Full text: Technical Commission IV (B4)

  
4. CONCLUSION AND FUTURE DIRECTIONS 
GPS data from various sources can be currently uploaded into 
the system. Since the study is an open-end one, any kind of 
data, which contributes valuable information, can be added into 
the system. As new datasets are being added, new applications 
become possible. This development model can generate many 
innovative applications. The integration of real-time GPS data 
from continuous GPS stations will be studied in the scope of the 
future applications (Figure 5). 
  
  
  
  
  
  
  
  
  
  
S À 1 Real Time 
p > Data 
Seismic GPS 
  
  
  
  
  
  
  
  
  
Archived 
Data 
À 
——- À = 
A Data 
  
  
  
  
  
Data 
Figure 5. Current and future data streaming to the system 
Service-oriented architecture of the application allows its 
components to be used by other applications and users over the 
Internet. Since reusability of components was provided, it 
minimized the need for new coding. Its infrastructure is ready to 
be used for other applications in Earth science. There is a need 
for bridging between Earth science and Computer science. Earth 
sciences need information technologies to solve data related 
problems. 
REFERENCES 
1. Seber, D., Vallve, M., Sandvol, E., Steer, D., 
Barazangi, M., 1997. Middle East Tectonics: 
Applications of Geographic Information Systems 
(GIS), GSA Today, 7, No. 2, February. 
2. Environmental Systems Research Institute, Inc. 
(ESRI), Computer Software, 380 New York Street, 
Redlands, CA 92373-8100, USA. 
3. Wessel, P., and W. H. F. Smith, 2001, The Generic 
Mapping Tools (GMT) version 3.4 Technical 
Reference & Cookbook, SOEST/NOAA. 
4. Haines, A.J. and Holt, W.E., 1993. A procedure to 
obtain the complete horizontal motions within zones 
of distributed deformation from the inversion of strain 
rate data, Journal of Geophysical Research, 98, 
12,057-12,082. 
5. Haines, A J., Jackson, J.A., Holt, W.E., Agnew, D.C., 
1998. Representing distributed deformation by 
continuous velocity fields, Institute of Geological and 
Nuclear Sciences science report, 98/5, Wellington, 
New Zealand. 
Aki, K. And Richards P. G. , 2002. Quantitative 
Seismology, University Science Books, New York, 
USA. 
Kostrov, V.V., 1974. Seismic Moment and Energy of 
Earthquakes, and Seismic Flow of Rocks, Izv Acad. 
Sci., USSR, Phys, Solid Earth, English Translation, 1, 
23-44. 
Ambraseys, N.N. and Finkel, C.F., 1995. The 
Seismicity of Turkey and Adjacent Areas, A 
Historical Review, 1500-1800, Eren, Istanbul, 
Turkey. 
Global CMT Catalog, 2006. Global Centroid Moment 
Tensor Project, May 2006, 
<http://www.globalcmt.org/>. 
KOERI NEMC, 2006. Bogazici University, Kandilli 
Observatory and Earthquake Research Institute, 
National Earthquake Monitoring Center Home Page, 
February 2007, 
<http://Www.koeri.boun.edu.tr/sismo>. 
ImageMagick, 2007. ImageMagick Home Page, 
February 2007, <http://www.imagemagick.org>. 
ABS 
The 
resol 
work 
geos] 
data 
com 
Nort] 
flow 
vecto 
prodi 
throu 
status 
prodi 
appli 
rectif 
inter 
autor 
the w 
techn 
to thi 
In re 
point 
comp 
meth 
for fa 
by v: 
frequi 
proce 
acqui 
In ad 
senso 
Withit 
risen. 
North 
Calga 
ALS 
comp.
	        
Waiting...

Note to user

Dear user,

In response to current developments in the web technology used by the Goobi viewer, the software no longer supports your browser.

Please use one of the following browsers to display this page correctly.

Thank you.