Baltic-Iranian super lineament — long-lived Trans-Eurasian belt of dislocations and planetary megafractures
Рубрика:
| 1Pokalyuk, VV, 2Lomakin, IE, 1Verkhovtsev, VG 1State Scientific Institution “Institute of Environmental Geochemistry, National Academy of Sciences of Ukraine", Kyiv, Ukraine 2State Scientific Institution "Center for Problems of Marine Geology, geoecology and sedimentary ore formation National Academy of Sciences of Ukraine", Kyiv, Ukraine |
| Space Sci. & Technol. 2020, 26 ;(5):048-072 |
| https://doi.org/10.15407/knit2020.05.048 |
| Язык публикации: Ukrainian |
Аннотация: Information on fault tectonics and the deep structure of the global trans-Eurasian belt of dislocations and planetary megafractures (Baltic-Iranian Super Lineament) is generalized based on the analysis of literary, geological and geophysical, cartographic, cosmographic materials, including the results of tectonic lineaments interpretation of cosmo-images of the Earth’s surface. The features of its distribution and segmentation are clarified. This Super Lineament is the trans-Eurasian structure of a planetary rank — an integral part of the regularly spatially oriented ancient reghmatic fault net of Eurasia, formed at the early stages of the formation of the rigid earth crust under the influence of global stresses associated with the factor of rotation of the Earth. The long-lived nature of the belt (the Upper Proterozoic — Cenozoic) and its quasi-stationary position throughout its formation history, as well as the absence of large-scale, hundreds of kilometers, of shear displacements along it and at intersections with transverse tectolineament belts of a similar rank indicate the low probability of the plate-tectonic convergence model of Afro-Arabia and Eurasia. The destruction model of the once united Afro-Eurasian continent in a potentially shear field of relatively low amplitude (on a planetary scale) dislocations is preferable.
The geodynamic mode of formation and development of the belt as a whole cannot be described by any one type — riftogenic, or collisional ones. Regional and supra-regional zones of extension (riftogenic zones) and compression (collision) alternate in it periodically. It shows the global nature of the belt, the union of different geodynamic regimes in it, as well as the wave character and hierarchy of the tectonic process.
|
| Ключевые слова: Baltic-Iranian tectolineament belt, decryption of cosmo-images, geodynamics, lineament, planetary megafractures, reghmatic fault net, tectonics, Teisseyre-Tornquist Zone |
References:
1. Anokhin V. M. (2006). Global Disjunctive Network of the Earth: Structure, Origin, and Geological Implications. St. Persburg: Nedra [in Russian].
2. Afanasenkov A. P., Nikishin A. M., Obukhov A. N. (2007). Eastern Black Sea Basin: Geological Structure and Hydrocarbon Potential. Moscow: Nauchnyy Mir [in Russian].
3. Bogdanov A. A. (1964). East European Platform / Tectonics of Europe: Explained. app. to the Intern. tecton. map of Europe. 1:2500000. Moscow: Nauka [in Russian].
4. Bush V. A. (1983). Systems of transcontinental lineaments of Eurasia. Geotectonics, 3, 15—31 [in Russian].
5. Bush V. A. (1983). Eurasia Transcontinental Lineament Systems. Space Information in Geol. V. G. Trifonov, V. I. Makarov, Yu. L. Safonov, P. V. Florensky (Ed). Moscow: Nauka [in Russian].
6. Bush V. A. (1983). Transcontinental lineaments and problems of mobilism. Geotectonics, 4, 14—25 [in Russian].
7. Verkhovtsev V. G. (2010). The latest tectonics of the Western (Pre-Dobrudja) segment of the Scythian Plate and adjacent territories. Geophys. J., 32 (3), 29—42 [in Russian].
8. Garetsky R. G., Teshke G. Yu. (1977). Dobrudja-Northern Sea and Sarmatian-Turan lineaments. Orogenic stage of variscid development in Central Europe and the USSR. Moscow: Nauka [in Russian].
9. Glushko V. V. (1968). Tectonics and oil and gas potential of the Carpathians and adjacent troughs. Moscow: Nedra [in Russian].
10. Goryachev A. V. (1986). Deep faults and structural heterogeneities of the Earth’s crust. Heterogeneity of the tectonosphere and development of the Earth’s crust. Moscow: Nedra [in Russian].
