Genesis and dynamics of local structures in Sredneobskaya petroleum province of Western Siberia

Authors: A.S. Flaas (Perm National Research Polytechnic University, RF, Perm)

Key words: structural and paleotectonic analysis, compaction, inversion structure, the Alpine tectonic activity, the mobile zone.

A detailed study of areal relations of the structural plan of the late-jurassic sediments from the rugged pre-jurassic basement has found that most of the area Sredneobskaya petroleum province one of the main reasons for the formation of local uplift of the sedimentary cover is the seal. Other factors that play in some areas and isolated areasis not less important are the Cimmerian-Alpine tectonic movements.

References

1. Flaas A.S., Chernova M.L., Geologiya nefti i gaza - The journal Oil and Gas Geology, 2003, no. 4.

2. Flaas A.S., Geotektonika (metodicheskie priemy paleotektonicheskogo analiza) (Geotectonics (methodical ways of paleotectonic analysis)), Perm': PGTU Publ., 2008, 197 p.

3. Flaas A.S., Chernova M.L., Vestnik PGTU. Geologiya, geoinformatsionnye sistemy, gorno-neftyanoe delo, 2000, V. 3, pp. 42-46.

4. Flaas A.S., Chernova M.L., Geologiya i poleznye iskopaemye Zapadnogo Urala, 2001, pp. 26-28.

5. Flaas A.S., Problemy mineralogii, petrografii i metallogenii PGU, 2004, V. 6, pp. 91-94.

6. Flaas A.S., Geologiya, geofizika i razrabotka neftyanykh i gazovykh mestorozhdeniy, 2005, no. 9-10, pp. 18 – 23.

7. Nassonova N.V., Romanchev M.A., Geologiya nefti i gaza - The journal Oil and Gas Geology, 2011, no. 4.

Key words: structural and paleotectonic analysis, compaction, inversion structure, the Alpine tectonic activity, the mobile zone.

A detailed study of areal relations of the structural plan of the late-jurassic sediments from the rugged pre-jurassic basement has found that most of the area Sredneobskaya petroleum province one of the main reasons for the formation of local uplift of the sedimentary cover is the seal. Other factors that play in some areas and isolated areasis not less important are the Cimmerian-Alpine tectonic movements.

References

1. Flaas A.S., Chernova M.L., Geologiya nefti i gaza - The journal Oil and Gas Geology, 2003, no. 4.

2. Flaas A.S., Geotektonika (metodicheskie priemy paleotektonicheskogo analiza) (Geotectonics (methodical ways of paleotectonic analysis)), Perm': PGTU Publ., 2008, 197 p.

3. Flaas A.S., Chernova M.L., Vestnik PGTU. Geologiya, geoinformatsionnye sistemy, gorno-neftyanoe delo, 2000, V. 3, pp. 42-46.

4. Flaas A.S., Chernova M.L., Geologiya i poleznye iskopaemye Zapadnogo Urala, 2001, pp. 26-28.

5. Flaas A.S., Problemy mineralogii, petrografii i metallogenii PGU, 2004, V. 6, pp. 91-94.

6. Flaas A.S., Geologiya, geofizika i razrabotka neftyanykh i gazovykh mestorozhdeniy, 2005, no. 9-10, pp. 18 – 23.

7. Nassonova N.V., Romanchev M.A., Geologiya nefti i gaza - The journal Oil and Gas Geology, 2011, no. 4.


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