کانی ‌شیمی و کانی‌شناسی در پگماتیت مسترون (شمال الیگودرز- استان لرستان)

نوع مقاله : مقاله پژوهشی

نویسندگان

1 گروه زمین‌شناسی، واحد الیگودرز، دانشگاه آزاد اسلامی، الیگودرز، ایران

2 گروه زمین‌شناسی، واحد خرم‌آباد، دانشگاه آزاد اسلامی، خرم‌آباد، ایران

چکیده

منطقه مسترون در شمال‌شرق شهر ازنا و در پهنه سنندج-سیرجان قرار دارد. واحدهای سنگی موجود شامل توالی به نسبت یکنواخت اسلیت و فیلیت همراه با توده نفوذی گرانودیوریتی دربرگیرنده مجموعه پگماتیتی هستند. مهم‌ترین کانی‌ها کوارتز، فلدسپار قلیایی، پلاژیوکلاز، تورمالین و موسکویت هستند. کوارتز با خلوص بالا و بدون عناصر جانبی است. تجزیه به روش ریزپردازش الکترونی نشان‌دهنده حضور فلدسپار از نوع آلبیت و به مقدار کمتر از نوع ارتوز با دمای تبلور کمتر از ºC550 است. این امر می‌تواند ناشی از دگرگونی­های زیر نقطه انجماد ترکیب فلدسپارها طی سرد شدن توده باشد. تورمالین‌های موجود از نوع شورل و قلیایی با کمبود در جایگاه X هستند و حضور فراوان، خودشکلی و نبود منطقه­بندی شیمیایی بیانگر ماگمایی بودن آنهاست. موسکویت‌ها به دو صورت دانه درشت در پگماتیت‌ها و دانه ریز در درزه‌ها و شکاف‌ها حضور دارند که موسکویت‌های دانه درشت به سمت قطب فنژیت کشش ندارند.

کلیدواژه‌ها

عنوان مقاله [English]

Mineral geochemistry and mineralogy of Masteroon pegmatite (North of Aligudarz - Lorestan Province)

نویسندگان [English]

  • Esmaeil Darvishi 1
  • SeyedVahid Shahrokhi 2
1 Department of Geology, Aligudarz Branch, Islamic Azad university, Aligudarz, Iran
2 Department of Geology, Khorramabad Branch, Islamic Azad university, Khorramabad, Iran
چکیده [English]

Masteroon area is located in the northeast of Azna city, in the Sanandaj-Sirjan zone. The rocks units include a relatively uniform sequence of slate and phyllite with a granodiorite intrusive mass that includes pegmatitic complex. The most important minerals include quartz, alkaline feldspar, plagioclase, tourmaline and muscovite. Quartz is high pure and does not have any other elements. EPMA shows the albite-type feldspar with a lesser extent than orthose-type with a less than 550⁰C crystallization temperature. This can be due to the result of below the freezing of the feldspars composition during the cooling of the mass. The available tourmalines are of schorl and alkaline type with a deficiency in the X position, and their numerous and abundant presence, automorphism and absence of chemical zoning, indicate that tourmalines are magmatic. Muscovites are present in two forms: coarse-grained in pegmatites and fine-grained in joints and cracks, and the coarse-grains does not stretch to phengite.

کلیدواژه‌ها [English]

  • pegmatite
  • quartz
  • Feldspar
  • tourmaline
  • muscovite
  • Masteroon
  • Aligudarz
  • Iran

