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Torkian A, Shirmohamadi Z, Kokabi F, Tahmasbi M. Application of mineral chemistry in determination of protolith and thermobarometry of the Sartip Abad metamorphic rocks (Qorveh-Kurdistan Province). www.ijcm.ir 2023; 31 (1) :105-122
URL: http://ijcm.ir/article-1-1725-en.html
URL: http://ijcm.ir/article-1-1725-en.html
1- Bu-Ali Sina University
Abstract: (819 Views)
The Sartip Abad metamorphic complex in Qorveh (Kurdistan Province) is located in the Sanandaj-Sirjan zone. The complex is composed of regional metamorphic rocks including contact metamorphic rocks (hornfels), variety of schists (amphibole schist, actinolite schist, mica schist, and garnet schist), marble, metadiorite, metagabbro, and paragneiss. In schists and paragneiss, biotite is siderophilite and in hornfels and metadiorite is anite to phlogopite in composition, respectively. Paragneiss and metadiorites include hornblende and actinolite. The garnets, in the garnet-mica schist, are almandine type, and plagioclase crystals in the metadiorites and metagabbros are labradorite type in composition, as well as their paragneiss have andesine- type plagioclase. Petrography and thermobarometric studies indicate that the different types of regional metamorphic rocks are formed in green schist to epidote-amphibolite facies and in the interval between biotite and staurolite zones. But for contact metamorphic rocks, the maximum facies is assumed albite-epidote hornfels in isograd of zoisite to amphibole. Thermometry calculations, using biotite single and garnet-biotite exchange, show that the average temperature for the metamorphic rocks of this region is about 567°C and for the contact metamorphic rocks is about 647 °C. Also, we used thermo-barometer methods for M1 and M2 metamorphic stages. Data are yielded, M1 stage temperature and pressure are about 578°C and 5.16 kb and for M2 stage ~565 °C and 4.6 kbar. Based on field relationships, petrographic evidence and geochemical data, protoliths are sedimentary rocks including greywackes/arkoses and shales for paragneiss, hornfels and schists, respectively.
References
1. [1] Aghanabati S.A., "Geology of Iran, Geological survey and mineral exploration of Iran, (In Persian)", (2004) 640P.
2. [2] Berberian M., Alavi-tehrani N., "Structural analyses of Hamadan metamorphic tectonites, A paleotetonic discussion. In: contribution to the seismotectonic of Iran", Geological and Mining Survey of Iran, 40 (1977) 263-278.
3. [3] Mohajjel M., "Structure and tectonic Evolution of Paleozoic-Mesozoic rocks, Sanandaj- Sirjan zone, Western Iran", Ph.D. thesis, The University of Wollongong, New south wales, Australia. (1997) 279p.
4. [4] Mohajjel M., Sahandi R., "Tectonic evolution of Sanandaj-Sirjan zone in the northwestern half and introduction of new sub-zones in it" (In Persian), Geosciences Scientific Quarterly Journal, 32(8) (1999) 21-49.
5. [5] Mahmoudi S., Corfu F., Masoudi F., Mehrabi B., Mohajjel M., "U-Pb dating and emplacement history of granitoid plutons in the northern Sanandaj-Sirjan Zone, Iran", Journal of Asian Earth Sciences, 41(3) (2011) 238-249. [DOI:10.1016/j.jseaes.2011.03.006]
6. [6] Hosseini M., "Geological Qorveh Map 1:100000", No. 5560", Geological Survey of Iran, (1999).
7. [7] Blourchi M.H., "Metamorphic lithological research in the south of Qorveh city", (In Persian), Master Thesis, Tehran University, (1967).
8. [8] Hariri A., A "view on the origin of a group of metamorphic rocks in Qorveh area", (In Persian), Master Thesis, Shahid Beheshti University, (1995) 161P.
9. [9] Omravani H., "Study of metamorphism and deformation of southern Qorveh rocks", (In Persian), Master Thesis, Tabriz University, (2005).
10. [10] Torkian A., Izadyar J., Rezvani-mokaber Z., sepahi A., "Petrography and application of mineral chemistry in thermodynamic studies of metamorphic rocks, Zarineh region, S-Qorveh, Kurdistan (In Persian)", Iranian Journal of Crystallography and Mineralogy, 27(4) (2018) 775-786. [DOI:10.29252/ijcm.25.4.775]
11. [11] Cheraghi S., "Petrology of metamorphic complex from the Asifabad-Tazehabad, South Qorveh, Kordistan Province" (In Persian), Bu-Ali Sina University, Master Thesis, (2019) 100P.
12. [12] Deer W.A., Howie R.A., Zussman J., "An Introduction to the Rock Forming Minerals", Longman, London, (1992) 528p.
13. [13] Coleman R.G., Lee D.E., Beatty L.B., Brannock W.W., "Eclogites and Eclogites: their differences and similarities", Geological Society of America Bulletin, 76 (5) (1965) 483-508. [DOI:10.1130/0016-7606(1965)76[483:EAETDA]2.0.CO;2]
14. [14] Leak B.E., Wolley A.R., Bird W.D., Gilbert M. C., Grice J.D., "Nomenclature of amphiboles: Report of the subcommittee on amphiboles of International mineralogical Association, commission on newminerals and mineral names", American Mineralogy, 82 (1997) 1019-1037.
