PL EN


Preferencje help
Widoczny [Schowaj] Abstrakt
Liczba wyników
Tytuł artykułu

Czy istnieje mazurska, prawoskrętna strefa podatnego ścinania?

Autorzy
Treść / Zawartość
Identyfikatory
Warianty tytułu
EN
Does the Mazury dextral shear zone exist?
Języki publikacji
PL
Abstrakty
EN
Throughout SW Fennoscandia, numerous approximately W-E trending faults and ductile shear zones have recently been recognized. The regiona--scale zone of strike-slip displacements [Mazury lineament] with a dextral component was referred by many authors as apparently influenced by the distribution of ca. 1.6-1.4 Ga old "anorogenic" intrusions of the Mazury Complex [NE Poland]. However, new detailed structural and kinematics studies of drill-cores from 255 boreholes located throughout NE Poland and SW Lithuania [Lazdijai region] indicate that the Mazury Complex, the Suwałki Anorthosite Massif and surrounding lithotectonic domains share a common ductile thrusting deformation, calling into question the concept of a large-scale dextral shear zone and also the "anorogenic" origin hypothesis of the Mazury Complex. One important advance has been the accumulation of structural and kinematics information that allows assessment of the main orogenic transport direction commonly towards the SW, locally to the NE [e.g., in the eastern part of the Suwałki Anorthosite Massif]. This assessment has been coupled with the recognition of the role of major and numerous ductile shear zones within the western part of the East European Platform. In general, compressional deformation with ductile thrusting predominated in the western part of the East European Platform. Very probable strike of regional mylonitic foliation [S1] from almost 100 boreholes has been established, based on geophysical measurements of the curvature of borehole axis and a few tens oriented core samples [SW Lithuania]. It is assumed that the crystalline rocks of NE Poland and SW Lithuania [Lazdijai region] were subjected to similar ductile thrusting to transpressional deformation during the late Gothian [or newly defined Dano-Polonian] orogeny [ca. 1.5 Ga].
Rocznik
Strony
157--157, 167
Opis fizyczny
Bibliogr. 58 poz., rys., wykr.
Twórcy
autor
Bibliografia
  • ANDERSSON J., SÖDERLUND U., CORNELL D., JOHANSSON L. & MÖLLER C. 1999 - Sveconorwegian (-Grenvillian) deformation, metamorphism and leucosome formation in SW Sweden, SW Baltic Shield: constraints from a Mesoproterozoic granite intrusion. Precambrian Res., 98: 151-171.
  • ANDRÉASSON P.-G. & RODHE A. 1989 - Geology of the Protogine Zone south of Lake Vättern, southern Sweden: a reinterpretation. Geol. Fören. Stockholm För., 112: 107-125.
  • ASPLER L.B., CHIARENZELLI J.R. & MCNICOLL V.J. 2002 - Paleoproterozoic basement-cover infolding and thick-skinned thrusting in Hearne domain, Nunavut, Canada: intracratonic response to Trans-Hudson orogen. Precambrian Res., 16: 331-354.
  • BAGIŃSKI B. & KRZEMIŃSKA E. 2005-Various kinds of charnockitic rocks from NE Poland. Min. Soc. Poland-Sp. Papers, 26: 13-17.
  • BAGIŃSKI B., BOGDANOVA S.V. & WISZNIEWSKA J. 1999 - The first results of P-T conditions of the emplacement of the multiphase Kościerzyna intrusion. 7th EUROBRODGE Workshop "Between EUROBRIDGE and TESZ". Suwałki-Szelment, Poland 26-30.05.1999: 3-4.
  • BAGIŃSKI B., DUCHESNE J.-C., MARTIN H. & WISZNIEWSKA J. 2001a - Mid-Proterozoic granitoids from the Mazury Complex (NE Poland): AMCG affinities? EUG XI J. Conf. Abstr., 6: 768.
  • BAGIŃSKI B., DUCHESNE J.-C., MARTIN H., VANDER-AUWERA J. & WISZNIEWSKA J. 2001b - Petrology and geochemistry of rapakivi- type granites from the crystalline basement of NE Poland. Geol. Quart., 45: 33-52.