مراجع

  1. [1] Simmons W. B., Webber K. L., "Pegmatite genesis: state of the art", European Journal of Mineralogy 20 (2008) 421-438. [DOI:10.1127/0935-1221/2008/0020-1833]
  2. [1] Simmons W. B., Webber K. L., "Pegmatite genesis: state of the art", European Journal of Mineralogy 20 (2008) 421-438. [DOI:10.1127/0935-1221/2008/0020-1833]
  3. [2] Thomas R., Davidson P., "The missing link between granites and granitic pegmatites", Journal of Geosciences 58 (2013) 183-200. [DOI:10.3190/jgeosci.135]
  4. [2] Thomas R., Davidson P., "The missing link between granites and granitic pegmatites", Journal of Geosciences 58 (2013) 183-200. [DOI:10.3190/jgeosci.135]
  5. [3] Thomas R., Davidson, "Water in granite and pegmatite-forming melts", Ore Geology Reviews 46 (2012) 32-46. [DOI:10.1016/j.oregeorev.2012.02.006]
  6. [3] Thomas R., Davidson, "Water in granite and pegmatite-forming melts", Ore Geology Reviews 46 (2012) 32-46. [DOI:10.1016/j.oregeorev.2012.02.006]
  7. [4] London D., "Estimating abundances of volatile and other mobile components in evolved silicic melts through mineral melt equilibria", Journal of Petrology 38 (1997) 1691-1706. [DOI:10.1093/petroj/38.12.1691]
  8. [4] London D., "Estimating abundances of volatile and other mobile components in evolved silicic melts through mineral melt equilibria", Journal of Petrology 38 (1997) 1691-1706. [DOI:10.1093/petroj/38.12.1691]
  9. [5] London D., "Reading Pegmatites: what minerals say. Rubellite Press, New Orleans, LA", Contributions to the 6th International Symposium on Granitic Pegmatites (2013) 5-6.
  10. [5] London D., "Reading Pegmatites: what minerals say. Rubellite Press, New Orleans, LA", Contributions to the 6th International Symposium on Granitic Pegmatites (2013) 5-6.
  11. [6] Cerný P., London D., Novák M., "Granitic pegmatites as reflections of their sources", Elements 8 (2012) 289-294. [DOI:10.2113/gselements.8.4.289]
  12. [6] Cerný P., London D., Novák M., "Granitic pegmatites as reflections of their sources", Elements 8 (2012) 289-294. [DOI:10.2113/gselements.8.4.289]
  13. [7] Samadi R., Mirnejad H., Kawabata H., Valizadeh M. V., Harris C., Gazel E., "Magmatic garnet in the Triassic (215 Ma) Dehnow pluton of NE Iran and its petrogenetic significance", International Geology Review 56 (2014) 596-621. [DOI:10.1080/00206814.2014.880659]
  14. [7] Samadi R., Mirnejad H., Kawabata H., Valizadeh M. V., Harris C., Gazel E., "Magmatic garnet in the Triassic (215 Ma) Dehnow pluton of NE Iran and its petrogenetic significance", International Geology Review 56 (2014) 596-621. [DOI:10.1080/00206814.2014.880659]
  15. [8] London D., "A petrologic assessment of internal zonation in granitic pegmatites", Lithos 184-187 (2014) 74-104. [DOI:10.1016/j.lithos.2013.10.025]
  16. [8] London D., "A petrologic assessment of internal zonation in granitic pegmatites", Lithos 184-187 (2014) 74-104. [DOI:10.1016/j.lithos.2013.10.025]
  17. [9] Cerný P., Ercit T. S., "The classification of granitic pegmatites revisited", The Canadian Mineralogist 43 (2005) 2005-2026 [DOI:10.2113/gscanmin.43.6.2005]
  18. [9] Cerný P., Ercit T. S., "The classification of granitic pegmatites revisited", The Canadian Mineralogist 43 (2005) 2005-2026 [DOI:10.2113/gscanmin.43.6.2005]
  19. [10] London D., "Granitic pegmatites: an assessment of current concepts and directions for the future", Lithos 80 (2005) 281-303. [DOI:10.1016/j.lithos.2004.02.009]
  20. [10] London D., "Granitic pegmatites: an assessment of current concepts and directions for the future", Lithos 80 (2005) 281-303. [DOI:10.1016/j.lithos.2004.02.009]
  21. [11] London D., "Pegmatites", The Canadian Mineralogist, Special Publication 10 (2008) 347 p.
