016 Kaikoura, New Zealand, earthquake revealed by ALOS‐2 , Bull. Seismol. Soc. Am. 107 , no.  6 , 2676...
Journal Article
Published: 07 November 2017
Bulletin of the Seismological Society of America (2017) 107 (6): 2676–2686.
... associated with the earthquake revealed by Advanced Land Observing Satellite 2 (ALOS‐2) SAR data (see Data and Resources ). We also constructed a fault model from the obtained displacement data to infer the complex mechanism of the earthquake. Following the earthquake, emergency observations were...
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Journal Article
Published: 01 November 2015
Seismological Research Letters (2015) 86 (6): 1549–1556.
... Synthetic Aperture Radar ( SAR ) data from Italian Space Agency’s (ASI’s) COSMO–SkyMed (CSK) satellites and Japan Aerospace Exploration Agency’s (JAXA’s) Advanced Land Observing Satellite-2 (ALOS-2), as part of an ongoing collaborative effort between the Jet Propulsion Laboratory (JPL) and the California...
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Journal Article
Published: 01 October 2013
Bulletin of the Seismological Society of America (2013) 103 (5): 2928–2936.
...Jianbao Sun; Zheng‐Kang Shen; Roland Bürgmann; Xiwei Xu Abstract We investigate coseismic deformation of the 24 March 2011 M w 6.8 Tarlay, Myanmar, earthquake using ALOS PALSAR data from both descending and ascending passes. Using high‐quality synthetic aperture radar interferograms and amplitude...
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Journal Article
Published: 01 November 2010
Bulletin of the Seismological Society of America (2010) 100 (5B): 2750–2766.
... identified by Xu et al. (2009) and Liu-Zeng et al. (2009) . Seven rectangles represent the areas observed by ALOS/PALSAR; each area is designated by a path number, 471–477. The color version of this figure is available only in the electronic edition. The overall locations, geometry, and slip...
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Book Chapter

Published: 01 January 2013
EISBN: 9780903056434
... relationships between aluminium and analogous iron compounds are illustrated in Table 53 . Table 53. Structural relationships between analogous oxides of aluminium and iron. Oxygens in c.c.p. arrangement α–AlO(OH) diaspore γ–AlO(OH) boehmite α–Al 2 O 3 corundum γ–Al 2 O 3 γ-alumina...
Book Chapter

Published: 01 January 2013
EISBN: 9780903056434
... are in a hexagonal close-packed layer; those within the double octahedral layers in boehmite are in a cubic packing relationship (Fig. 282 ). These differences in oxygen packing are consistent with the behaviour of the two polymorphs of AlO(OH) on dehydration in that diaspore yields a-alumina (trigonal...
Journal Article
Published: 23 July 2019
Bulletin of the Seismological Society of America (2019) 109 (5): 2142–2144.
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Journal Article
Published: 04 July 2018
Seismological Research Letters (2018) 89 (5): 1826–1837.
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Journal Article
Published: 20 December 2017
Seismological Research Letters (2018) 89 (1): 77–85.
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Journal Article
Published: 06 September 2017
Seismological Research Letters (2017) 88 (6): 1472–1479.
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Journal Article
Published: 21 April 2015
Bulletin of the Seismological Society of America (2015) 105 (3): 1792–1796.
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Journal Article
Published: 01 November 2014
Earthquake Spectra (2014) 30 (4): 1487–1509.
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Journal Article
Published: 01 November 2012
Vadose Zone Journal (2012) 11 (4): vzj2011.0133.
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Journal Article
Published: 01 November 2012
Vadose Zone Journal (2012) 11 (4): vzj2011.0142.
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Journal Article
Published: 01 May 2009
Vadose Zone Journal (2009) 8 (2): 510–522.
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Journal Article
Published: 01 February 2004
Vadose Zone Journal (2004) 3 (1): 203–219.
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Image
The predicted InSAR deformation fields of (a) ALOS‐2 ascending, (b) ALOS‐2 descending, (c) Sentinel‐1 ascending, and (d) Sentinel‐1 descending by the best‐fitting faulting model. The red star indicates the epicenter of the 2017 Sarpol Zahab earthquake.
Published: 10 October 2018
Figure 5. The predicted InSAR deformation fields of (a) ALOS‐2 ascending, (b) ALOS‐2 descending, (c) Sentinel‐1 ascending, and (d) Sentinel‐1 descending by the best‐fitting faulting model. The red star indicates the epicenter of the 2017 Sarpol Zahab earthquake.
Image
The residual InSAR deformation fields of (a) ALOS‐2 ascending, (b) ALOS‐2 descending, (c) Sentinel‐1 ascending, and (d) Sentinel‐1 descending between the predicted and observed deformation. Black dashed ellipses indicate the significant InSAR deformation residual areas.
Published: 10 October 2018
Figure 6. The residual InSAR deformation fields of (a) ALOS‐2 ascending, (b) ALOS‐2 descending, (c) Sentinel‐1 ascending, and (d) Sentinel‐1 descending between the predicted and observed deformation. Black dashed ellipses indicate the significant InSAR deformation residual areas.