  • BERTHELSEN A. 1988 - Boornholms Fjeld. Bornholms Geologi. J. Int., 112: 325-343.
  • BEUNK F.F., PAGE L.M., WIJBRANS J.R. & BARLING J. 1996 - Deformational, metamorphic and geochronological constraints from the Loftahammar-Linköping deformation zone (LZ) in SE Sweden: implications for the development of the Svecofennian Orogen. Geol. Fören. Stockholm Förh. 118 (Jubilee Issue), A9.
  • BOGDANOVAS.V. & GORBATSCHEV R. 1997-Major crustal boundaries of the East European Craton cut by the TESZ. Terra Nostra 97/11: 24- 28.
  • BOGDANOVA S.V. 2001 - Tectonic settings of 1.65-1.4 Ga AMCG magmatism in the Western East European Craton (Western Baltica). EUG XI J. Confer. Abstr., 6: 769.
  • BOGDANOVA S.V. 2005 - The East European Craton: some aspects of the Proterozoic evolution in its south-west. Min. Soc. Poland - Sp. Papers, 26: 18-24.
  • BOGDANOVA S.V., BIBIKOVAE.V. & GORBATSCHEV R. 1994- Palaeoproterozoic U-Pb zircon ages from Belorussia: New tectonic implications for the East European Craton. Precambrian Res., 68: 231-240.
  • BOGDANOVA S.V., PAGE L.M., SKRIDLAITE G. & TARAN L.N. 1996 - The Proterozoic tectonothermal history of the western part of the East European Craton: implications from 40Ar/39Ar geochronology. GFF, 118 (Jubilee Issue): A11-A12.
  • BOGDANOVA S.V., PAGE L.M., SKRIDLAITE G. & TARAN L.N. 2001 - Proterozoic tectonothermal history in the western part of the East European Craton: Ar/Ar geochronological coinstraints. Tectonophysics, 339: 39-66.
  • BRIDWATER D. & WINDLEY B.F. 1973 - Anorthosites, post-orogenic granites, acid volcanic rocks, and crustal development in the North Atlantic Shield during the mid-Proterozoic. Geol. Soc. South Africa Spec. Public., 3: 307-317.
  • BROWN M. 1994 - The generation, segregation, ascent and emplacement of granite magma: and migmatite to crustally derived granite connection in thickened orogens. Earth Science Rev., 36: 83-130.
  • ÈEÈYS A. 2004 - Tectonic implications if the ca. 1.4 Ga granitoid magmatism at the southwestern margin of the East European Craton. Litholund theses No. 5; Lund University: 115.
  • CLAESSON S., BOGDANOVA S.V., BIBIKOVA E.V. & GORBATSCHEV R. 2001-Isotopic evidence for Palaeorpoterozoic accretion in the basement of the east European craton. Tectonophysics, 339: 1-18.
  • CYMERMAN Z. 1997 - Structure, kinematics and an evolution of the Orlica-Śnieżnik Dome, Sudetes. Pr. Państw. Inst. Geol., 156: 1-120.
  • CYMERMAN Z. 2004a-Prekambr platformy wschodnioeuropejskiej na obszarze Polski: tektonika i rozwój skorupy. Pr. Państw. Inst. Geol., 180: 1129.
  • CYMERMAN Z. 2004b - Prekambryjskie struktury Bornholmu i ich odniesienia do regionu Kaszub. Prz. Geol., 52: 593-602.
  • CYMERMAN Z. 2004c - Strefy ścinań a mineralizacje suwalskiego masywu anortozytowego. CAG PIG.
  • CYMERMAN Z. 2006-Interpretacja geologiczna wyników głębokich sondowań sejsmicznych eksperymentu POLONAISE'97 dla polskiej części kratonu wschodnioeuropejskiego. Pr. Państw. Inst. Geol., 188: 167-202.