  22. [11] London D., "Pegmatites", The Canadian Mineralogist, Special Publication 10 (2008) 347 p.
  23. [12] Stocklin j., "Structual history and tectonic of Iran, a review", American Association of Petroleum Geologist Bulletin 52-7 (1968) 1229-1258. [DOI:10.1306/5D25C4A5-16C1-11D7-8645000102C1865D]
  24. [12] Stocklin j., "Structual history and tectonic of Iran, a review", American Association of Petroleum Geologist Bulletin 52-7 (1968) 1229-1258. [DOI:10.1306/5D25C4A5-16C1-11D7-8645000102C1865D]
  25. [13] Mohajjel M., Sahandi M.R., "Tectonic evolution of Sanandaj-Sirjan Zone", Scientific Quarterly journal Geosience 31-32 (2001) 28-49.
  26. [13] Mohajjel M., Sahandi M.R., "Tectonic evolution of Sanandaj-Sirjan Zone", Scientific Quarterly journal Geosience 31-32 (2001) 28-49.
  27. [14] Shahrokhi S.V., "Ore-control Determinations of Cu-Mineralization and Its Related) Elements at Kondor Area on Part of Aligudarz(NE-Lorestan Province"(, M.Sc. Thesis, North Tehran Branch, Islamic Azad University, Tehran, Iran (2002)155pp.
  28. [14] Shahrokhi S.V., "Ore-control Determinations of Cu-Mineralization and Its Related) Elements at Kondor Area on Part of Aligudarz(NE-Lorestan Province"(, M.Sc. Thesis, North Tehran Branch, Islamic Azad University, Tehran, Iran (2002)155pp.
  29. [15] Lotfi M., Shahrokhi S.V., "Cu-Au ore mineralization in Kondor area (N-Aligoudarz) connecting with relavant geodynamic problems of Masterrun granitoids (NE-lorestan province in Iran)", 7th conference of geological survey of Iran, Isfahan, Iran-Mining, D.A.C., (2004).
  30. [15] Lotfi M., Shahrokhi S.V., "Cu-Au ore mineralization in Kondor area (N-Aligoudarz) connecting with relavant geodynamic problems of Masterrun granitoids (NE-lorestan province in Iran)", 7th conference of geological survey of Iran, Isfahan, Iran-Mining, D.A.C., (2004).
  31. [16] Esna-Ashari A., Hassanzadeh J., Valizadeh M.V., "Geochemistry of microgranular enclaves in Aligoodarz Jurassic arc pluton, western Iran: implications for enclave generation by rapid crystallization of cogenetic granitoid magma" Mineralogy and Petrology 101(2011) 195-216. [DOI:10.1007/s00710-011-0149-7]
  32. [16] Esna-Ashari A., Hassanzadeh J., Valizadeh M.V., "Geochemistry of microgranular enclaves in Aligoodarz Jurassic arc pluton, western Iran: implications for enclave generation by rapid crystallization of cogenetic granitoid magma" Mineralogy and Petrology 101(2011) 195-216. [DOI:10.1007/s00710-011-0149-7]
  33. [17] Esna-Ashari A., Tiepolo M., Valizadeh M.V., Hassanzadeh J., Sepahi A. A., "Geochemistry and zircon U-Pb geochronology of Aligoodarzgranitoid complex, Sanandaj-Sirjan Zone, Iran", Journal of Asian Earth Sciences 43 (2012) 11-12. [DOI:10.1016/j.jseaes.2011.09.001]
  34. [17] Esna-Ashari A., Tiepolo M., Valizadeh M.V., Hassanzadeh J., Sepahi A. A., "Geochemistry and zircon U-Pb geochronology of Aligoodarzgranitoid complex, Sanandaj-Sirjan Zone, Iran", Journal of Asian Earth Sciences 43 (2012) 11-12. [DOI:10.1016/j.jseaes.2011.09.001]
  35. [18] Esna-Ashari A., Tiepolo M., Hassanzadeh J., "On the occurrence and implications of Jurassic primary continental boninite-like melts in the Zagros orogeny", Lithos 258-259 (2016) 37-57. [DOI:10.1016/j.lithos.2016.04.017]
  36. [18] Esna-Ashari A., Tiepolo M., Hassanzadeh J., "On the occurrence and implications of Jurassic primary continental boninite-like melts in the Zagros orogeny", Lithos 258-259 (2016) 37-57. [DOI:10.1016/j.lithos.2016.04.017]
  37. [19] Shahrokhi S.V., "Genetic of Kondor copper and gold mineralization in Aligudarz area, Lorestan, Iran", 6th European congress on regional geoscientific cartography and information system, Bologna, Italy (2009)
