Rola procesów tektonicznych oraz eustatycznych w rozwoju sekwencji stratygraficznych utworów neoproterozoiku i kambru basenu lubelsko-podlaskiego

Pacześna, J.; Poprawa, P.

Powiadomienia systemowe

Sesja wygasła!

Artykuł - szczegóły

Tytuł artykułu

Rola procesów tektonicznych oraz eustatycznych w rozwoju sekwencji stratygraficznych utworów neoproterozoiku i kambru basenu lubelsko-podlaskiego

Autorzy

Pacześna J. , Poprawa P.

Treść / Zawartość

Pełne teksty:

Pobierz

Identyfikatory

Warianty tytułu

Relative role of tectonic and eustatic processes in development of the Neoproterozoic and Cambrian stratigraphic sequences of the Lublin-Podlasie Basin

Języki publikacji

Abstrakty

Sequence stratigraphy approach has been applied for the Neoproterozoic to Cambrian sedimentary fill of the Lublin–Podlasie Basin; the main goal of the study is to discriminate between eustatic and tectonic control of the observed sequence development. The Neoproterozoic and Cambrian sedimentary fill of the Lublin–Podlasie Basin is subdivided here into two second-order depositional sequences, separated by a basin-wide unconformity. The lower sequence A is poorly recognised. It is presumably of the early Neoproterozoic age, and is characterized by continental to costal shallow marine developments. Sequence B comprises the (late?) Neoproterozoic to Middle Cambrian. The lowermost part of the sequence B is composed of a lowstand systems tract (LST). At that time a low relative sea level was con-trolled by regional thermal doming, followed by rapid clastic and volcanogenic deposition, with rate exceeding that of subsidence of extensional grabens. During the latest Ediacaran, a transgressive systems tract I (TST I) developed. Increase of the rate of relative sea level rise was induced by a transition from syn-rift to post-rift subsidence. During the development of a following highstand systems tract I (HST I), significant sediment supply exceeded the rate of basement subsidence, causing progradation of shoreline. The next higher up-section transgressive system tract (TST II) is characterized by a gradual rela-tive sea level increase and reflects continued thermal sag phase of the Lublin–Podlasie Basin. Development of the TST II was coeval with a global transgression and controlled mainly by eustatic sea level rise. The beginning of the Middle Cambrian corresponds to the development of a HST II, controlled by a low rate of increase of the relative sea level, even if it was coeval in time with the Hawke Bay regression. The HST II is therefore interpreted here as controlled by local tectonic processes, superimposed on continued post-rift thermal subsidence of the passive margin.

Słowa kluczowe

basen lubelsko-podlaski basen sedymentacyjny neoproterozoik kambr stratygrafia sekwencji

Lublin-Podlasie Basin Neoproterozoic Cambrian sequence stratigraphy

Wydawca

Państwowy Instytut Geologiczny - Państwowy Instytut Badawczy

Czasopismo

Przegląd Geologiczny

Rocznik

2005

Tom

Vol. 53, nr 7

Strony

562--571

Opis fizyczny

bibliogr. 44 poz., fot., wykr.

Twórcy

autor

Pacześna J.

jolanta.paczesna@pgi.gov.pl

Państwowy Instytut Geologiczny, ul. Rakowiecka 4, 00-975 Warszawa

autor

Poprawa P.

