A Late Carboniferous olistostrome at the front of the Southern Tian Shan nappes (Kadamzhai and Khaidarkan deposits, Kyrgyzstan)

• Autorzy: Hnylko Oleh , Tsukornyk Ihor , Heneralova Larysa , Dvorzhak Oleksiy

Identyfikatory

DOI

10.7306/gq.1478

• Języki publikacji: EN

Abstrakty

EN

A Late Carboniferous (Early Moscovian) olistostrome developed in the Kadamzhai and Khaidarkan gold-antimony-mercury deposits on the Alay Ridge northern slope (Kyrgyzstan), at the front of the Late Paleozoic Southern Tian Shan nappes, is characterized. It comprises a sub-nappe olistostrome in a collisional tectonic setting. The olistostrome contains olistoliths and olistoplaques containing parts of the mid-Paleozoic sedimentary successions belonging to the parautochthon and lower nappes of the northern Bukantau-Kokshaal branch of the Southern Tian Shan nappe belt. The olistostrome accumulated ahead the advancing nappes in the foredeep basin that was filled with turbidities and debris-flow deposits (Tolubai Formathion). The parautochthon was partly dismembered into thrust limestone sheets which disintegrated and slid into unconsolidated sediments of the foredeep basin, forming large limestone olistoliths and olistoplaques. Olistoliths containing shales and bedded cherts were slid from the lower nappes. Tectonic breccias up to melange scale are present in some olistoliths, suggesting tectonic disintegration within the nappe pile and the subsequent sliding of the tectonized blocks into the olistostrome basin. Ore-bearing silicified rocks (so-called “jasperoids”) with antimony-mercury and gold mineralization are located predominantly along the contacts of the limestone olistoliths/olistoplaques with a terrigenous matrix.

Słowa kluczowe

EN

olistostrome; nappe; Southern Tian Shan; Kadamzhai; Khaidarkan; Kyrgyzstan

• Wydawca: Państwowy Instytut Geologiczny - Państwowy Instytut Badawczy
• Czasopismo: Geological Quarterly
• Rocznik: 2019
• Tom: Vol. 63, No. 2
• Strony: 407--423
• Opis fizyczny: Bibliogr. 56 poz., fot., mapa, rys., tab., wykr.

Twórcy

autor

Hnylko Oleh

• Institute of Geology and Geochemistry of Combustible Minerals of NAS of Ukraine, Naukova 3a, Lviv 79060, Ukraine

autor

Tsukornyk Ihor

• Ivan Franko National University of Lviv, Faculty of Geology, Mykhaila Hryshevskoho 4, Lviv 79005, Ukraine

autor

Heneralova Larysa

• Ivan Franko National University of Lviv, Faculty of Geology, Mykhaila Hryshevskoho 4, Lviv 79005, Ukraine

autor

Dvorzhak Oleksiy

• Ivan Franko National University of Lviv, Faculty of Geology, Mykhaila Hryshevskoho 4, Lviv 79005, Ukraine