  38. [19] Shahrokhi S.V., "Genetic of Kondor copper and gold mineralization in Aligudarz area, Lorestan, Iran", 6th European congress on regional geoscientific cartography and information system, Bologna, Italy (2009)
  39. [20] Ahmadi-Khalaji A., "Petrology of granitoid rocks of the Boroujerd area", Ph.D. Thesis, Tehran Univesity, Tehran, Iran. (2006) 190pp.
  40. [20] Ahmadi-Khalaji A., "Petrology of granitoid rocks of the Boroujerd area", Ph.D. Thesis, Tehran Univesity, Tehran, Iran. (2006) 190pp.
  41. [21] Ahmadi-Khalaji A., Esmaeily D., Valizadeh M.V., Rahimpour-Bonab H., "Petrology and Geochemistry of the Granitoid Complex of Boroujerd, Sanandaj-Sirjan Zone, Western Iran", Journal of Asian earth Sciences 29 (2007) 859-877. [DOI:10.1016/j.jseaes.2006.06.005]
  42. [21] Ahmadi-Khalaji A., Esmaeily D., Valizadeh M.V., Rahimpour-Bonab H., "Petrology and Geochemistry of the Granitoid Complex of Boroujerd, Sanandaj-Sirjan Zone, Western Iran", Journal of Asian earth Sciences 29 (2007) 859-877. [DOI:10.1016/j.jseaes.2006.06.005]
  43. [22] Masoudi F., "Contact metamorphism and pegmatite development in the region SW of Arak, Iran", Ph.D. Thesis, Leeds University, UK (1997) 135p.
  44. [22] Masoudi F., "Contact metamorphism and pegmatite development in the region SW of Arak, Iran", Ph.D. Thesis, Leeds University, UK (1997) 135p.
  45. [23] Masoudi F., Yardley B.W.D., Cliff R.A., "Rb-Sr geochronology of pegmatites, plutonic rocks and a hornfels in the region southwest of Arak, Iran. Islamic Republic of Iran", Journal of Sciences 13-3 (2002) 249-254.
  46. [23] Masoudi F., Yardley B.W.D., Cliff R.A., "Rb-Sr geochronology of pegmatites, plutonic rocks and a hornfels in the region southwest of Arak, Iran. Islamic Republic of Iran", Journal of Sciences 13-3 (2002) 249-254.
  47. [24] Sepahi Garoo A.A., Salami S., Tabrizi M., "Geochemistry of tourmalines in aplitic and pegmatitic dikes from Alvand plutonic and metamorphic rocks of the Hamedan area", Iranian Journal of Crystallography and Mineralogy 22-3 (2014) 495-506.
  48. [24] Sepahi Garoo A.A., Salami S., Tabrizi M., "Geochemistry of tourmalines in aplitic and pegmatitic dikes from Alvand plutonic and metamorphic rocks of the Hamedan area", Iranian Journal of Crystallography and Mineralogy 22-3 (2014) 495-506.
  49. [25] Darvishi E., "Petrography, Geochemistry and Petrogenesis of North Azna Granite mass (Marziyan-Kolbor), Sanandaj-Sirjan Zone", Ph.D Thesis, Isfahan University (2015) 185 P.
  50. [25] Darvishi E., "Petrography, Geochemistry and Petrogenesis of North Azna Granite mass (Marziyan-Kolbor), Sanandaj-Sirjan Zone", Ph.D Thesis, Isfahan University (2015) 185 P.
  51. [26] Darvishi E., "The investigation of mineral chemistry of garnet and tourmaline in Marziyan leucogranite (North Azna, Sanandaj-Sirjan Zone)", Advanced Applied Geology 11-1 (2021) 12-28.
  52. [26] Darvishi E., "The investigation of mineral chemistry of garnet and tourmaline in Marziyan leucogranite (North Azna, Sanandaj-Sirjan Zone)", Advanced Applied Geology 11-1 (2021) 12-28.
  53. [27] Shahrokhi S.V., Delfani H., "Geochemistry and source determination of tourmalines in Mollataleb Area (North of Aligoudarz- Iran)", Iranian Journal of Crystallography and Mineralogy 27-2 (2019) 385-400. [DOI:10.29252/ijcm.27.2.385]
  54. [27] Shahrokhi S.V., Delfani H., "Geochemistry and source determination of tourmalines in Mollataleb Area (North of Aligoudarz- Iran)", Iranian Journal of Crystallography and Mineralogy 27-2 (2019) 385-400. [DOI:10.29252/ijcm.27.2.385]