11. Guterh A., Matezhok R., Payhel J., Perchutz E. (1977). The structure of the earth’s crust along the VII International Profile of the NHS in Poland. The structure of the earth’s crust and upper mantle according to seismic data. Kiev: Naukova Dumka [in Russian].
12. Zaika-Novatsky V. S., Chekunov A. V. (1970). The main features of the junction of the East European platform with the Galician folded region of Baikalides. Soviet Geol., 12, 3—15 [in Russian].
2. Afanasenkov A. P., Nikishin A. M., Obukhov A. N. (2007). Eastern Black Sea Basin: Geological Structure and Hydrocarbon Potential. Moscow: Nauchnyy Mir [in Russian].
3. Bogdanov A. A. (1964). East European Platform / Tectonics of Europe: Explained. app. to the Intern. tecton. map of Europe. 1:2500000. Moscow: Nauka [in Russian].
4. Bush V. A. (1983). Systems of transcontinental lineaments of Eurasia. Geotectonics, 3, 15—31 [in Russian].
5. Bush V. A. (1983). Eurasia Transcontinental Lineament Systems. Space Information in Geol. V. G. Trifonov, V. I. Makarov, Yu. L. Safonov, P. V. Florensky (Ed). Moscow: Nauka [in Russian].
6. Bush V. A. (1983). Transcontinental lineaments and problems of mobilism. Geotectonics, 4, 14—25 [in Russian].
7. Verkhovtsev V. G. (2010). The latest tectonics of the Western (Pre-Dobrudja) segment of the Scythian Plate and adjacent territories. Geophys. J., 32 (3), 29—42 [in Russian].
8. Garetsky R. G., Teshke G. Yu. (1977). Dobrudja-Northern Sea and Sarmatian-Turan lineaments. Orogenic stage of variscid development in Central Europe and the USSR. Moscow: Nauka [in Russian].
9. Glushko V. V. (1968). Tectonics and oil and gas potential of the Carpathians and adjacent troughs. Moscow: Nedra [in Russian].
10. Goryachev A. V. (1986). Deep faults and structural heterogeneities of the Earth’s crust. Heterogeneity of the tectonosphere and development of the Earth’s crust. Moscow: Nedra [in Russian].
11. Guterh A., Matezhok R., Payhel J., Perchutz E. (1977). The structure of the earth’s crust along the VII International Profile of the NHS in Poland. The structure of the earth’s crust and upper mantle according to seismic data. Kiev: Naukova Dumka [in Russian].
12. Zaika-Novatsky V. S., Chekunov A. V. (1970). The main features of the junction of the East European platform with the Galician folded region of Baikalides. Soviet Geol., 12, 3—15 [in Russian].
13. Znosko E., Petrenko V. S., Chirvinskaya M. V. (1977).The main features of the tectonic structure of the western edge of the Russian plate and its surroundings. Moscow Univer. Bull. Ser. Geol., 3, 21—30 [in Russian].
14. Bagrov N. V., Shnyukov E. F., Maslakov N. A., Shnyukova E. E., Pasynkov A. A., Glushchenko I. V., et al. (2012). Map of the bottom topography of the Black and Azov Seas 1: 1250000. Simferopol : Department of Marine Geol. and Sedimentary Ore Formation of the National Academy of Sciences of Ukraine, Tauride National University of the Ministry of Education and Science of Ukraine, SIC “Technologies for Sustainable Development” TNU
15. Catterfeld G. N., Charushin G. V. (1970). Global Fracturing of the Earth and Other Planets. Geotectonics, 6, 3—12 [in Russian].
16. Krasheninnikova O. V. (1960). Riphean deposits of the Ukrainian SSR and the conditions for their formation. International Geological Congress, XXI session. Late Precambrian and Cambrian stratigraphy (Repts. of Soviet geologists). Moscow: Academy of Sciences of the USSR [in Russian].
17. Mezhelovsky N. V. (1987). (Eds). Cosmotectonic map of the European countries — members of the CMEA and the SFRY. 1: 1 000 000. CMEA
18. Lomakin I. E., Pokalyuk V. V., Kochelab V. V., Shuraev I. N. (2018). The Azov-Adriatic megalineament — a trans-regional zone of conjugated deep faults in the south of Europe. Geol. and minerals of the oceans, 2, 29—47 [in Russian].
19. Hain V. E., Leonov Yu. G (Eds). (1996). International tectonic map of Europe. 1: 5 000 000. Third edition. UNESCO, RAS
20. Mokryak I. M. (2014). On the question of the position of the western border of the Eastern European Platform. Mineral resources of Ukraine, 2, 15—19 [in Ukrainian].
