رشد دنباله‌ای همزمان با دگرشکلی طی دگرگونی مجاورتی ناحیه‌ای فشار کم – دمای بالای منطقه قنداب، فریمان، شمال شرقی ایران

نوع مقاله : مقاله پژوهشی

نویسندگان

دانشگاه فردوسی مشهد

چکیده

در این پژوهش، ویژگی های ریزساختاری سنگ­های مجموعه دگرگونی قنداب به عنوان یکی از مهم­ترین دگرگونی­های مجاورتی ناحیه­ای فشار کم - دمای بالای مطالعه شده در ایران بررسی شده است. شواهد بافتی معرف رشد دنباله­ای کانی­ها با افزایش درجه دگرگونی و در طول گسترش چین­خوردگی - برگوارگی است. ترتیب رشد دنباله­ای کانی­ها به صورت کوردیریت، آندالوزیت، گارنت و سیلیمانیت پیشنهاد شده است. برگوارگی اولیه(S1)  عموماً به صورت الگوی میانبارها در شکفته بلورهای کوردیوریت حفظ گردیده است. با این وجود، رشد شکفته­بلورهای آندالوزیت و گارنت همزمان با دگرشکلی و طی کسترش برگوارگی کنگره­ای (S2) صورت گرفته است. بر اساس شواهد بافتی گسترش سیلیمانیت در مراحل نهایی دگرگونی و دگرشکلی صورت گرفته است.     

کلیدواژه‌ها


عنوان مقاله [English]

Sequential syndeformational porphyroblast growth during low-pressure/high temperature contact regional metamorphism in the Ghandab region, NE Iran

نویسندگان [English]

  • Seyed Masoud Homam
  • Fereshteh Ranjbar Moghadam
Ferdowsi University of Mashhad
چکیده [English]

Detailed microstructural analysis has been conducted in the Ghandab metamorphic Complex, which is one of the most important high temperature – low pressure regional contact metamorphism studied areas in Iran. Textural evidence suggests the sequence of growth of minerals with increasing metamorphic grade and during development of a crenulation foliation. The sequence of mineral growth is considered to be cordierite, andalusite, garnet, and sillimanite.  The first foliation (S1) is preserved largely as inclusion trails in cordierite porphyroblasts. However, garnet and andalusite porphyroblasts are syndeformation crystals and grow during development of crenulation-foliation of S2. According to textural evidence, sillimanite produced late in the thermal history of metamorphism and deformation

کلیدواژه‌ها [English]

