The Zadnie Kamienne "ravenous" shear zone (High-Tatric Nappe) - conditions of deformation

• Autorzy: Jurewicz E. , Słaby E.
• Języki publikacji: EN

Abstrakty

EN

The Zadnie Kamienne shear zone is a high-angle Riedel type shear zone (R'), exhibiting an antithetic sense of displacement, which may have developed synchronously with the nappe-thrusting of the Giewont Unit (High-Tatric Nappe). The amount of displacement along this zone is very low and does not explain the very intense deformation, which is of the same character as that at the base of the Giewont Unit (mylonitization, stylolitization and vein forming). The explanation of this phenomenon lies in the multiple activity of this zone, the change of the direction of movement and the important role of pressure solution in hydrothermal conditions responsible for dissolution creep, mass loss and stress relaxation. This kind of shear can be referred to as a "ravenous" shear zone. Neo-forming minerals accompanying these processes were applied as a temperature gauge. Simultaneous growth of albite and adularia indicates a temperature of about 350 degrees C. Chlorites accompanying them occur in two thermal episodes, the first of which indicating a similar temperature (292-357 C).

Słowa kluczowe

EN

Tatra Mts.; Carpathians; shear zone; pressure solution; feldspar growth; geothermometers

• Wydawca: Państwowy Instytut Geologiczny - Państwowy Instytut Badawczy
• Czasopismo: Geological Quarterly
• Rocznik: 2004
• Tom: Vol. 48, No 4
• Strony: 371--382
• Opis fizyczny: Bibliogr. 51 poz., rys., tab.

Twórcy

autor

Jurewicz E.

• Faculty of Geology, Warsaw University, Żwirki i Wigury 93, 02-089 Warsaw, Poland

autor

Słaby E.

• Faculty of Geology, Warsaw University, Żwirki i Wigury 93, 02-089 Warsaw, Poland