21. Trifonov V. G., Dodonov A. E., Bachmanov D. M., Ivanova T. P., Karakhanyan A. S., et al. (2012). Neotectonics, modern geodynamics and seismic hazard of Syria. Proc. Geol. Institute. Vol. 598. Moscow: GEOS [in Russian].
22. Petrenko V. S., Pozharisky V. (1972). The problem of the tectonic structure of the southwestern margin of the East European platform. News of higher educational institutions. Ser. Geol. and exploration, 4, 17—24 [in Russian].
14. Bagrov N. V., Shnyukov E. F., Maslakov N. A., Shnyukova E. E., Pasynkov A. A., Glushchenko I. V., et al. (2012). Map of the bottom topography of the Black and Azov Seas 1: 1250000. Simferopol : Department of Marine Geol. and Sedimentary Ore Formation of the National Academy of Sciences of Ukraine, Tauride National University of the Ministry of Education and Science of Ukraine, SIC “Technologies for Sustainable Development” TNU
15. Catterfeld G. N., Charushin G. V. (1970). Global Fracturing of the Earth and Other Planets. Geotectonics, 6, 3—12 [in Russian].
16. Krasheninnikova O. V. (1960). Riphean deposits of the Ukrainian SSR and the conditions for their formation. International Geological Congress, XXI session. Late Precambrian and Cambrian stratigraphy (Repts. of Soviet geologists). Moscow: Academy of Sciences of the USSR [in Russian].
17. Mezhelovsky N. V. (1987). (Eds). Cosmotectonic map of the European countries — members of the CMEA and the SFRY. 1: 1 000 000. CMEA
18. Lomakin I. E., Pokalyuk V. V., Kochelab V. V., Shuraev I. N. (2018). The Azov-Adriatic megalineament — a trans-regional zone of conjugated deep faults in the south of Europe. Geol. and minerals of the oceans, 2, 29—47 [in Russian].
19. Hain V. E., Leonov Yu. G (Eds). (1996). International tectonic map of Europe. 1: 5 000 000. Third edition. UNESCO, RAS
20. Mokryak I. M. (2014). On the question of the position of the western border of the Eastern European Platform. Mineral resources of Ukraine, 2, 15—19 [in Ukrainian].
21. Trifonov V. G., Dodonov A. E., Bachmanov D. M., Ivanova T. P., Karakhanyan A. S., et al. (2012). Neotectonics, modern geodynamics and seismic hazard of Syria. Proc. Geol. Institute. Vol. 598. Moscow: GEOS [in Russian].
22. Petrenko V. S., Pozharisky V. (1972). The problem of the tectonic structure of the southwestern margin of the East European platform. News of higher educational institutions. Ser. Geol. and exploration, 4, 17—24 [in Russian].
23. Pokalyuk V. V., Lomakin I. E., Shuraev I. N. (2018). Tectonic-lineament zones of East-north-east trending as constituent element of a rhegmatogenic fault network of the Balkan-Black Sea region. Ukr. J. Remote Sensing of the Earth, 18, 40—52 [in Russian].
24. Rasvetsaev L. M., Tveritinova T. Yu. (2016). Earth rotation and planetary zones of cleavage, compression, and tension. Fourth Tectonophysical Conference. Section 5. General theoretical issues of tectonophysics and problems of geodynamics. Moscow: IPE RAS. V. 2. Р. 545—552 [in Russian].
25. Rasvetsaev L. M. (1980). Regular structural drawing of the earth’s surface and its dynamic interpretation. Problems of global correlation of geological phenomena. Moscow: Nauka, 145—216 [in Russian].
26. Rasvetsaev L. M. (1987). Identification of paragenetic families of tectonic disjunctives as a method of paleogeomechanical analysis of stress fields and deformations of the earth’s crust. Fields of stresses and deformations in the earth’s crust. Moscow : Nauka, 171—181 [in Russian].
27. Skaryatin V. D., Atanasyan S. V. (1976). Linear and ring structures of some regions of Eurasia. News of higher educational institutions. Geol. and exploration, 11, 135—148 [in Russian].
28. Tveritinova T. Yu. (2013). Lineaments as a reflection of the structural framework of the lithosphere (Lineaments — faults or phantoms?). Electronic scientific publication Almanac Space and Time. Vol. 4, 1, Special issue System «Planet Earth».[in Russian].