15. [15] Hawthorne F.C., Oberti R., Harlow G.E., Maresch W.V., Martin R.F., Schumacher J.C., Welch M.D., "IMA report, nomenclature of the amphiboles upper group", American Mineralogist, 97 (2012) 2031-2048. [DOI:10.2138/am.2012.4276]
16. [16] Henry D.J., Guidotti C.V., Thomson J.A., "The Tisaturation surface for low-to-medium pressure metapelitic biotites: implications for geothermometry and Ti substitution mechanisms implications for geothermometry and Ti-substitution mechanisms", American Mineralogist, 90 (2005) 316-328. [DOI:10.2138/am.2005.1498]
17. [17] Henry D.J., Guidotti C.V., "Titanium in biotite from metapelitic rocks: Temperature effects, crystal-chemical controls, and petrologic applications", American Mineralogist, 87 (2002) 375- 382. [DOI:10.2138/am-2002-0401]
18. [18] Winter J., "An introduction to igneous and metamorphic petrology", (2010), No., 552.
19. [19] Kuthe J.R., "The classification of eclogites and how the role of fluids, mineralogy and chemistry helps to determine their processes of formation", Geological hazards and mitigation, (2016).
20. [20] Vielzeuf D., Holloway J.R., "Experimental determination of fluid-ascent melting relations in the pelitic system", Contributions to Mineralogy and Petrology, 98 (1988) 257-276. [DOI:10.1007/BF00375178]
21. [21] Vielzeuf D., Schmidt M.W., "Melting relations in hydrous systems revisited: application to metapelites, metagreywackes and metabasalts", Contributions to Mineralogy and Petrology 141(2001) 251-267. [DOI:10.1007/s004100100237]
22. [22] Holland T.J.B., "Experimental determination of the reaction paragonite: jadeite + kyanite + water, and internally consistent thermodynamic data for part of the system Na2O-Al2O3- SiO2-H2O, with applications to eclogites and blueschists", Contributions to Mineralogy and Petrology, 68 (1979) 293-301. [DOI:10.1007/BF00371551]
23. [23] Ferry J. M., Spear F. S., "Experimental calibration of the partitioning of Fe and Mg between biotite and garnet", Contributions to Mineralogy and Petrology, 66 (1978) 113-117. [DOI:10.1007/BF00372150]
24. [24] Thompson A.B., "Mineral reactions in pelitic rocks: I Predication P-T-X (Fe-Mg) phase relations", American Journal of Science, (1976). [DOI:10.2475/ajs.276.4.401]
25. [25] Schmidt M.W., "Amphibole composition in tonalite as a function of pressure: an experimental calibration of the Al-in hornblende barometer", Contribution to Mineralogy and Petrology, 110 (1992) 304-310. [DOI:10.1007/BF00310745]
26. [26] Graham C.M., Powell R., "A garnet-hornblende geothermometer: calibration, testing, and application to the Pelona Schist, Southern California", Journal of Metamorphic Geology, 3 (1984) 13-31. [DOI:10.1111/j.1525-1314.1984.tb00282.x]
27. [27] Spear F.S., Rumble D., "Pressure, temperature and structural evolution of the Orfordville Belt, west-central New Hampshire", Journal of Petrology, 27 (1986) 1071-1093. [DOI:10.1093/petrology/27.5.1071]
28. [28] Hodges K.V., Crowley P.D., "Error estimation in empirical geothermometry and geobarometry for pelitic systems", American Mineralogist, 70 (7-8) (1985) 702-709.
29. [29] Ellis D.J., Green D.H., "An experimental study of the effect of Ca upon garnet-clinopyroxene Fe-Mg exchange equilibria", Contributions to Mineralogy and Petrology, 71 (1979) 13-22. [DOI:10.1007/BF00371878]
30. [30] Bohlen S.R., Wall V.J., Boettcher A.L., "Experimental investigation and application of garnet granulite equilibria", Contrib. Mineral. Petrol., 83 (1983) 52-61. [DOI:10.1007/BF00373079]
31. [31] Newton R.C., Perkins D., "Thermodynamic calibration of geobarometers based on the assemblages garnet-plagioclase-orthopyroxene (clinopyroxene)-quartz", American Mineralogist, 67 (3-4) (1982) 203-222.
32. [32] Goldman D.S.Y., Albee A.L., "Correlation of Mg/Fe partitioning between garnet and biotite with 18O/16 O partitioning between quartz and magnetite", American Journal of Science, 277 (1977) 750-767. [DOI:10.2475/ajs.277.6.750]
33. [33] Holdaway M., Lee, S.N., "Fe-Mg cordierite stability in high-grade pelitic rocks based on experimental, theoretical and natural observations", Contributions to Mineralogy and Petrology, 63 (1977) 175-98. [DOI:10.1007/BF00398778]
34. [34] Lavrenteva E.V., Perchuck L.L., "Cordierite-garnet thermometer, A collection of these", The Academy of Sciences of the USSR, 259 (1981) 607-700.