  • CYMERMAN Z. 2007 - Czy magmatyzm w mezoproterozoiku był anorogeniczny na Mazurach?. Prz. Geol. (w druku).
  • CZUBAW., GRAD M., LUOSTO U., MOTUZA G., NASEDKIN V. & POLONAISE P5 Working Group 2002 - Upper crustal seismic structure of the Mazury Complex and Mazowsze Massif within East European Craton in NE Poland. Tectonophysics, 360: 115-128.
  • DÖRR W., BELKA Z., MARHEINE D., SCHASTOK J., VALVERDE- VAQUERO P. & WISZNIEWSKA J. 2002 - U-Pb and Ar-Ar geochronology of anorogenic granite magmatism of the Mazury Complex, NE Poland. Precambrian Res., 119: 101-120.
  • DUCHESNE J.C., VANDER AUWERA J. & WISZNIEWSKA J. 1998 - Geochemical evidence of a crustal derivation of the Suwałki anorthosites (NE Poland). Abstract at EUROBRIDGE workshop, Tallin-Arbavere, June 2-4, 1998.
  • ELMING S.A., MIKHAILOVA N.P. & KRAVCHENKO S.N. 1998 - The consolidation of the East European Craton: a paleomagnetic analysis of Proterozoic rocks from the Ukrainian Shield and tectonic reconstructions versus Fennoscandia. Geophysical J., 20: 71-74.
  • GORBATSCHEV R. & BOGDANOVA S.V. 1993 - Frontiers in the Baltic shield. Prec. Research. 64: 3-21.
  • HANMER S. 2000 - Matrix mosaics, brittle deformation, and elongate porphyroclasts: granulite facies microstructures in the Striding-Athabasca mylonite zone, western Canada. J. Struct. Geol., 22: 947-967.
  • HARWEGH M. & HANDY M.R. 1996 - The evolution of high-temperature mylonitic microfabrics: evidence from simple shearing of a quartz analogue (norcamphor). J. Struct. Geol., 18: 689-710.
  • JUSKOWIAK O. 1971 - Skały plutoniczne północno-wschodniej Polski. Biul. Inst. Geol., 245: 7-172.
  • JUSKOWIAK O. 1973-Skały plutoniczne. [W:] Łaszkiewicz A. (red.), Skały platformy prekambryjskiej w Polsce. cz. 1. Podłoże krystaliczne. Pr. Inst. Geol., 68: 69-108.
  • JUSKOWIAK O. 1993 - Podłoże krystaliczne Suwalszczyzny. Przew. 64. Zjazdu Pol. Tow. Geol. Państw. Inst. Geol.
  • KRAUSS M., FRANZ K.-M., HAMMER J. & LINDH A. 1996 - Zur Geologie der Smaland-Störungszone (SE-Schweden). Z. geol. Wiss., 24: 273-282.
  • KUBICKI S. & RYKAW. 1982 - Atlas geologiczny podłoża krystalicznego polskiej części platformy wschodnioeuropejskiej. Wyd. Geol.
  • LAFRANCE B., JOHN B.E. & FROST B.R. 1998 - Ultra high-temperatureand subsolidus shear zones: examples from the POE Mountain anorthosite, Wyoming. J. Struct. Geol., 20: 945-955.
  • MORGAN J.W., STEIN H. J., HANNAH J.L., MARKEY R.J. & WISZNIEWSKA J. 2000 - Re-Os study of Fe-Ti-V oxide and Fe-Cu-Ni sulfide deposits, Suwałki Anortosite Massif, Northeast Poland. Miner. Deposita, 35: 391-401.
  • MOTUZA G. 2004 - The geological map of the Precambrian crystalline basement of Lithuania. Lietuvous geologijos taryba.
  • PUURA V. & HUHMA H. 1993 - Paleoproterozoic age of the East Baltic granulitic crust. Precambrian Res., 64: 289-294.
  • ROMER R.L. & NISCA D.H. 1995 - Svecofennian crustal deformation of the Baltic Shield and U-Pb age of late-kinematic tonalitic intrusions in the Burträsk Shear Zone, northern Sweden. Precambrian Res., 75: 17-29.