Bibliografia

• 1. Alexeiev, D.V., Kröner, A., Hegner, E., Rojas-Agramonte, Y., Biske, Y.S., Wong, J., Geng, H.Y., Ivleva, E.A., Mühlberg, M., Mikolaichuk, A.V., Liu, D., 2016. Middle to Late Ordovician arc system in the Kyrgyz Middle Tianshan: from arc-continent collision to subsequent evolution of a Palaeozoic continental margin. Gondwana Research, 39: 261-291.
• 2. Aristov, V.A., Chernyshuk, V.P., 1984. New data on stratigraphy of siliceous sediments of the Southern Tien Shan (in Russian). Doklady Akademii Nauk SSSR, 274: 417-421.
• 3. Belousov, V.I., 1998. On the role of olistostromes and nappes in the geology of the Turkestan-Alay (in Russian). Geologiya i razvedka, 6: 33-45.
• 4. Belousov, V.I., Beer, M.A., 1989. Flysch-olistostrome formation of the Alay (in Russian). Izvestiya vysshikh uchebnykh zavedeniy. Geologiya i razvedka, 6: 3-12.
• 5. Belov, S.I., Aksenov V.A., Aksenenko V.V., 1991.State geological map of the USSR. Scale 1:50,000. South Fergana mercury-antimony belt. Turkestan-Alay group of the sheets (in Russian). Archives of the South Kyrgyz Geological Expedition, Osh, Kyrgyztan.
• 6. Biske, Yu.S., 1983. Shaly melange of Maidan and overthrusts of the Southern Ferghana (in Russian). Vestnik of Leningrad University, Series 6: 40-45.
• 7. Biske, Yu.S., 1996. Paleozoic Structure and History of Southern Tian-Shan (in Russian). Leningrad State University, Leningrad.
• 8. Biske, Yu.S., 2015. Geology and evolution of the Central Asian orogenic belt in Kazakhstan and the western Tianshan. In: The Central Asian Orogenic Belt. Geology, Evolution, Tectonics and Models (ed. A. Kroner): 6-49. Borntraeger Science Publishers, Stuttgart.
• 9. Biske, Yu.S., 2018. The Southern Tian-Shan: upgrading the geologic synthesis (in Russian). Vestnik of Saint-Petersburg University. Earth Sciences, 63: 416-452.
• 10. Biske, Yu.S., Seltmann, R., 2010. Paleozoic Tian-Shan as a transitional region between the Rheic and Urals-Turkestan oceans. Gondwana Research, 17: 602-613.
• 11. Bolgar, B.D., Rezvoy, P.D., 1971. Materials on the morphology of thrust structures in the Alay Range (in Russian). Geologicheskiy sbornik Lvovskogo universiteta, 13: 179-182.
• 12. Burtman, V.S., 1976. Structural Evolution of Paleozoic Fold Systems (Variscides of Tian-Shan and Caledonides of Northern Europe) (In Russian). Nauka, Moscow.
• 13. Burtman, V.S., 2006. Tien Shan and high Asia. Tectonics and Geodynamics in the Paleozoic (in Russian). GEOS, Moscow.
• 14. Burtman, V.S., 2015. Tectonics and geodynamics of the Tian Shan in the middle and late Paleozoic. Geotectonics, 49: 302-319.
• 15. Burtman, V.S., Schmidt, O.A., 1970. Investigation of the folded structure of the Teghermach Nappe remnant (in Russian). Proceedings of the USSR Academy of Sciences, 190: 1165-1168.
• 16. Cieszkowski, M., Golonka, J., Krobicki, M., Ślączka, A., Oszczypko, N., Waśkowska, A., Wendorff, M., 2009. The Northern Carpathians plate tectonic evolutionary stages and origin of olistoliths and olistostromes. Geodynamica Acta, 22: 101-126.
• 17. Cherenkov, I.N., 1964. Landfalls and landslides in the flysch deposits of the Karavshin river basin (northern slope of the Turkestan Range) (in Russian). Litologiya i poleznyye iskopayemyye, 6: 112-115.
• 18. Cherenkov, I.N., 1973. Upper Paleozoic flysch formation of the Gissar-Alay (in Russian). Donish, Dushanbe.
• 19. Chernyshuk, V.P., 1986. Olistostromes of the Turkestan-Alay (in Russian). Izvestiya Akademii Nauk SSSR, seriya geologicheskaya, 1: 57-63.
• 20. Dobretsov, N.L., Berzin, N.A., Buslov, M.M., 1995. Opening and tectonic evolution of the Paleo-Asian Ocean. International Geology Review, 37: 335-360.
• 21. Djenchuraeva, A.V., 1979. Stratigraphy and foraminifera of Middle Carboniferous deposited northern slopes of Turkestan-Alay (in Russian). Ilim, Frunze.