pawel.poprawa@pgi.gov. pl

Państwowy Instytut Geologiczny, ul. Rakowiecka 4, 00-975 Warszawa

Bibliografia

1. AREN B. 1982 - Lithological and facies development of the upper Vendian in the eastern Poland. Prz. Geol., 30: 225-230
2. BOGDANOVA S.V., PASHKEVICH I.K., GORBATSCHEV R. & ORLYUK M.I. 1997 - Riphean rifting and major Palaeoproterozoic crustal boundaries in the basement of the East European Craton: geology and geophysics. Tectonophysics, 268: 1-21.
3. BOND G.C., NICKESON P.A. & KOMINZ M.A. 1984 - Breakup of a supercontinent between 625 Ma and 555 Ma: new evidence and implications for continental histories. Earth Planetary Sci. Letters, 70: 325-345.
4. BRASIER M. 1980 - The Lower Cambrian transgression and glauconite-phosphate facies in western Europe. J. Geol. Soc. London, 137: 695-703.
5. CALVER C.R. & WALTER M.R. 2000 - The Late Neoproterozoic Grassy Group of King Island, Tasmania: correlation and palaeogeographic significance. Precambrian Res., 100: 299-312.
6. COMPSTON W., SAMBRIDGE M.S., REINFRANK R.F., MOCZYDLOWSKA M., VIDAL G. & CLAESSON S. 1995 - Numerical ages of volcanic rocks and the earliest faunal zone within the Late Precambrian of east Poland. J. Geol. Soci. London, 152: 599-611.
7. CRAWFORD A.J., STEVENS B.PJ. & FANNING M. 1997 - Geochemistry and tectonic setting of some Neoproterozoic and Early Cambrian volcanics in western New South Wales. J. Geol. Soc. Australia, 26: 353-361.
8. ERIKSSON P.G., CONDIE K.C., TIRSGAARD H., MUELLER W.U., ALTERMANN W., MIALL A.D., ASPLER L.B., CATUNEANU O. & CHIARENZELLI J.R. 1998 - Precambrian clastic sedimentation systems. Sedimentary Geology, 120: 5-53.
9. FEDO C.M. & COOPER J.D. 1990 - Braided fluvial to marine transition: the basal Lower Cambrian Wood Campon Formation, Southern Marble Mountains, Majave Desert, California. J. Sedimentary Petrology, 60: 220-234.
10. FEDO C.M. & COOPER J.D. 2001 - Sedimentology and sequence stratigraphy of Neoproterozoic and Cambrian units across a craton-margin hinge zone, southeastern California, and implications for the early evolution of the Cordilleran margin. Sedimentary Geology, 141-142: 466-501.
11. GARETSKY R.G. (red.) 1981 - Geology of the western part of the East-European Platform. Publishing Nauka i Tehnika, Minsk.
12. GARETSKY R.G., ZINOVIENKO G.V., VISNJAKOV I.B., GLUSKO V.V., POMJANOVSKAJA G.M. & LVOV G.M. 1987 - Die perikratone Baltik-Dnestr-Senkungszone. Zeitschrift fur angewandte Geologie, 33: 207-213.
13. GRADSTEIN F.M., OGG J. & SMITH A.G. (red.) 2004 - A Geologic Time Scale. Cambridge University Press, Cambridge.
14. JAWOROWSKI K. 1978 - Charakterystyka sedymentologiczna osadów morskich z pogranicza prekambru i kambru. Pr. Inst. Geol., 90: 145-151.
15. JAWOROWSKI K. 1997 - Warunki depozycji ciał piaszczystych kambru dolnego i środkowego w polskiej części platformy wschodnioeuropejskiej. Biul. Państw. Inst. Geol., 377.
16. JAWOROWSKI K. 2000 - Facies variability in the Cambrian deposits from the Kościerzyna and Gdańsk sections (Pomeranian Caledonides foreland, northern Poland): a comparative study. Geol. Quart., 44: 249-260.
17. JAWOROWSKI K. & SIKORSKA M. 2003 - Composition and provenance of clastic material in the Vendian-lowermost Cambrian from Northern Poland: geotectonic implications. Pol. Geol. Inst. Spec. Papers, 8.
18. KRASHENINNIKOVA O.V. (red.) 1971 - Stratigraphy of the USSR. Riphean-Vendian. Publishing Naukova Dumka, Kyiv.
19. LENDZION K. 1983a - Biostratygrafia osadów kambru w polskiej części platformy wschodnioeuropejskiej. Kwart. Geol., 27: 669-694.
20. LENDZION K. 1983b - Rozwój kambryjskich osadów platformowych Polski. Prace Instytutu Geologicznego, 105.
21. LENDZION K., MODLIŃSKI Z. & SZYMAŃSKI B. 1979 - Trema- dok Lubelszczyzny. Kwart. Geol., 23: 713-724.
22. MAHNATSCH A.S., WERETENNIKOV N.W., SHKURATOV W.I. & BORDON W.E. 1976 - Riphean and Vendian of Belarus. Minsk.
23. MENS K.A. 1987 - Early Cambrian-Lontova Stage. [W:] Palaeogeography and Lithology of the Vendian and Cambrian of the western East-European Platform. Wyd. Geol., Warszawa: 32-37.