  55. [28] Bloodate E.S., Hughes G.M., Dyar M.D., Grew E.S., Guidotti C., "Linking structure and chemistry in the schorl-dravite series", American Mineralogist, 84 (1999) 922-928. [DOI:10.2138/am-1999-5-627]
  56. [28] Bloodate E.S., Hughes G.M., Dyar M.D., Grew E.S., Guidotti C., "Linking structure and chemistry in the schorl-dravite series", American Mineralogist, 84 (1999) 922-928. [DOI:10.2138/am-1999-5-627]
  57. [29] Dutrow B.L., Henry D.J., "Tourmaline: a geologic DVD", Elements 7-5 (2011) 301-306. [DOI:10.2113/gselements.7.5.301]
  58. [29] Dutrow B.L., Henry D.J., "Tourmaline: a geologic DVD", Elements 7-5 (2011) 301-306. [DOI:10.2113/gselements.7.5.301]
  59. [30] Didier J., Barbarin B., "Enclaves and granite petrology", Elsevier (1991) 601 p.
  60. [30] Didier J., Barbarin B., "Enclaves and granite petrology", Elsevier (1991) 601 p.
  61. [31] Siivola J., Schmid R., "List of mineral abbreviation Recommendations by the IUGS Subcommission on the Systematics of Metamorphic Rocks", American Mineralogist, Web version 01.02.07 (2017).
  62. [31] Siivola J., Schmid R., "List of mineral abbreviation Recommendations by the IUGS Subcommission on the Systematics of Metamorphic Rocks", American Mineralogist, Web version 01.02.07 (2017).
  63. [32] Deer W.A., Howie R.A., Zuss man J., "An Introduction to the Rock forming Minerals", London (Longman) (1992) 696 p.
  64. [32] Deer W.A., Howie R.A., Zuss man J., "An Introduction to the Rock forming Minerals", London (Longman) (1992) 696 p.
  65. [33] Deer W.A., Howie R.A., Zussman J., "An introduction to the rock- forming minerals", 17th, Longman, Ltd (1991) p.528.
  66. [33] Deer W.A., Howie R.A., Zussman J., "An introduction to the rock- forming minerals", 17th, Longman, Ltd (1991) p.528.
  67. [34] Koroll H., Evangelakakkis C., Voll G., "Two feldspar Geothermometry: a review and revision for slowly cooled rocks", Contributions to Mineralogy and Petrology 3 (1993) 510-518. [DOI:10.1007/BF00321755]
  68. [34] Koroll H., Evangelakakkis C., Voll G., "Two feldspar Geothermometry: a review and revision for slowly cooled rocks", Contributions to Mineralogy and Petrology 3 (1993) 510-518. [DOI:10.1007/BF00321755]
  69. [35] Anderson J. L., "Statuse of thermo-barometry in granitic batholiths", Earth Science Review 87 (1993)125- 138. [DOI:10.1017/S0263593300006544]
  70. [35] Anderson J. L., "Statuse of thermo-barometry in granitic batholiths", Earth Science Review 87 (1993)125- 138. [DOI:10.1017/S0263593300006544]
  71. [36] Hawthorne F.c., Henry D.J., "Classification of the minerals of the tourmaline group", European Journal of Mineralogy 11 (1999), 201-215. [DOI:10.1127/ejm/11/2/0201]
  72. [36] Hawthorne F.c., Henry D.J., "Classification of the minerals of the tourmaline group", European Journal of Mineralogy 11 (1999), 201-215. [DOI:10.1127/ejm/11/2/0201]
  73. [37] Trumbull R.B., Chaussidon M., "Chemical and boron isotopic composition of magmatic and hydrothermal tourmalines from the Sinceni granite-pegmatite system in Swaziland", Chemical Geology 153(1999)125-137. [DOI:10.1016/S0009-2541(98)00155-7]
  74. [37] Trumbull R.B., Chaussidon M., "Chemical and boron isotopic composition of magmatic and hydrothermal tourmalines from the Sinceni granite-pegmatite system in Swaziland", Chemical Geology 153(1999)125-137. [DOI:10.1016/S0009-2541(98)00155-7]
  75. [38] Manning D.A.C., "Chemical and morphological variation in tourmalines from the Hub Kapong batholith of peninsular Thailand", Mineralogical Magazine 45 (1982) 139- 147. [DOI:10.1180/minmag.1982.045.337.16]
  76. [38] Manning D.A.C., "Chemical and morphological variation in tourmalines from the Hub Kapong batholith of peninsular Thailand", Mineralogical Magazine 45 (1982) 139- 147. [DOI:10.1180/minmag.1982.045.337.16]
