P530 STUDY IN THE DEVELOPMENT OF MAIN DOLOMITE (Ca2) IN WESTERN POLAND IN THE ASPECT OF HYDROCARBONS SEARCH 1 The area in question has been intensively analysed in geological and seismic terms. It is situated on two separate tectonic units that are defined and limited in different ways in literature. It may be stated that in geological terms the area comprises the most south-east protruding part of Szczecin Synclinorium. At the end of it a regional strike of tectonic displacement and layers of permian – mezozoic elevations connected with it and called Gorzów Region are to be found. The drilling


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