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.