• 22. Festa, A., Pini, G.A., Dilek, Y., Cadegone, G., 2010. Mélanges and mélange-forming processes: a historical overview and new concepts. International Geology Review, 52: 1040-1105.
• 23. Festa, A., Ogata, K., Pini, G.A., Dilek, Y., Alonso, J.L., 2016. Origin and significance of olistostromes in the evolution of orogenic belts: a global synthesis. Gondwana Reseach, 39: 180-203.
• 24. Flores, G., 1955. Les résultats des études pour les recherches pétroliféres en Sicile: discussion. Proceedings of the 4th World Petroleum Congress, Section 1/A/2. Casa Editrice Carlo Colombo, Rome: 121-122.
• 25. Flores, G., 1959. Evidence of slump phenomena (Olistostromes) in areas of hydrocarbon exploration in Sicily. Proceedings 5th World Petroleum Congress, Section 1, pap. 13, Roma: 259-275.
• 26. Ghes, M.D., 2008. Terrain structure and geodynamic evolution of Caledonian Tian-Shan (in Russian). National Academy of Science of Kyrgyzstan, Bishkek.
• 27. Golonka, J., Krobicki, M., Pająk, J., Nguyen Van Giang, Zuchiewicz, W., 2006. Global Plate Tectonics and Paleogeography of Southeast Asia. Faculty of Geology, Geophysics and Environmental Protection, AGH University of Science and Technology, Kraków, Poland.
• 28. Golonka, J., Krobicki, M., Waśkowska, A., Cieszkowski, M., Ślączka, A., 2015. Olistostromes of the Pieniny Klippen Belt, Northern Carpathians. Geological Magazine, 152: 269-286.
• 29. Hsü, K.J., 1974. Mélanges and their distinction from olistostromes. Special Publication. Society of economic Paleontologists and Mineralogists, Tulsa: 321-333.
• 30. Hnylko, O.M., 2000. Chaotic formation of south-western part of the Krosno Zone - the products of origin and development of Dukla Nappe (Ukrainian Carpathians) (in Ukrainian). Geodynamics, 3: 65-74.
• 31. Hnylko, O., 2014. Olistostromes in the Miocene salt-bearing folded deposits at the front of the Ukrainian Carpathian orogen. Geological Quarterly, 58 (3): 381-392.
• 32. Konopelko, D., Wilde, S.A., Seltmann, R., Romer, R.L., Biske, Yu.S., 2018. Early Permian intrusions of the Alai range: understanding tectonic settings of Hercynian post-collisional magmatism in the South Tien Shan, Kyrgyzstan. Lithos, 302-303: 405-420.
• 33. Kukhtikov, M.M., Vinnichenko, G.P., Cherenkov, I.P., 1983. Olistostromes of the folded regions of the Pamir and Gissar-Alay (in Russian). In: Tektonika Tyan'-Shanya i Pamira (eds. I.E. Gubin and S.A. Zakharov): 78-86. Science, Moscow.
• 34. Kurenkov, S.A., 1978. Serpentinite melange and olistostrome complexes of the Alay Range (South Tien Shan) (in Russian). Geotektonika, 5: 84-93.
• 35. Leonov, M.G., 1981. Olistostromes in the structure of the folded regions (in Russian). Nauka, Moscow.
• 36. Lucente, C.C., Pini G.A., 2008. Basin-wide mass-wasting complexes as markers of the Oligo-Miocene foredeep-accretionary wedge evolution in the Northern Apennines, Italy. Basin Research, 20: 49-71.
• 37. Mikhailov, A.Y., 1947. On the origin of limestone blocks (cliffs) in the Lower Carboniferous sediments of the eastern part of the Alay Range (in Russian). Byulleten' Mokovskogo obshchestva ispytateley prirody, 22: 33-48.
• 38. Nenakhov, V.M., Belov, S.I., 2000. Features of the formation of some dislocation structural-material complexes and folded structures of the northern slope of the Alay Range (in Russian). Vestnik Voronezhskogo universiteta, Geologiya, 5: 15-20.
• 39. Nenakhov, V.M., Lytochkin, V.Yu., Perfilyev, A.S., Kuznetsov, L.V., Stavsky, A.P., Morozov, O.L., Safonov, V.G., Berezner, O.S., Semenov, G.G., Mukhaylenko, V.G., 1992. Geological mapping of chaotic complexes (in Russian). Roskomnedra, Geokart, Moscow.
