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Study of the effects of processing strategy variations on GPS position estimates

Mulić M., Bilajbegović A., Altiner Y.

Reports on Geodesy

2006

z. 5/80

111--119

Is Adria a promontory or does it exist as an independent microplate?

Altiner Y., Marjanovic-Kavanagh R., Medak D., Medić Z., Prelegović E., Pribičević B., Seliškar A.

Reports on Geodesy

2001

z. 2/57

224-229

Is the Adria a Promontory or Exists as an Independent Microplate ?

Altiner Y., Colic K., Marjanovic M., Medic Z., Medved M., Miskovic D., Pitribicevic B., Rasic L., Seeger H., Szabo M.

Reports on Geodesy

1999

z. 5/46

149-157

In 1994, for the investigation of the present-day tectonics in the area of the Adriatic Sea a GPS network of 22 stations distributed over Croatia (17), Slovenia (3), and Italy (2) was established. In 1996, the network was extended towards the south and the west by 7 new stations. Three GPS campaigns in 1994, 1996, and 1998 were conducted within this network. Processing ofthe data from 1994 and 1996 was completed by the Bundesamt fur Kartographie und Geodasie in Frankfurt/Main using the Bernese GPS Software (Version 4.0). Based on an analytical surface deformation theory applied to the velocities derived within the CRODYN'94 and CRODYN'96 campaigns, the Adriatic Sea area indicates three different defermotion zones.