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other (Emre et al., 2005). The length of this segment is 15 km and it has 10 km long
undersea part (Ocakoglu et al., 2005). Moreover, this segment is very close to a 15 km
long normal fault, Gumuldur fault (GuF), so this complexity has to be considered in
any design process. Adding extra control points to the network would be a solution for
monitoring this dynamic region of study area. There are some short baselines in the
network such as CCEK-GMDR baseline because of the adjacency of two active faults.
There is another fault very near to TF and GMDR and CCEK points are very close to
that GuF. The WGS84 coordinates of the control station shown in Table 2.
Figure 5.
Locations of the sites of Izmir microgeodetic network.
Table 2.
Locations of network stations.
Site name
q> Latitude (in Degrees)
A. Longitude (in Degrees)
KG01
38.36416
27.02072
KG02
38.23637
27.34451
KG03
38.25372
27.18084
KG04
38.26320
26.80143
KG05
38.22815
26.94152
KG06
38.10099
26.90646
KG07
38.06433
26.87388
PAYM
38.31700
26.92600
KNRL
38.14244
27.12700
GMDR
38.06800
26.99700