  • Ghandab metamorphic complex
  • sequential growth
  • foliation
  • deformation
  1. [1] Gibson R.L., "Sequential, syndeformational porphyroblast growth during Hercynian low-pressure/high-temperature metamorphism in the Canigou massif, Pyrenees", Journal of Metamorphic Geology, 10, (1992) 637-650. [DOI:10.1111/j.1525-1314.1992.tb00112.x]
  2. [1] Gibson R.L., "Sequential, syndeformational porphyroblast growth during Hercynian low-pressure/high-temperature metamorphism in the Canigou massif, Pyrenees", Journal of Metamorphic Geology, 10, (1992) 637-650. [DOI:10.1111/j.1525-1314.1992.tb00112.x]
  3. [2] Vernon R. H., "Sequential growth of cordierite and andalusite porphyroblasts, Cooma Complex, Australia: microstructural evidence of a prograde reaction", Journal of Metamorphic Geology, 6, (1992) 255-269. [DOI:10.1111/j.1525-1314.1988.tb00418.x]
  4. [2] Vernon R. H., "Sequential growth of cordierite and andalusite porphyroblasts, Cooma Complex, Australia: microstructural evidence of a prograde reaction", Journal of Metamorphic Geology, 6, (1992) 255-269. [DOI:10.1111/j.1525-1314.1988.tb00418.x]
  5. [3] Pattison D.R.M., Tracy R.J., "Phase equilibria and thermobarometry of metapelites", In Reviews in Mineralogy, 26: Contact metamorphism (ed. D.M. Kerrick), pp. 105-206. Mineralogical Society of America (1991).
  6. [3] Pattison D.R.M., Tracy R.J., "Phase equilibria and thermobarometry of metapelites", In Reviews in Mineralogy, 26: Contact metamorphism (ed. D.M. Kerrick), pp. 105-206. Mineralogical Society of America (1991).
  7. [4] Gramont X. B., Guillon Y., Maurizot P., Vaslet D., Villeon H., "The 1:100000 geological map of Kariz Now", Geological survey of Iran (1979).
  8. [4] Gramont X. B., Guillon Y., Maurizot P., Vaslet D., Villeon H., "The 1:100000 geological map of Kariz Now", Geological survey of Iran (1979).
  9. [5] Vaezipour M., Khalghi M., Alavi-Naeeni M., "Geology of Fariman and a review on metamorphic rocks from north-East of Iran", Geological Survey of Iran (1983).
  10. [5] Vaezipour M., Khalghi M., Alavi-Naeeni M., "Geology of Fariman and a review on metamorphic rocks from north-East of Iran", Geological Survey of Iran (1983).
  11. [6] Safuraee S., "Petrology and geochemistry of metamorphic rocks from south-east of Fariman", Ms.C Thesis, Shahrood University of Technology (2007).
  12. [6] Safuraee S., "Petrology and geochemistry of metamorphic rocks from south-east of Fariman", Ms.C Thesis, Shahrood University of Technology (2007).
  13. [7] Ranjbar Moghadam F., "Petrology and petrogenesis of metamorphic rocks from south-East of Ghandab with special reference to economic potential of andalusite schists, Ms.C Thesis, ferdowsi University of Mashhad (2009) .
  14. [7] Ranjbar Moghadam F., "Petrology and petrogenesis of metamorphic rocks from south-East of Ghandab with special reference to economic potential of andalusite schists, Ms.C Thesis, ferdowsi University of Mashhad (2009) .
  15. [8] Eftekhar-Nejad J., "Some Information about the Origin of the Flysch Basin in Eastern Iran and its Relation to Plate Tectonics Theory", Report No.22. Geological Survey of Iran, (1973).
  16. [8] Eftekhar-Nejad J., "Some Information about the Origin of the Flysch Basin in Eastern Iran and its Relation to Plate Tectonics Theory", Report No.22. Geological Survey of Iran, (1973).
  17. [9] Aghanabati S.A., "Etude geologique de la region de Kalmard (W.Tabas) Iran Central; stratgraphie et tectonique, Thesis, Grenoble, 231p (1975).
  18. [9] Aghanabati S.A., "Etude geologique de la region de Kalmard (W.Tabas) Iran Central; stratgraphie et tectonique, Thesis, Grenoble, 231p (1975).
  19. [10] Alavi M., Vaziri H., Seyed-Emami K., Lasemi Y., "The Triassic and associated rocks of the Nakhlak and Aghdarband areas in central and northeastern Iran as remnants of the southern Turanian active continental margin", GSA Bulletin; v. 109; No. 12; (1997) p. 1563-1575

    https://doi.org/10.1130/0016-7606(1997)1092.3.CO;2 [DOI:10.1130/0016-7606(1997)1092.3.CO;2]
  20. [10] Alavi M., Vaziri H., Seyed-Emami K., Lasemi Y., "The Triassic and associated rocks of the Nakhlak and Aghdarband areas in central and northeastern Iran as remnants of the southern Turanian active continental margin", GSA Bulletin; v. 109; No. 12; (1997) p. 1563-1575

    https://doi.org/10.1130/0016-7606(1997)1092.3.CO;2 [DOI:10.1130/0016-7606(1997)1092.3.CO;2]
  21. [11] Barker A.J., "Introduction to metamorphic textures and microstructures", Stanley Thornes, Oxford, (1998) 264pp. [DOI:10.1007/978-1-4615-7291-6]
  22. [11] Barker A.J., "Introduction to metamorphic textures and microstructures", Stanley Thornes, Oxford, (1998) 264pp. [DOI:10.1007/978-1-4615-7291-6]