29. Mezhelovsky N. V. (Ch. Ed.) (1987). Tectonic structures of central and south-eastern Europe based on satellite imagery. Explanatory note to the Cosmotectonic map of the European CMEA and SFRY member countries at a scale of 1: 1 000 000. CMEA Secretariat. [in Russian].
30. Trifonov V. G. (1999). Neotectonics of Eurasia. Moscow: Nauchnyy mir [in Russian].
31. Trifonov V. G., Soboleva O. V., Trifonov R. V., Vostrikov G. A. (2002). Modern geodynamics of the Alpine-Himalayan collision belt. Moscow : GEOS. (Works GIN RAS; issue 541) [in Russian].
32. Tugolesov D. A., Gorshkov A. S., Meissner L. B., et al. (1985). Tectonics of Meso-Cenozoic sediments of the Black Sea basin Moscow: Nedra [in Russian].
33. Utrobin V. M., Vitryk S. P. (1968). The role of deep faults in the formation of the Precarpathian marginal deflection. Geol. J., 6, 39—45 [in Ukrainian].
34. Hain V. E. (2009). On the main directions in modern Earth sciences. Bull. Russian Acad. of Sci., 79 (1), 50—56 [in Russian].
35. Hain V. E. (1977). Regional geotectonics. Extra-Alpine Europe and West Asia. Moscow: Nedra [in Russian].
36. Hain V. E. (1984). Regional geotectonics. Alpine Mediterranean belt. Moscow: Nedra. Vol. 1 [in Russian].
37. Hain V. E. (2001). Tectonics of continents and oceans. Moscow: Nauchnyy mir [in Russian].
38. Khomenko V. I . (1987). The deep structure of the southwestern edge of the East European platform. Kiev: Naukova Dumka [in Russian].
24. Rasvetsaev L. M., Tveritinova T. Yu. (2016). Earth rotation and planetary zones of cleavage, compression, and tension. Fourth Tectonophysical Conference. Section 5. General theoretical issues of tectonophysics and problems of geodynamics. Moscow: IPE RAS. V. 2. Р. 545—552 [in Russian].
25. Rasvetsaev L. M. (1980). Regular structural drawing of the earth’s surface and its dynamic interpretation. Problems of global correlation of geological phenomena. Moscow: Nauka, 145—216 [in Russian].
26. Rasvetsaev L. M. (1987). Identification of paragenetic families of tectonic disjunctives as a method of paleogeomechanical analysis of stress fields and deformations of the earth’s crust. Fields of stresses and deformations in the earth’s crust. Moscow : Nauka, 171—181 [in Russian].
27. Skaryatin V. D., Atanasyan S. V. (1976). Linear and ring structures of some regions of Eurasia. News of higher educational institutions. Geol. and exploration, 11, 135—148 [in Russian].
28. Tveritinova T. Yu. (2013). Lineaments as a reflection of the structural framework of the lithosphere (Lineaments — faults or phantoms?). Electronic scientific publication Almanac Space and Time. Vol. 4, 1, Special issue System «Planet Earth».[in Russian].
29. Mezhelovsky N. V. (Ch. Ed.) (1987). Tectonic structures of central and south-eastern Europe based on satellite imagery. Explanatory note to the Cosmotectonic map of the European CMEA and SFRY member countries at a scale of 1: 1 000 000. CMEA Secretariat. [in Russian].
30. Trifonov V. G. (1999). Neotectonics of Eurasia. Moscow: Nauchnyy mir [in Russian].
31. Trifonov V. G., Soboleva O. V., Trifonov R. V., Vostrikov G. A. (2002). Modern geodynamics of the Alpine-Himalayan collision belt. Moscow : GEOS. (Works GIN RAS; issue 541) [in Russian].
32. Tugolesov D. A., Gorshkov A. S., Meissner L. B., et al. (1985). Tectonics of Meso-Cenozoic sediments of the Black Sea basin Moscow: Nedra [in Russian].
33. Utrobin V. M., Vitryk S. P. (1968). The role of deep faults in the formation of the Precarpathian marginal deflection. Geol. J., 6, 39—45 [in Ukrainian].
34. Hain V. E. (2009). On the main directions in modern Earth sciences. Bull. Russian Acad. of Sci., 79 (1), 50—56 [in Russian].
