SUMMARY
The arti<:le presents an analysis of vertical
ti-anes llDeas.u.red In 2!1 !bore holes iSf.tuated in !the
Po-merania.n 8ynclLnorlium area, and 1n 2 bore holes
made ~lth!l4l ilts periphery. A c01DII)ll.rison has been
made of ver,tLcal times an 'diagrams, korn the eaclh sur:fa'Ce to the top of the Jurassie, Trlusic, Permian. CarIbanilferous and Devonia.n. CUrves in :time-.depth system have 'been approximated usl~ functions by selecting adequate formulae of T-a.!Z type.
Cc.n.seQuently also a reduction
at
:the da.ta hasbeen .made ·dOwn ,to the :bo.ttam oi the Tertiary de-!posits, and
new
dependencie$ have been dbrtaJ.ned.~ a rewlt cd ,the analylSis. relaltiOIlB betwee.n the velocity and dePth jm the :indiviidual g~Jc8l
s,ta-ges have ·been :recaved in the form of a time-depth ,diagram for .the entiire area of ·the Pamerania.n
syn-.olin'Ol"iUllIl. Du.ri.ng the interpreta.tio.n of seismical da-ta Itlhls ena.bleS us to a'Jjpoly velocilties more approxi-ma.te ,to the actual ones.
'l1he 'diagram ;here o1:Jtai.ned S1houlld Ibci ~
u8e-ful. ,partieularly in !plc>tting depth structural maps.
PE3IOME
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