Bibliografia

• 1. AHLGREN S. G. (2001) - The nucleation and evolution of Riedel shear zones as deformation bands in porous sandstone. J. Struct. Geol., 23 (8): 1203-1214.
• 2. ANDRUSOV D.(1965) - Aperęu générale sur la géologie des Carpathes occidentales. Bull. Soc. Géol. France, 7: 1029-1062.
• 3. BAC-MOSZASZWILI M., BURCHART J., GŁAZEK J., IWANOW A., JAROSZEWSKI W., KOTAŃSKI Z., LEFELD J., MASTELLA L., OZIMKOWSKI W., RONIEWICZ P., SKUPIŃSKI A. and WESTFALEWICZ-MOGILSKA E. (1979) - Mapa geologiczna Tatr Polskich 1:30 000. Wyd. Geol. PAN, Pol. Tow. Geol.
• 4. BAC-MOSZASZWILI M., GAMKERLIDZE I. P., JAROSZEWSKI W., SCHROEDER E., STOJANOV S. and TZANKOV T. V. (1981) - Thrust zone of the Križna Nappe at Stoły in Tatra Mts (Poland). Stud. Geol. Pol., 68:61-73.
• 5. BAC-MOSZASZWILI M., JAROSZEWSKI W. and PASSENDORFER E. (1984) - On the tectonics of Czerwone Wierchy and Giewont area in the Tatra Mts., Poland (in Polish with English summary). Ann. Soc. Geol. Pol., 52 (1-4): 67-88.
• 6. BRANQUET Y., CHEILLETZ A., GILLIANI G., LAUMONIER B. and BLANCO O. (1999) - Fluidized hydrothermal breccia in dilatant faults during thrusting: the Colombian emerald deposits. In: Fractures, Fluid Flow and Mineralization (eds. K. J. W. McCaffrey, L. Lonergan and J. J. Wilkinson). Geol. Soc. Spec. Publ., 155: 182-195.
• 7. BURCHART J. (1972) - Fission-track age determination of accessory apatite fromthe Tatra Mts, Poland. Earth Plane. Sc. Lett., 15: 418-422.
• 8. BURKHARD M. (1993) - Calcite-twins, their geometry, appearance and significance as stress-strain markers and indicators of tectonic regime: a review. J. Structur. Geol., 15: 351-368.
• 9. CATHELINEAU M. (1988) - Cation site occupancy in chlorites and illites as a function of temperature. Clay Minerals, 23: 471-485.
• 10. DAVIS G. H. and REYNOLDS S. J. (1996) - Structural Geology. John Wiley and Sons, Inc.
• 11. FUHRMANN M. L. and LINDSLEY D. L. (1988) - Ternary-feldspar modelling and thermometry. Am. Miner., 73: 201-215.
• 12. GIGGENBACH W. F. (1984) - Mass transfer in hydrothermal alteration systems. A conceptual approach. Geochim. Cosmochim. Acta, 48: 2693-2711.
• 13. GRATIER J. P., RENARD F. and LABAUME P. (1999) - How pressure solution creep and fracturing process interact in the upper crust to make it behave in both a viscous and brittle manner. J. Structur. Geol., 21 (8-9): 1189-1197.
• 14. GUZIK K. (1959) - Mapa geologiczna Tatr polskich ark. Kominy Tylkowe, 1:10 000. Inst. Geol.
• 15. JANÁK M. (1994) - Variscan uplift of the crystalline basement, Tatra Mts, Central West Carpathians: evidence from 40Ar/39Ar laser probe dating of biotite and P-T-t paths. Geol. Carpath., 45 (5): 239-300.
• 16. JAROSZEWSKI W. (1982) - Hydrotectonic phenomena at the base of the Križna Nappe, Tatra Mts. In: Alpine Structural Elements: Carpathian-Balkan-Caucasus-Pamir Orogene Zone, Veda, Bratislava (ed. M. Mahel’): 137-148.
• 17. JUREWICZ E.(2000) - Tentative reconstructions of the stress axes from the thrust-folding stage in the Tatra Mts. onthe basis of slickensides in the granitoid core, southern Poland (in Polish with English summary). Prz. Geol., 48 (3): 239-246.
• 18. JUREWICZ E. and KOZŁOWSKI A. (2003) - Formation conditions of quartz mineralization in the mylonitic zones and on the slickenside fault planes in the High Tatra granitoids. Archiw. Miner., 54: 65-75.
• 19. JUREWICZ E. (2003) - Multistage evolution of the shear zone at the base of the GiewontUnit, Polish Tatra Mts. Geol. Carpat., 54 (5): 337-351.
• 20. JUREWICZ E. and BAGIŃSKI B. (2005) - Deformationphases inthe selected shear zones within the Tatra Mts granitoid core. Geol. Carpat. (in press).
• 21. KARCZ Z. and SCHOLZ C. H. (2003) - The fractal geometry of some stylolites from the Calcare Massiccio Formation, Italy. J. Structur. Geol., 25 (8): 1301-1316.
• 22. KENNEDY L. A. and LOGAN J.M.(1997) - The role of veining and dissolution in the evolution of fine-grained mylonites: the McConnell thrust, Alberta. J. Structur. Geol., 19 (6): 785-797.
• 23. KOTAŃSKI Z. (1956) - High-Tatric Campillian in the Tatra Mts. (in Polish with English summary). Acta Geol. Pol., 6 (1): 65-73.
• 24. KOTAŃSKI Z.(1959) - Stratigraphical sections of the high-Tatric Series in the Polish Tatra Mts. (in Polish with English summary). Biul. Inst. Geol., 139.
• 25. KOTAŃSKI Z. (1965) - La structure géologique de la chaine subtatrique entre la vallée de Mała Łąka et la vallée Kościeliska dans les Tatras Occidentales (in Polish with French summary). Acta Geol.Pol., 15 (3): 257-320.