35. Hain V. E. (1977). Regional geotectonics. Extra-Alpine Europe and West Asia. Moscow: Nedra [in Russian].
36. Hain V. E. (1984). Regional geotectonics. Alpine Mediterranean belt. Moscow: Nedra. Vol. 1 [in Russian].
37. Hain V. E. (2001). Tectonics of continents and oceans. Moscow: Nauchnyy mir [in Russian].
38. Khomenko V. I . (1987). The deep structure of the southwestern edge of the East European platform. Kiev: Naukova Dumka [in Russian].
39. Khortov A. V., Schlesinger A. E. (2015). The deep structure and features of the formation of the Black Sea topodepression in connection with the prospects of oil and gas. News of gas science, 2, 64—69 [in Russian].
40. Chekunov A. V. (1972). The structure of the earth’s crust and tectonics of the south of the European part of the USSR. Kiev: Naukova Dumka [in Russian].
41. Chekunov A. V. (1987). Problems of the Black Sea Depression. Geofiz. J., 9 (4), 3—25 [in Russian].
42. Chebanenko I. I., Dovgal Yu. I ., Znamenskaya T. A., et al. (1988). Tectonics of the Northern Black Sea region. Kiev: Naukova Dumka [in Russian].
43. Shatsky N. S. (1964). On the deflections of the Donetsk type. Selected Works. Moscow: Nauka. Vol. 2, 544—553 [in Russian].
44. Shatsky N.S., Bogdanov A. A. (1961). On the International Tectonic Map of Europe, scale 1:2 500 000. Proceedings of the USSR Academy of Sciences, Ser. Geol., 4, 3—25 [in Russian].
45. Stille G. (1964). Favorites Proceedings. Moscow: Mir, 602—625 [in Russian].
46. Shtoklin J. (1966). Tectonics of Iran. Geotectonics, 1, 3—21 [in Russian].
47. Schultz S. S. (1973). Planetary Fracturing (Fundamentals). Planetary Fracturing. Leningrad: Leningrad State University, 5—37 [in Russian].
48. Banks C. J., Robinson A. G. (1997). Mesozoic strike-slip back-arc basins of the western Black Sea region. Robinson A. G. (Ed.), Regional and Petroleum Geology of the Black Sea and Surrounding Region. AAPG Mem. 68, 53—62.
49. Barka A., Reilinger R. (1997). Active tectonics of the Eastern Mediterranean region: Deduced from GPS, neotectonic and seismicity data. Ann. Geofis., 40, 587—610.
50. Bogdanova S. V., Gorbatschev R., Garetsky R. G. (2005). Europe. East European Craton. Encyclopedia of Geol. Elsevier. 2, 34—49.
51. Chebanenko I. I., Klochko V. P., Tokovenko V. S. (1998). The net of global fracturing of the Carpathian-Balkanian-Dinarian orogenic system. Geol. J., No. 1-2, 9—13.
52. Dadlez R. (1994). Strike-slip movements in the Polish Lowlands. Geol. Quart., 38 (2), 307—318.
53. Diaconescu M., Craiu A., Toma-Danila D., Craiu G. M., Ghita C. (2019). Main active faults from the eastern part of Romania (Dobrogea and Black Sea). Part 1: Longitudinal fault system. Romanian Repts. in Phys., 71 (702), 18 p.
54. Dinu C.,Wong H. K., Tambrea D. (2002). Stratigraphic and tectonic syntheses of the Romanian Black Sea shelf and correlation with major land structures. Bucharest Geosci. Forum. Spec., 2, 101—117.
55. Dinu C., Wong H. K., Tambrea D., Matenco L. (2005). Stratigraphic and structural characteristics of the Romanian Black Sea shelf. Tectonophys., 410, 417—435.
56. Georgiev G. (2012). Geology and Hydrocarbon Systems in the Western Black Sea. Turkish J. Earth Sci., 21, 723—754.
57. Gradinaru E. (1988). Jurassic sedimentary rocks and bimodal volcanics of the Cielari-Camena outcrop belt: evidence for a transtensile regime of the Peceneaga-Camena Fault. St. Cerc. Geol. Geofiz. Geogr. (Geol.), 33, 97—121.
58. Hippolyte J.-C. (2002). Geodynamics of Dobrogea (Romania): new constraints on the evolution of the Tornquist-Teisseyre Line, the Black Sea and the Carpathians. Tectonophys., 357, 33—53.
