Published December 2009

About study internel structure of Mesozoic sediments in Yevlakh-Aghjabedy through by seismic survey

Y.H.Ganbarov

In Gazanbulag-Borsunlu-Ziyadkhan-Chayly areas of Yevlax Aghjabedy throuqh by CDP method with 125 fold overlaps is worked 6 profiles using 240 canols of seismic station “Progress T” and vibrators group. Received seismic records are developed using package of programms “PROMAX”. In all seismic sections lower V seismic horizon ( cretaceous surface) for the first time are traced dynamic expression of reflected borders in deep interval 600-3400 m. These reflected borders belong to upper and low cretaceous sediments and apparently illuminate interval geological structure of mesozoic complex. Achieved new seismic materials show that with application modern technics and technology can study internel structure of mesozoic sediments in Yevlakh-Aghjabedy through. Acquired Qazanbulag region new seismic data show that, if mesozoic sediments are presented by principal carbonate facies, then one may study their internel geological structure with new methodes application. Simultaneously it is show that from volconogenic formation intervals of mesozoic complex to acquire useful seismic information is impossible. Thus acguired initial seismic data give new possibility of application modern seismic survey technology for study of internel geological structure of mesozoic sediments perspectivy areas Yevlakh-Aghjabedy throuqh.