• 26. KRAJEWSKI K. (1980) - Zbadań sedymentologicznych utworów kredy wierchowej w Dolinie Kościeliskiej. Prz. Geol., 28 (11): 636-637.
• 27. KRETZ R. (1983) - Symbols for rock-forming minerals. Am. Miner., 68: 277-279.
• 28. KÜSTER M. and STÖCKHERT B. (1999) - High differential stress and sublithostatic pore fluid pressure in the ductile regime - microstructural evidence for short-term post-seismic creep in the Sesia Zone, Western Alps. Tectonophysics, 303 (1-4): 263-277.
• 29. LEFELD J., GAŹDZICKI A., IWANOW A. and KRAJEWSKI K. (1985) - Jurassic and Cretaceous lithostratigraphic units of the Tatra Mts. Stud. Geol. Pol., 84.
• 30. ŁUCZYŃSKI P. (2001) - Pressure-solution and compaction of condensed Middle Jurassic deposits, High Tatric series, Tatra Mts. Geol. Carpat., 52 (2): 91-102.
• 31. MCKINNON S. D. and GARRIDO DE LA BARRA I. (1998) - Fracture initiation, growth and effect on stress field: a numerical investigation. J. Structur. Geol., 20 (12): 1673-1689.
• 32. MILOVSKÝ R., HURAI V., PLAŠIENKA D. and BIROŇ A. (2003) - Hydrotectonic regime at soles of overthrust sheets: textural and fluid inclusion evidence from basal cataclasites of the Muráň nappe (Western Carpathians, Slovakia). Geodinam. Acta, 16: 1-20.
• 33. NEKVASILH. and BURNHAM C. W. (1987) - The calculated individual effects of pressure and water content on phase equilibria in the granite system. In: “Magmatic Processes: Physicochemical Principles (ed. B. O. Mysen). University Park, Pa.: Geochemical Society”.
• 34. NEWMAN J. and MITRA G. (1994) - Fluid influenced deformation and recrystallization of dolomite at low temperatures along a natural fault zone, Mountain City window, Tennessee. Geol. Soc. Am. Bull., 106 (10): 1267-1279.
• 35. NEX P. A., KINNAIRD J. A. and IXER R. A. (2003) - Localized ductile thrusting north of the Variscan Front, Ross Island, southwest Ireland. Geol. J., 38 (1): 15-29.
• 36. PASSCHIER C. W. and TROUW R. A. J. (1998) - Microtectonics. Springer-Verlag.
• 37. PETIT J. P., WIBBERLEY C. A. J. and RUIZ G. (1999) - “Crack-seal”, slip: a new fault valve mechanism? J. Structur. Geol., 21 (8-9): 1199-1207.
• 38. PIOTROWSKI J. (1978) - Mesostructural analysis of the main tectonic units of the Tatra Mts. Along the KościeliskaValley. Stud. Geol. Pol., 55.
• 39. PLAŠIENKA D. and SOTÁK J. (1996) - Rauwackized carbonate tectonic breccias in the West Carpathian nappe edifice: introductory remarks and preliminary results. Slovak Geol. Magaz., 3-4: 287-291.
• 40. RENARD F., GRATIER J. P. and JAMTVEIT B. (2000) - Kinetics of crack-sealing, intergranular pressure solution, and compaction around active faults. J. Structur. Geol., 22 (10): 1395-1407.
• 41. RAJLICH P. (1993) - Riedel shear: a mechanism for crenulation cleavage. Earth Sc. Rev., 34 (3): 167-195.
• 42. SIBSON R. H. (1996) - Structural permeability of fluid-driven fault-fracture meshes. J. Structur. Geol., 18 (8): 1031-1042.
• 43. SŁABYE. (1990) – Adularia from Miękinia (in Polish with English summary). Archiw. Miner., 46 (1-2): 55-69.
• 44. SŁABY E. (1992) - Changes in the structural state of secondary albite during progressive albitization. Neues Jahrb. Miner., Monatsh., H7: 321-335.
• 45. SŁABY E. (2000) - Sodium and potassium feldspars - products of late magmatic alteration. Pr. Spec. Pol. Tow. Miner., 17: 35-38.
• 46. SŁABY E., KOZŁOWSKI A., LENSCH G. and MIHM A. (1993) - Origin of albite-adularia paragenesis - an example of alkali metasomatism through magmatic-meteoric fluid mixing. Miner. Pol., 24 (1-2): 3-19.
• 47. STESKYR. M. (1978) - Mechanisms of high temperature frictional sliding inWesterly granite. Canad. J. Earth Sc., 15: 361-375.
• 48. TEIXELL A., DURNEY D. W. and ARBOLEYA M. L. (2000) - Stress and fluid on décollement within competent limestone. J. Structur. Geol., 22 (3): 349-371.
• 49. VERNON R. H. (1998) - Chemical and volume changes during deformation and prograde metamorphism of sediments. In: What Drives Metamorphism and Metamorphic Reactions? (eds. P. J. Treloar and P. J. O’Brien). Geol. Soc., London. Spec. Public., 138: 215-246.
• 50. WHITE S. H., BURROWS S. E., CARRERAS J., SHAW N. D. and HUMPHREYS F. J. (1980) - On mylonites in ductile shear zones. J. Structur. Geol., 2: 175-187.
• 51. WILCOXR. E.,HARDINGT. P. andSELLYD. R. (1973) - Basicwrench tectonics. Am. Ass. Petrol. Geol. Bull., 57: 74-96.