59. Mazur S., Krzywiec P., Malinowski M., Lewandowski M., Aleksandrowski P., Mikołajczak M. (2018). On the nature of the Teisseyre-Tornquist Zone. Geol., Geophys. and Environment, 44 (1), 17—30.
60. Munteanu I., Matenco L., Dinu C., Cloetingh S. (2011). Kinematics of back-arc inversion of the Western Black Sea Basin. Tectonics, 30, 21 p.
40. Chekunov A. V. (1972). The structure of the earth’s crust and tectonics of the south of the European part of the USSR. Kiev: Naukova Dumka [in Russian].
41. Chekunov A. V. (1987). Problems of the Black Sea Depression. Geofiz. J., 9 (4), 3—25 [in Russian].
42. Chebanenko I. I., Dovgal Yu. I ., Znamenskaya T. A., et al. (1988). Tectonics of the Northern Black Sea region. Kiev: Naukova Dumka [in Russian].
43. Shatsky N. S. (1964). On the deflections of the Donetsk type. Selected Works. Moscow: Nauka. Vol. 2, 544—553 [in Russian].
44. Shatsky N.S., Bogdanov A. A. (1961). On the International Tectonic Map of Europe, scale 1:2 500 000. Proceedings of the USSR Academy of Sciences, Ser. Geol., 4, 3—25 [in Russian].
45. Stille G. (1964). Favorites Proceedings. Moscow: Mir, 602—625 [in Russian].
46. Shtoklin J. (1966). Tectonics of Iran. Geotectonics, 1, 3—21 [in Russian].
47. Schultz S. S. (1973). Planetary Fracturing (Fundamentals). Planetary Fracturing. Leningrad: Leningrad State University, 5—37 [in Russian].
48. Banks C. J., Robinson A. G. (1997). Mesozoic strike-slip back-arc basins of the western Black Sea region. Robinson A. G. (Ed.), Regional and Petroleum Geology of the Black Sea and Surrounding Region. AAPG Mem. 68, 53—62.
49. Barka A., Reilinger R. (1997). Active tectonics of the Eastern Mediterranean region: Deduced from GPS, neotectonic and seismicity data. Ann. Geofis., 40, 587—610.
50. Bogdanova S. V., Gorbatschev R., Garetsky R. G. (2005). Europe. East European Craton. Encyclopedia of Geol. Elsevier. 2, 34—49.
51. Chebanenko I. I., Klochko V. P., Tokovenko V. S. (1998). The net of global fracturing of the Carpathian-Balkanian-Dinarian orogenic system. Geol. J., No. 1-2, 9—13.
52. Dadlez R. (1994). Strike-slip movements in the Polish Lowlands. Geol. Quart., 38 (2), 307—318.
53. Diaconescu M., Craiu A., Toma-Danila D., Craiu G. M., Ghita C. (2019). Main active faults from the eastern part of Romania (Dobrogea and Black Sea). Part 1: Longitudinal fault system. Romanian Repts. in Phys., 71 (702), 18 p.
54. Dinu C.,Wong H. K., Tambrea D. (2002). Stratigraphic and tectonic syntheses of the Romanian Black Sea shelf and correlation with major land structures. Bucharest Geosci. Forum. Spec., 2, 101—117.
55. Dinu C., Wong H. K., Tambrea D., Matenco L. (2005). Stratigraphic and structural characteristics of the Romanian Black Sea shelf. Tectonophys., 410, 417—435.
56. Georgiev G. (2012). Geology and Hydrocarbon Systems in the Western Black Sea. Turkish J. Earth Sci., 21, 723—754.
57. Gradinaru E. (1988). Jurassic sedimentary rocks and bimodal volcanics of the Cielari-Camena outcrop belt: evidence for a transtensile regime of the Peceneaga-Camena Fault. St. Cerc. Geol. Geofiz. Geogr. (Geol.), 33, 97—121.
58. Hippolyte J.-C. (2002). Geodynamics of Dobrogea (Romania): new constraints on the evolution of the Tornquist-Teisseyre Line, the Black Sea and the Carpathians. Tectonophys., 357, 33—53.
59. Mazur S., Krzywiec P., Malinowski M., Lewandowski M., Aleksandrowski P., Mikołajczak M. (2018). On the nature of the Teisseyre-Tornquist Zone. Geol., Geophys. and Environment, 44 (1), 17—30.
