HUSCAP logo Hokkaido Univ. logo

Hokkaido University Collection of Scholarly and Academic Papers >
Graduate School of Science / Faculty of Science >
Peer-reviewed Journal Articles, etc >

Coseismic displacement due to the 2008 Iwate-Miyagi Nairiku earthquake detected by ALOS/PALSAR : preliminary results

Files in This Item:
6104e009.pdf5.38 MBPDFView/Open
Please use this identifier to cite or link to this item:http://hdl.handle.net/2115/52818

Title: Coseismic displacement due to the 2008 Iwate-Miyagi Nairiku earthquake detected by ALOS/PALSAR : preliminary results
Authors: Takada, Youichiro Browse this author
Kobayashi, Tomokazu Browse this author
Furuya, Masato Browse this author →KAKEN DB
Murakami, Makoto Browse this author
Keywords: 2008 Iwate-Miyagi Nairiku earthquake
pixel offset field
stereoscopic effect
complex fault structure
Issue Date: 12-Mar-2009
Publisher: TERRAPUB
Journal Title: Earth, Planets and Space
Volume: 61
Issue: 4
Start Page: e9
End Page: e12
Rights: Applying interferometric SAR (InSAR) analysis to the 2008 Iwate-Miyagi Nairiku earthquake, we detected notable ground displacements of several tens of centimeters to about 1.2 m that extend further south of the epicentral area. We explained the InSAR data by constructing a fault model consisting of four WNW dipping and one ESE dipping reverse faults. The residuals between observed and modeled deformation are less than 6 cm in most of the area, which is comparable to the errors caused by atmospheric effect. To fill the lack of InSAR data in the hypocentral area, we applied a pixel matching technique to the intensity images, which shows a shortening in range offsets by as much as ∼2 m along a narrow zone stretching along the eastern foot of Mt. Kurikoma, indicating a localized uplift. We also found remarkable contrasts in the range offsets around the low coherence area equivalent to a very large displacement gradient to the WNW of the hypocentral area as well as ESE. We conclude that the main faulting occurred on the WNW dipping reverse faults, but that the overall geometry of the fault system is quite complex including at least one conjugate faulting, as also supported by the hypocentral distribution of aftershocks.
Type: article
URI: http://hdl.handle.net/2115/52818
Appears in Collections:理学院・理学研究院 (Graduate School of Science / Faculty of Science) > 雑誌発表論文等 (Peer-reviewed Journal Articles, etc)

Submitter: 古屋 正人

Export metadata:

OAI-PMH ( junii2 , jpcoar_1.0 )

MathJax is now OFF:


 

 - Hokkaido University