  • RYKAW. 1973 - Struktury metamorficzne. [W:] A. Łaszkiewicz (red.), Skały platformy prekambryjskiej w Polsce; częśæ 1 - podłoże krystaliczne. Pr. Inst. Geol., 68: 19-59.
  • RYKAW. 1982 - Precambrian evolution of the Polish part of the East European Platform. Geol. Quart., 26: 257-272.
  • SKRIDLAITE G. & MOTUZA G. 2001-Precambrian domains in Lithuania: evidence of terrane tectonics. Tectonophysics, 339: 113-133.
  • SKRIDLAITE G., WISZNIEWSKA J. & DUCHESNE J.-C. 2003-Ferro- potassic A-type granites and related rocks in NE Poland and S Lithuania: west of the East European Craton. Precambrian Res., 124: 305-326.
  • STEIN H.J., MORGAN J.W., MARKEY R.J. & WISZNIEWSKA J. 1998 - A Re-Os study of the Suwałki anorthosite massif, northeast Poland. Geophys. J., 20: 111-114.
  • STEPHENS M.B., WAHLGREN C.-H., WEIJERMARS R. & CRUDEN A.R. 1996 - Left-lateral transpressive deformation and ist tectonic implications, Sveconorwegian orogen, Baltic Shield, southwestern sweden. Precambrian Res., 79: 261-279.
  • ZRODA P. & POLONAISE P3 Working Group 1999 - P- and S-wave velocity model of the southwestern margin of the Precambrian East European Craton; POLONAISE'97, profile P3. Tectonophysics, 314: 175-192.
  • WINDLEY B.F. 1993 - Proterozoic anorogenic magmatism and ist orogenic connections. J. Geol. Soc. London., 150: 39-50.
  • WISZNIEWSKA J. & BAGIŃSKI B. 2001 - Geochronology of anorogenic magmatism in the Mazury Complex. Min. Soc. Poland - Sp. Papers, 19: 20-22.
  • WISZNIEWSKA J. & KRZEMIŃSKA E. 2005 - Precambrian crystalline basement of northeastern Poland - new approach. Min. Soc. Poland - Sp. Papers, 26: 96-103.
  • WISZNIEWSKA J. 2002 - Wiek i geneza rud Fe-Ti-V i skał towarzyszących w suwalskim masywie anortozytowym (NE Polska). Biul. Państw. Inst. Geol., 401: 1-96.
  • WISZNIEWSKA J., CLAESSON S., STEIN H., VANDER AUWERA J. & DUCHESNE J.C. 2002 - The north-eastern Polish anorthosite massifs: petrological, geochemical and isotopic evidence for a crustal derivation. Terra Nova, 14: 451-460.
  • WISZNIEWSKA J., DUCHESNE J.C., CLAESSON S., STEIN H. & MORGAN J. 1999 - Geochemical constrains on the origin of the Suwałki anorthosite massif and related Fe-Ti-V ores, NE Poland (abstract). EUG 10. J. Conf. Abstr., 4: 686.
  • WISZNIEWSKA J., DUCHESNE J-C. & DOERR W. 2002-Titanomagnetite and Cu-Co-Ni sulfide mineralization in the Suwałki and Sejny AMCG complexes (NE Poland). 11th Quadrennial IAGOD Symposium and GEOCONGRESS, 22-26 July 2002. Windhśk, Namibia.
  • WISZNIEWSKA J., WYBRANIEC S. & BOGDANOVA S. 2000 - Combined geological and geophysical characteristics of AMCG complexes in NE Poland. The Abstract Volume of the 31 IGC in Rio de Janeiro, 6-17 August 2000.
  • WYBRANIEC S. 1999 - Transformations and visualization of potential field data. Polish Geol. Institute Spec. Papers, 1: 1-88.
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-article-BUS3-0025-0014
JavaScript jest wyłączony w Twojej przeglądarce internetowej. Włącz go, a następnie odśwież stronę, aby móc w pełni z niej korzystać.