[go: up one dir, main page]
More Web Proxy on the site http://driver.im/
Next Article in Journal
An Inter-Comparison Study of Multi- and DBS Lidar Measurements in Complex Terrain
Previous Article in Journal
An Inter-Comparison of Techniques for Determining Velocities of Maritime Arctic Glaciers, Svalbard, Using Radarsat-2 Wide Fine Mode Data
You seem to have javascript disabled. Please note that many of the page functionalities won't work as expected without javascript enabled.
 
 
Search for Articles:
Title / Keyword
Author / Affiliation / Email
Journal
Article Type
 
 
Advanced Search
 
Section
Special Issue
Volume
Issue
Number
Page
 
Journals
Remote Sensing
Volume 8
Issue 9
10.3390/rs8090784
remotesensing-logo
Submit to this Journal Review for this Journal Propose a Special Issue
► Article Menu

Article Menu

share Share announcement Help format_quote Cite question_answer Discuss in SciProfiles thumb_up
...
Endorse textsms
...
Comment
Correction to Remote Sens. 2016, 8(8), 649.
first_page
settings
Order Article Reprints
Font Type:
Arial Georgia Verdana
Font Size:
Aa Aa Aa
Line Spacing:
Column Width:
Background:
Correction

Correction: Liu, Y. et al. Time-Dependent Afterslip of the 2009 Mw 6.3 Dachaidan Earthquake (China) and Viscosity beneath the Qaidam Basin Inferred from Postseismic Deformation Observations. Remote Sens. 2016, 8, 649

by
Yang Liu
1,2,3,4,*,
Caijun Xu
1,2,3,
Zhenhong Li
4,
Yangmao Wen
1,2,3,
Jiajun Chen
4 and
Zhicai Li
5
1
School of Geodesy and Geomatics, Wuhan University, Wuhan 430079, China
2
Key Laboratory of Geospace Environment and Geodesy, Ministry of Education, Wuhan University, Wuhan 430079, China
3
Collaborative Innovation Center for Geospatial Technology, Wuhan 430079, China
4
COMET, School of Civil Engineering and Geosciences, Newcastle University, Newcastle upon Tyne NE1 7RU, UK
5
Department of Geodesy, National Geomatics Center of China, Beijing 100048, China
*
Author to whom correspondence should be addressed.
Remote Sens. 2016, 8(9), 784; https://doi.org/10.3390/rs8090784
Submission received: 6 September 2016 / Accepted: 16 September 2016 / Published: 21 September 2016
Browse Figure
Figure 1
<p>Tectonics associated with the 2009 Mw 6.3 DCD earthquake. The bottom-left and bottom-right insets show the location of the main figure, respectively. The light blue rectangle is the spatial extent of the Envisat Advanced Synthetic Aperture Radar (ASAR) descending Track 319 images, with AZI and LOS referring to satellite azimuth and look directions. The focal mechanisms of the 2008 and 2009 events are from United States Geological Survey (USGS) [4]. The two purple rectangles are the surface projections of the main fault rupturing zones during the 2008 and 2009 events [3,21]. The black and yellow hollow circles are the aftershocks of the 2008 and 2009 events, respectively [4]. The purple and black lines are the active faults from Peltzer and Saucier [24] and Deng et al. [5], respectively. (Note that the references here correspond to those in the original manuscript).</p> ">
Versions Notes
After publication of the research paper [1] an error was recognized. Figure 1 was partly misplotted and should be replaced with the following figure.
The change does not affect the results. The manuscript will be updated on the article webpage.
We apologize for any inconvenience this has caused.

Reference

  1. Liu, Y.; Xu, C.; Li, Z.; Wen, Y.; Chen, J.; Li, Z. Time-dependent afterslip of the 2009 Mw 6.3 Dachaidan earthquake (China) and viscosity beneath the Qaidam Basin inferred from postseismic deformation observations. Remote Sens. 2016, 8, 649. [Google Scholar] [CrossRef]
Remotesensing 08 00784 g001 1024
Figure 1. Tectonics associated with the 2009 Mw 6.3 DCD earthquake. The bottom-left and bottom-right insets show the location of the main figure, respectively. The light blue rectangle is the spatial extent of the Envisat Advanced Synthetic Aperture Radar (ASAR) descending Track 319 images, with AZI and LOS referring to satellite azimuth and look directions. The focal mechanisms of the 2008 and 2009 events are from United States Geological Survey (USGS) [4]. The two purple rectangles are the surface projections of the main fault rupturing zones during the 2008 and 2009 events [3,21]. The black and yellow hollow circles are the aftershocks of the 2008 and 2009 events, respectively [4]. The purple and black lines are the active faults from Peltzer and Saucier [24] and Deng et al. [5], respectively. (Note that the references here correspond to those in the original manuscript).
Figure 1. Tectonics associated with the 2009 Mw 6.3 DCD earthquake. The bottom-left and bottom-right insets show the location of the main figure, respectively. The light blue rectangle is the spatial extent of the Envisat Advanced Synthetic Aperture Radar (ASAR) descending Track 319 images, with AZI and LOS referring to satellite azimuth and look directions. The focal mechanisms of the 2008 and 2009 events are from United States Geological Survey (USGS) [4]. The two purple rectangles are the surface projections of the main fault rupturing zones during the 2008 and 2009 events [3,21]. The black and yellow hollow circles are the aftershocks of the 2008 and 2009 events, respectively [4]. The purple and black lines are the active faults from Peltzer and Saucier [24] and Deng et al. [5], respectively. (Note that the references here correspond to those in the original manuscript).
Remotesensing 08 00784 g001

Share and Cite

MDPI and ACS Style

Liu, Y.; Xu, C.; Li, Z.; Wen, Y.; Chen, J.; Li, Z. Correction: Liu, Y. et al. Time-Dependent Afterslip of the 2009 Mw 6.3 Dachaidan Earthquake (China) and Viscosity beneath the Qaidam Basin Inferred from Postseismic Deformation Observations. Remote Sens. 2016, 8, 649. Remote Sens. 2016, 8, 784. https://doi.org/10.3390/rs8090784

AMA Style

Liu Y, Xu C, Li Z, Wen Y, Chen J, Li Z. Correction: Liu, Y. et al. Time-Dependent Afterslip of the 2009 Mw 6.3 Dachaidan Earthquake (China) and Viscosity beneath the Qaidam Basin Inferred from Postseismic Deformation Observations. Remote Sens. 2016, 8, 649. Remote Sensing. 2016; 8(9):784. https://doi.org/10.3390/rs8090784

Chicago/Turabian Style

Liu, Yang, Caijun Xu, Zhenhong Li, Yangmao Wen, Jiajun Chen, and Zhicai Li. 2016. "Correction: Liu, Y. et al. Time-Dependent Afterslip of the 2009 Mw 6.3 Dachaidan Earthquake (China) and Viscosity beneath the Qaidam Basin Inferred from Postseismic Deformation Observations. Remote Sens. 2016, 8, 649" Remote Sensing 8, no. 9: 784. https://doi.org/10.3390/rs8090784

APA Style

Liu, Y., Xu, C., Li, Z., Wen, Y., Chen, J., & Li, Z. (2016). Correction: Liu, Y. et al. Time-Dependent Afterslip of the 2009 Mw 6.3 Dachaidan Earthquake (China) and Viscosity beneath the Qaidam Basin Inferred from Postseismic Deformation Observations. Remote Sens. 2016, 8, 649. Remote Sensing, 8(9), 784. https://doi.org/10.3390/rs8090784

Note that from the first issue of 2016, this journal uses article numbers instead of page numbers. See further details here.

Article Metrics

Back to TopTop