  77. [39] London D., Manning D., "Chemical variation and significance of tourmaline from Southwest England", Economic Geology 90 (1995), 495-519. [DOI:10.2113/gsecongeo.90.3.495]
  78. [39] London D., Manning D., "Chemical variation and significance of tourmaline from Southwest England", Economic Geology 90 (1995), 495-519. [DOI:10.2113/gsecongeo.90.3.495]
  79. [40] Cavarretta G., puxeddu M., "Schorl-dravite-ferridravite tourmalines deposited by hydrothermal magmatic fluids during early evolution of the Larderelli geothermal field, Italy", Economic Geology 85-6 (1990) 1236-1251. [DOI:10.2113/gsecongeo.85.6.1236]
  80. [40] Cavarretta G., puxeddu M., "Schorl-dravite-ferridravite tourmalines deposited by hydrothermal magmatic fluids during early evolution of the Larderelli geothermal field, Italy", Economic Geology 85-6 (1990) 1236-1251. [DOI:10.2113/gsecongeo.85.6.1236]
  81. [41] Henry D.J., Dutrow B.L. "Metamorphic tourmaline and its petrologic applications", reviews in Mineralogy 33 (1996) 503-557. [DOI:10.1515/9781501509223-012]
  82. [41] Henry D.J., Dutrow B.L. "Metamorphic tourmaline and its petrologic applications", reviews in Mineralogy 33 (1996) 503-557. [DOI:10.1515/9781501509223-012]
  83. [42] Harraz H.Z., El-Sharkaway M.F., "Origin of tourmaline in the metamorphosed Sikait pelitic belt, south eastern desert, Egypt", Journal of African Earth Science 33 (2001) 391-416. [DOI:10.1016/S0899-5362(01)80071-3]
  84. [42] Harraz H.Z., El-Sharkaway M.F., "Origin of tourmaline in the metamorphosed Sikait pelitic belt, south eastern desert, Egypt", Journal of African Earth Science 33 (2001) 391-416. [DOI:10.1016/S0899-5362(01)80071-3]
  85. [43] Henry D.J., Guidotti C.V., Thomson J.A., "The Ti-saturation surface for low-to-medium pressure metapelitic biotites: Implications for geothermometry and Ti-substitution mechanisms", American Mineralogist, 90 (2-3) (2005) 316-328. [DOI:10.2138/am.2005.1498]
  86. [43] Henry D.J., Guidotti C.V., Thomson J.A., "The Ti-saturation surface for low-to-medium pressure metapelitic biotites: Implications for geothermometry and Ti-substitution mechanisms", American Mineralogist, 90 (2-3) (2005) 316-328. [DOI:10.2138/am.2005.1498]
  87. [44] Pirajno F., Smithies R.H., "The FeO/(FeO+MgO) ratio of tourmaline: A useful indicator of spatial variations in granite-related hydrothermal mineral deposits", Journal of Geochemical Exploration 42 (1992) 371-381. [DOI:10.1016/0375-6742(92)90033-5]
  88. [44] Pirajno F., Smithies R.H., "The FeO/(FeO+MgO) ratio of tourmaline: A useful indicator of spatial variations in granite-related hydrothermal mineral deposits", Journal of Geochemical Exploration 42 (1992) 371-381. [DOI:10.1016/0375-6742(92)90033-5]
  89. [45] Feenstra A., "An EMP and TEM-AEM Study of Margarite, Muscovite and Paragonite in Polymetamorphic Metabauxites of Naxos (Cyclades, Greece) and the Implications of Fine-scale Mica Interlayering and Multiple Mica Generations", Journal of Petrology, 37-1 (1996) 201-233. [DOI:10.1093/petrology/37.2.201]
  90. [45] Feenstra A., "An EMP and TEM-AEM Study of Margarite, Muscovite and Paragonite in Polymetamorphic Metabauxites of Naxos (Cyclades, Greece) and the Implications of Fine-scale Mica Interlayering and Multiple Mica Generations", Journal of Petrology, 37-1 (1996) 201-233. [DOI:10.1093/petrology/37.2.201]
مجله بلورشناسی و کانی شناسی ایران
دوره 32، شماره 1 - شماره پیاپی 93
فروردین 1403
صفحه 127-144

فایل ها

سابقه مقاله

  • تاریخ دریافت: 28 خرداد 1402
  • تاریخ بازنگری: 11 مرداد 1402
  • تاریخ پذیرش: 29 شهریور 1402

هم رسانی

ارجاع به این مقاله

آمار