• 40. Nevolko, P.A., Hnylko, O.M., Mokrushnikov, V.P., Gibsher, A.S., Redin, Yu.O., Zhimulev, F.I., Drovzhak, A.E., Svetlitskaya, T.V., Fomynikh, P.A., Karavashkin, M.I., 2019. Geology and geochemistry of the Kadamzhai and Chauvai gold-antimony-mercury deposits: implications for new province of Carlin-type gold deposits at the Southern Tien Shan (Kyrgyzstan). Ore Geology Reviews, 105: 551-571.
• 41. Osmonbetov, K.O., Knauf, V.I., Korolev, V.T., eds., 1982. Stratified and intrusive formations of Kyrgyzstan. Volume 1 and 2 (in Russian). Ilim, Frunze.
• 42. Porshnyakov, G.S., 1968. On the tectonic position of limestone with a “mixed” fauna in the Middle Carboniferous of the Alay (in Russian). In: Voprosy regionalnoy geologii (ed. V.N. Ognev): 44-52. Leningrad State University Publishing House, Leningrad.
• 43. Porshnyakov, G.S., 1973. The Hercynides of Alay and Adiacent Southern Tien-Shan (in Russian). Leningrad University, Leningrad.
• 44. Richter, D., 1973. Olisthostrom, Olistholit, Olisthorymma und Olisthoplaka als Merkmale von Gleistungsund Resedimentationsvorgangen infolge synsedimentarer tectogenetischer Bewengungen in Geosynklinalbereichen. Neues Jahrbuch für Geologie und Palaeontologie Abhandlungen, 143: 304-344.
• 45. Sabirov, A.A., ed., 2012. Stratigraphic Dictionary of the Phanerozoic of Tajikistan (Northern, Central and South-Western Tajikistan) (in Russian). Nedra, Dushanbe.
• 46. Safonova, I., Kotlyarov, A., Krivonogov, S., Xiao, W., 2017. Intra-Oceanic arcs of the Paleo-Asian Ocean. Gondvana Research, 50: 167-194.
• 47. Vaulin, O.V., 2016. Structurally-material complexes of Turkestan-Alay. Geodynamics. Geochemistry. Metallogeny. Ore content (in Russian). Rokizol. Bishkek.
• 48. Vishnevsky, L.I., Savochkina, E.N., Soloveva, M.N., 1978. Wild Flysch of the northern slope of the Alay Range (South Fergana) (in Russian). Byulleten' Moskovskogo obshchestva ispytateley prirody, Otdeleniye geologicheskoye, 1: 146-147.
• 49. Vishnevsky, L.I., Alekseev, A.S., Soloveva, M.N., 1982. Upper Paleozoic olistostrome strata of the northern slope of the Alay Range (South Fergana) (in Russian). Doklady Akademii Nauk SSSR (Reports of the USSR Academy of Sciences), 266: 936-940.
• 50. Wendorff, M., 2005. Lithostratigaphy of Neoproterozoic syn-rift sedimentary megabreccia from Mwambashi, Copperbelt of Zambia, and correlation with olistostrome succession from Mufulira. South African Journal of Geology, 108: 505-524.
• 51. Windley, B.F., Alexeiev, D., Xiao, W., Kroner, A., Badarch, G., 2007. Tectonic models for accretion of the Central Asian Orogenic Belt. Journal of the Geological Society of London, 164: 31-47.
• 52. Zhdan, A.V., 1985. About tectonic confinement of some ore manifestations of the Alay Range (in Russian). Geotektonika, 2: 57-66.
• 53. Zonenshain, L.P., Kuzmin, M.I., Natapov, L.M., 1990. Geology of the USSR: a plate-tectonic synthesis. Geodynamic Series 21. American Geophysical Union, Washington.
• 54. Zubtsov, S.E., 1997. New interpretation of collisional deformations in the Hercynides of the Alay Range (in Russian). Vestnik Sankt-Peterburgskogo universiteta, Seriya 7 , 4: 25-40.
• 55. Zubtsov, S.E., Porshnyakov, G.S., 1995. The structure and history of the formation of the Kauzan anticlinaloid (Southern Tien Shan) (in Russian). In: Voprosy stratigrafii i regional'noy geologii (eds. V.A. Prozorovsky and V.M. Tzeisler): 166-190. Publishing House of St. Petersburg University, St. Petersburg.
• 56. Zubtsov, Y.I., Porshniakov, G.S., Yagovkin, A.V., 1974. New sketch of pre-Mesozoic tectonics of Tian-Shan (in Russian). Doklady Akademii Nauk SSSR, 217: 1153-1156.

Uwagi

Opracowanie rekordu w ramach umowy 509/P-DUN/2018 ze środków MNiSW przeznaczonych na działalność upowszechniającą naukę (2019).