24. MOCZYDŁOWSKA M. 1991 - Acritarch biostratigraphy of the Lower Cambrian and the Precambrian-Cambrian boundary in southeastern Poland. Fossils and Strata, 29: 1-97.
25. MOCZYDŁOWSKA M. 1998 - Cambrian acritarchs from Upper Silesia, Poland - biochronology and tectonic implications. Fossils and Strata, 46: 1-121.
26. MYROW P.M. 1995 - Neoproterozoic rocks of the Newfoundland Avalon Zone. Precambrian Research, 73: 123-136.
27. NIKISHIN A.M., ZIEGLER P.A., STEPHENSON R.A., CLOETHINGH S.A.P.L., FURNE A.V., FOKI P.A., ERSHOV A.V., BOLOTOV S.N., KOROTAEV M.V., ALEEKSEEV A.S., GORBACHEV V.I., SHIPILOV E.V., LANKREIJER A., BEMBINOVA E.YU. & SHALIMOV I.V. 1996 - Late Permian to Triassic history of the East European Craton: dynamics of sedimentary basin evolution. Tectonophysics, 268: 23-63.
28. PACZESNA J. 1996 - Upper Vendian and Cambrian ichnocoenose from the Polish part of the East European Craton. Pr. Państw. Inst. Geol., 152: 1-77.
29. PACZESNA J. 2001 - An application of trace fossils in the facies analysis and high-resolution sequence stratigraphy - an example from the Cambrian of the Polish part of the East European Craton. Prz. Geol., 49: 1137-1146.
30. PACZESNA J. & POPRAWA P. 2005 (w druku) - Eustatic versus tectonic control on development of the Neoproterozoic and Cambrian stratigraphic sequences of the Lublin-Podlasie Basin (SW margin of Baltica). Geosciences Journal.
31. PALMER A.R. & JAMES N.P. 1980 - The Hawke Bay event: a cir- cum Iapetus regression near the Lower-Middle Cambrian boundary. [W:] Wones D.R. (red.) - The Caledonides in the USA. Virginia Polytechnic Institute State University Department of Geological Sciences Memoir, 2: 15-18.
32. POPRAWA P. & PACZESNA J. 2002 - Late Neoproterozoic to Early Paleozoic development of a rift at the Lublin-Podlasie slope of the East European Craton - analysis of subsidence and facies record. Prz. Geol., 50: 49-61.
33. POPRAWA P., ŠLIAUPA S., STEPHENSON R.A. & LAZAUSKIENE J. 1999 - Late Vendian-Early Palaeozoic tectonic evolution of the Baltic basin: regional implications from subsidence analysis. Tectonophysics, 314: 219-239.
34. POŻARSKI W. & KOTAŃSKI Z. 1979 - Tectonic development of the Baikalian and Caledonian-Variscan foreland of the East European Platform in Poland. Geological Quarterly, 23: 7-19.
35. ROZANOV A.YU. & ŁYDKA K. 1987 - Palaeogeography and lithology of the Vendian and Cambrian of the western East European Platform. Wyd. Geol.
36. RYKA W. 1984 - Precambrian evolution of the East-European Platform in Poland. Biul. Inst. Geol., 347: 17-28
37. SEMENENKO N.P. (red.) 1968 - Riphean volcanism and metallization of the western part of the Ukrainian Shield. Publishing Naukova Dumka, Kiev.
38. SIMPSON E.L. & ERIKSSON K.A. 1989 - Sedimentology of the Unicoi Formation in southern and central Virginia: evidence for late Proterozoic to early Cambrian rift-to-passive margin transition. J. Geol. Soc. Amer., 101: 42-54.
39. SIMPSON E.L. & ERIKSSON K.A. 1990 - Early Cambrian progradational and transgressive sedimentation in Virginia: an example of the early history of a passive margin. J. Sediment. Petrol., 60: 84-100.
40. VELIKANOV V.A. & KORENCHUK L.V. 1997 - Phases of magma- tism and their relation to the sediment deposition in the Late Precambrian (Riphean-Vendian) of the Volhyn-Podolia. Geol. J., 1-2: 124-131.
41. VIDAL G. & MOCZYDŁOWSKA M. 1995 - The Neoproterozoic of Baltica - stratigraphy, palaeobiology and general geological evolution. Precambrian Res., 73: 197-216.
42. VIDAL G. & MOCZYDŁOWSKA M. 1996 - Vendian-Lower Cambrian acritarch biostratigraphy of the central Caledonian fold belt in Scandinavia and the palaeogeography of the Iapetus-Tornquist seaway. Norsk Geologisk Tidsskrift, 76: 147-168.
43. WALTER M.R., VEEVERS J.J., CALVER C.R. & GREY K. 1995 - Neoproterozoic stratigraphy of the Centralian Superbasin, Australia. Precambrian Research, 73: 173-195.
44. WICHROWSKA M. 1992 - Riphean on cratonic area of Poland. Prz. Geol., 2: 94-99.

Typ dokumentu

Bibliografia

Identyfikator YADDA

bwmeta1.element.baztech-article-BUS2-0014-0080