60. Munteanu I., Matenco L., Dinu C., Cloetingh S. (2011). Kinematics of back-arc inversion of the Western Black Sea Basin. Tectonics, 30, 21 p.
61. Narkiewicz M., Maksym A., Malinowski M., et al. (2014). Transcurrent nature of the Teisseyre—Tornquist Zone in Central Europe: results of the POLCRUST-01 deep reflection seismic profile. Int. J. Earth Sci. (Geol. Rundsch), 104 (3), 775—796.
62. Oaie G., Seghedi A., Radulescu V. (2016). Natural marine hazards in the Black Sea and the system of their monitoring and real-time warning. Geo-Eco-Marina [e-journal], 22, 5—28.
63. Pegrum R. M. (1984). The extension of the Tornquist Zone in the Norwegian North Sea. Norsk Geologisk Tidsskrift, 64, 39—68.
64. Pharaoh T. C., Winchester J. A., Verniers J., Lassen A., Seghedi A. (2006). The Western Accretionary Margin of the East European Craton: an overview. Geol. Soc., London, Memoirs, 32, 291—311.
65. Poźaryski W. (1957). Poludniowo-zachodnia krawedz Fennosarmacii. Kwart. Geol., 1/2, No. 3/4, 383—424 [in Polish].
66. Poźaryski W., Brochwicz-Lewiński W., Tomczyk H. (1982). O heterochronicznoości linii Teisseyre’a-Tornquista. Prz. Geol., 30 (11), 569—574 [in Polish].
67. Robinson A. G. (Ed). (1997). Regional and Petroleum Geology of the Black Sea and Surrounding Regions. AAPG Memoir, 68, 385 p.
68. Robynson A. G., Rudat J. H., Banks C. J., Wyles R. L. F. (1996). Petroleum Geology of the Black Sea. Marine and Petroleum Geol., 13, 195—223.
69. Săndulescu M. (1984). Geotectonics of Romania. Bucharest: Technical Publishing House [in Romanian].
62. Oaie G., Seghedi A., Radulescu V. (2016). Natural marine hazards in the Black Sea and the system of their monitoring and real-time warning. Geo-Eco-Marina [e-journal], 22, 5—28.
63. Pegrum R. M. (1984). The extension of the Tornquist Zone in the Norwegian North Sea. Norsk Geologisk Tidsskrift, 64, 39—68.
64. Pharaoh T. C., Winchester J. A., Verniers J., Lassen A., Seghedi A. (2006). The Western Accretionary Margin of the East European Craton: an overview. Geol. Soc., London, Memoirs, 32, 291—311.
65. Poźaryski W. (1957). Poludniowo-zachodnia krawedz Fennosarmacii. Kwart. Geol., 1/2, No. 3/4, 383—424 [in Polish].
66. Poźaryski W., Brochwicz-Lewiński W., Tomczyk H. (1982). O heterochronicznoości linii Teisseyre’a-Tornquista. Prz. Geol., 30 (11), 569—574 [in Polish].
67. Robinson A. G. (Ed). (1997). Regional and Petroleum Geology of the Black Sea and Surrounding Regions. AAPG Memoir, 68, 385 p.
68. Robynson A. G., Rudat J. H., Banks C. J., Wyles R. L. F. (1996). Petroleum Geology of the Black Sea. Marine and Petroleum Geol., 13, 195—223.
69. Săndulescu M. (1984). Geotectonics of Romania. Bucharest: Technical Publishing House [in Romanian].
70. Sandulescu M., Visarion M. (1988). La structure des plate-formes situees dans l’avant-pays et au dessous des nappes du flysch des Carpathes orientales. Stud. Teh. Econ. Geofiz., 15, 61—70 [in Romanian].
71. Thybo H. (2000). Crustal structure and tectonic evolution of the Tornquist Fan region as revealed by geophysical methods. Bull. of the Geol. Soc. of Denmark, 46, 145—160.
72. Zielhui A., Nolet G. (1994). Deep Seismic Expression of an Ancient Plate Boundary in Europe. Science, New Series, 265 (5168), 79—81.
71. Thybo H. (2000). Crustal structure and tectonic evolution of the Tornquist Fan region as revealed by geophysical methods. Bull. of the Geol. Soc. of Denmark, 46, 145—160.
72. Zielhui A., Nolet G. (1994). Deep Seismic Expression of an Ancient Plate Boundary in Europe. Science, New Series, 265 (5168), 79—81.