35. [35] Hodges K.V.Y., Spear F.S., "Geothermometry, geobarometry and the Al2SiO 5 triple point at Mt, Moosilauke, New Hampshire", American Mineralogis, 67(1982) 1118-1134.
36. [36] Pigage L.C., Greenwood H.J., "Internally consistent estimates of pressure and temperature: the staurolite problem", American Journal of Science, 282(7) (1982) 943 - 969. [DOI:10.2475/ajs.282.7.943]
37. [37] Perchuk L.L., Lavrenteva I.V., "Experimental investigation of exchange equilibria in the system cordierite-garnet-biotite", In: Saxena, S.K. (Eds.) Kinetics and Equilibrium in Mineral Reactions, Advances in Physical Geochemistry, Springer, New York, 3 (1983) 199-239. [DOI:10.1007/978-1-4612-5587-1_7]
38. [38] Ganguly J., Saxena S.K., "Mixing properties of aluminosilicate garnets: constrains for natural and experimental data and application to geothermobarometry", American Mineralogist, 69 (1984) 88-97.
39. [39] Perchuk L.L., Aranovich L.Ya., Podlesskii K.K., Lavrenteva I.V., "Precambrian granulites of the Alden Shield, eastern Siberia USSR", Journal Metamorphic Geology, 3 (1985) 265-310. [DOI:10.1111/j.1525-1314.1985.tb00321.x]
40. [40] Indares A.Y., Martignole J., "Biotite-garnet geothermometry in granulite facies: the influence of Ti and Al in biotite", American Mineralogist, 70 (1985) 272-278.
41. [41] Williams M.L., Grambling J.A., "Manganese, ferric iron, and the equilibrium between garnet and biotite", American Mineralogist, 75 (1990) 886-908.
42. [42] Dasgupta S., Sengupta P., Guha, D., Fukuoka M., "A refined garnet-biotite Fe-Mg exchange geothermometer and its application in amphibolites and granulites", Contributions to Mineralogy and Petrology, 109 (1991) 130-137. [DOI:10.1007/BF00687206]
43. [43] Bhattacharya A., Mohanty L., Maji A., Sen S.K., Raith M., "Non-ideal mixing in the phlogopite annite binary: constraints from experimental data on Mg-Fe partitioning and a reformulation of the biotite-garnet geothermometer", Contributions to Mineralogy and Petrology, 111 (1992) 87-93. [DOI:10.1007/BF00296580]
44. [44] Yardley B.W.D., "An Introduction to Metamorphic Petrology", Longman, (1991) 248p.
45. [45] Kretz R., "Metamorphic crystallization", John Wiley and Sons, (1994) 507p.
46. [46] Spear F.S., "Metamorphic phase equilibria and pressure-temperature-time paths", Mineralogical Society of America Monograph, (1993) 799p.
47. [47] Winkler H.G.F., "Petrogenesis of metamorphic rock" (4thed.), Springer- Verlag, New York Inc., (1976) 334p. [DOI:10.1007/978-1-4615-9633-2]
48. [48] Thompson J.B., Norton S.A., "Paleozoic regional metamorphism in New England and adjacent areas", In: Zen et al. (Eds.) Studies in Appalachian geology- Northern and Maritime, New York, Interscience, (1968) 319-327.
49. [49] Miyashiro A., "Metamorphism and Metamorphic belts", George Allen and Unwin, London, (1973) 492p. [DOI:10.1007/978-94-011-6836-6]
50. [50] Hsu K.J., "The principles of melanges and their bearing on the Franciscan-Knoxville paradox. Bull", Geological Society of America, 79 (1968) 1063-1074. [DOI:10.1130/0016-7606(1968)79[1063:POMATB]2.0.CO;2]
51. [51] Hirschberg A., Winkler H.G.F., "Stabilitats beziehungen Zwischen Chlorit, Cordierit und Almandin bei der metamorphose", Contributions to Mineralogy and Petrology, 18 (1968) 17-92. [DOI:10.1007/BF00371984]
52. [52] Spear F.S., "Petrologic determination of metamorphic pressure-temperature-time paths", Metamorphic pressure‐temperature‐time paths. (1989), 7:1-55. [DOI:10.1029/SC007p0001]
53. [53] De La Roche H., "Sur l' existence de plusiers facies geochimiques dans les schistes palezoiques des Pyrenees Luchonnaises", Geologische Rundschau, (1966), 55(2): 274-301. [DOI:10.1007/BF01765767]
54. [54] Herron M.M., "Geochemical classification of terrigenous sands and shales from core or log data", Journal of Sedimentary Petrology 58 (1988) 820-829. [DOI:10.1306/212F8E77-2B24-11D7-8648000102C1865D]
55. [55] Mackenzie, F.T. and Garrels, R.M., "Evolution of sedimentary rocks", New York: Norton (1971).
56. [56] Mason B., Moore C.B., "Principle of geochemistry", John Wiley and Sons, (1982) 344p.
57. [57] Barker A.J., "Introduction to metamorphic textures and microstructures", Routledge, (2013). [DOI:10.4324/9781315831626]
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