There was supposed a geodynamic and petrochemcal models of collision magmatism evolution of the Zesser Caucasus;

There was established bipolar zonality of magmatism and metallogeny along Zangezur suture zone  and prediction is given for fields discovery;

There was established a vertical migration of the Cenoroic magmatic depths along the suture zone of the Zesser Cancasus;

There was studied petromagmatic feantures of opniolitic complexes and a role of linnation processes while thoir formation had been revelated;

There was supposed a petrological model of the optyolitic type of gold;

Ore field; the was studied depth inclusions in the volcanogenic comploxes of the Z.Cancasus and Talysh; co-antor of the tectonik, geologic maps of Azerbaijan; map of magmatism and metemofphism of Talysh.

1. Geology and volcanism of Tallish. Baku, Elm, 1979.

2. The indicator roles of the cainozoics volcanic formations in the geodynamical reconstruction of Zesser Cancasus. DAN Az.SSR, v XV, 1989, N5.

3. Graben-riftogen nature of Kura-South Caspian basic. vol."New tectonic processes and its influence in the oil and gas deposits". Baku, 1999.

4.  Geochemical evolution of the Alpine basic volcanism Zesser Cancasus. GIA, Baku, 2000.

5. Geology of the Azerbaijan, vol.Magmatism, Baku, 2001 (co-author)