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  • Study of micro-textures and chemistry of feldspar minerals of East Sarbisheh volcanic complex (Eastern Iran), for evidence of magma chamber process

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عنوان URL للمقالة


رقم المقالة : IJES-1904-1319 (R4) زيارة : 227 الصفحة: 10 - 31

10.30495/ijes.2020.671654

نوع المخطوط: ابحاث

Study of micro-textures and chemistry of feldspar minerals of East Sarbisheh volcanic complex (Eastern Iran), for evidence of magma chamber process

الموضوعات :

Mahboobeh Jamshidibadr 1 , Sahar Tarabi 2 , Kazem Qolizadeh 3

1 - Geology Department, Payame Noor University, 19395-4697 Tehran, Iran
2 - Young Researchers and Elites club, Science and Research Branch, Islamic Azad University, Tehran, Iran
3 - Iran minerals processing research center (IMPRC), Karaj, Iran

تاريخ الإرسال : 10 الإثنين , شعبان, 1440 تاريخ التأكيد : 21 الخميس , ذو الحجة, 1440 تاريخ الإصدار : 06 الأربعاء , جمادى الأولى, 1441

الکلمات المفتاحية: micro-textures, Sarbisheh Volcanic Complex, Magma, Lut-Sistan Zone, Plagioclase,

ملخص المقالة :

The Eocene-Oligocene Sarbisheh volcanic complex is a part of the Lut-Sistan Zone that outcrops in eastern Iran. In the east of this complex, three groups of volcanic rocks (i.e., andesite, dacite, and rhyolite) exist. Plagioclase as the main mineral of these rocks is found with varying micro-textures. Based on a changing trend in the concentration of anorthite, the developed micro-textures (coarse/fine-sieve, fine-scale oscillatory zoning, and resorption surfaces) are not affected by the chemical composition of the magma. Rather, such changes can occur by temperature variations during magma crystallization or H2O fugacity changes in the magmatic system. The recharge of basic magma leads to a temperature rise, partial melting of the central part of the crystal, and formation of sieve texture, and resorption surfaces. Consequently, the chemical changes of magma in the chamber cause the formation of An-enrichment in the outer layer of the plagioclase crystal and formation of oscillatory zoning. In addition, the morphological micro-textures (i.e., glomerocryst, synneusis, swallow-tailed, microlite, and broken crystals) are developed by the influence of dynamic behavior of the crystallizing magma and magmatic differentiation. The thermobarometry evaluation using pyroxene and biotite chemistry showed that the temperature ranges between 700 and 1150°C and the pressure were less than 2 kbar.

المصادر:


  1. Abdel-Rahman A (1994) Nature of biotites from alkaline, calc-alkaline and peraluminous magmas, Journal of Petrology 35: 525– 541.
    2.
  2. Angiboust S, Agard P, De Hoog JCM, Omrani J, Plunder A (2013) Insights on deep, accretionary subduction processes fromthe Sistan ophiolitic “melange” (Eastern Iran), Lithos 156: 139–158.
    3.
  3. Arjmandzadeh R, Karimpour MH, Mazaheri SA, Santos JF, Medina JM, Homam SM, (2011) Sr/Nd isotope geochemistry and petrogenesis of the Chah-Shaljami granitoids (Lut Block, Eastern Iran), Journal of Asian Earth Sciences 41: 283–296.
    4.
  4. Babazadeh SA, de Wever P (2004) Early Cretaceous radiolarian assemblages from radiolarites in the Sistan Suture (eastern Iran), Geodiversitas 26:185–206.
    5.
  5. Beccaluva L, Macciotta G, Piccardo GB, Zeda O (1989) Clinopyroxene composition of ophiolite basalts as petrogenetic indicator, Chemical Geology 77:165-182.
    6.
  6. Bröcker M, Fotoohi Rad G, Burgess R, Theunissen S, Paderin I, Rodionov N, Salimi Z (2013) New age constraints for the geodynamic evolution of the Sistan Suture Zone, eastern Iran, Lithos 170–171: 17–34.
    7.
  7. Camp VE, Griffis RJ (1982) Character, genesis and tectonic setting of igneous rocks in the Sistan suture zone, eastern Iran, Lithos 15: 221–239.
    8.
  8. Couch SR, Sparks SJ, Carroll MR (2001) Mineral disequilibrium in lavas explained by convective self-mixing in open magma chambers, Nature 411: 1037-1039.
    9.
  9. Deer WA, Howie RA, Zussman J (1966) An introduction to the rock forming minerals, UK: Longman Group UK Ltd 528.
    10.
  10. Elthon D (1987) Petrology of the gabbroic rocks from the Mid-Cayman rise spreading centre, Journal of Geophysical Research 92: 658–682.
    11.
  11. Foster MD (1960) Layer charge relations in the dioctahedral and trioctahedral micas, American Mineralogist 45: 383-398.
    12.
  12. Ginibre C, Kronz A, Wörner G (2002) High-resolution quantitative imaging of plagioclase composition using accumulated backscattered electron images: new constraints on oscillatory zoning, Contributions to Mineralogy and Petrology 142: 436-448.
    13.
  13. Ginibre C, Wörner G, Kronz A (2007) Crystal zoning as an archive for magma evolution, Mineralogical Society of America 3(4): 261–266.
    14.
  14. Henry DJ, Guidotti CV, Thomoson JA (2005) The Ti-saturation surface for low-to-medium pressure metapelitic biotites: implications for geothermonmetry and Ti-substitution mechanisms, American Mineralogist 90: 316-328.
    15.
  15. Humphreys MCS, Blundy JD, Sparks SJ (2006) Magma evolution and opensystem processes at shiveluch volcano: insights from phenocryst zoning, Journal of Petrology 47 (12): 2303-2334.
    16.
  16. Huppert HE, Sparks RS, Turner JS (1982) Effect of volatiles on mixing in calcalkaline magma systems, Nature 297: 554-557.
    17.
  17. Kahl  M, Chakraborty S, Pompilio M, Costa F (2015) Constraints on the nature and evolution of the magma plumbing system of mt. etna volcano (1991–2008) from a combined thermodynamic and kinetic modelling of the compositional record of minerals, Journal of Petrology 56: 2025-2068.
    18.
  18. Karimpour MH, Malekzadeh Shafaroudi A, Farmer L, Stern CR (2012) Petrogenesis of Granitoids, U-Pb zircon geochronology, Sr-Nd Petrogenesis of granitoids, U-Pb zircon geochronology, Sr-Nd isotopic characteristics, and important occurrence of Tertiary mineralization within the Lut block, eastern Iran, Journal of Economic Geology 4(1): 1-27 (in Persian with English abstract).
    19.
  19. Karimpour MH, Stern CR, Farmer L, Saadat S, Malekezadeh A (2011) Review of age, Rb\Sr geochemistry and petrogenesis of Jurassic to Quaternary igneous rocks in Lut Block, Eastern Iran, Geopersia 1: 19–36.
    20.
  20. Karsli O, Aydın F, Sadıklar MB (2004) Magma interaction recorded in plagioclase zoning in granitoid systems, Zigana Granitoid, eastern Pontides, Turkey, Turkish Journal of Earth Sciences 13: 287-305.
    21.
  21. Le Base MJ (1962) The role of aluminum in igneous clinopyroxenes with relation to their Parentage, American Journal of Science 26: 267-288.
    22.
  22. Leterrier J, Maury RC, Thonon P, Girard D, Marchal M (1982) Clinopyroxene composition as a method of identification of the magmatic affinities of paleo- volcanic series, Earth and Planetary Science Letters 59(1): 139-154.
    23.
  23. Lindsley DH (1983) Pyroxene thermometry, American Mineralogist 68: 477-493.
    24.
  24. Marsh BD (1998) On the interpretation of crystal size distributions in magmatic systems, Journal of Petrology 39 (4): 553-599.
    25.
  25. Mazhari SA (2016) Geochemistry and petrogenesis of volcanic associations in Zouzan area, East of Iran, Arabian Journal of Geosciences 9: 37.
    26.
  26. McCall GJH (1997) The geotectonic history of the Makran and adjacent areas of southern Iran, Journal of Asian Earth Sciences 15: 517–531.
    27.
  27. Morimoto N (1989) Nomenclature of Pyroxenes, Canadian Mineralogist 27: 143-156. 
    28.
  28. Nachit H, Razafimahefa N, Stussi JM, Carron JP (1985) Composition chimique des biotites et typologie magmatique des granitoides, Comptes Rendus de l’Académie des Sciences Paris 301: 813-819.
    29.
  29. Nazari H, Salamati R (1999) Geological map of Sarbisheh (1:100000), Sheet 7955, Geological survey of Iran.
    30.
  30. Nisbet EG, Pearce JA (1977) Clinopyroxene composition in mafic lavas from different tectonic settings, Contributions to Mineralogy and Petrology 63: 149–160.
    31.
  31. Pang KN, Chung SL, Zarrinkoub MH, Khatib MM, Mohammadi SS, Chiu HY, Chu CH, Lee HY, Lo CH (2013) Eocene–Oligocene post-collisional magmatism in the Lut–Sistan region, eastern Iran: Magma genesis and tectonic implications, Lithos 180–181: 234–251
    32.
  32. Pang KN, Chung SL, Zarrinkoub MH, Mohammadi SS, Yang HM, Chu CH, Lee HY, Lo CH (2012) Age, geochemical characteristics and petrogenesis of Late Cenozoic intraplate alkali basalts in the Lut–Sistan region, eastern Iran, Chemical Geology 306–307: 40–53.
    33.
  33. Pietranik A, Koepke J, Puziewicz J (2006) Crystallization and resorption in plutonic plagioclase: Implications on the evolution of granodiorite magma (Gesiniec granodiorite, Strzelin Crystalline Massif, SW Poland), Lithos 86: 260-280.
    34.
  34. Renjith ML (2014) Micro-textures in plagioclase from 1994e1995 eruption, Barren Island Volcano: Evidence of dynamic magma plumbing system in the Andaman subduction zone, Geoscience Frontiers 5: 113-126.
    35.
  35. Schroder JW (1944) Essai sur la structure de l'Iran, Ecologae Geologicae Helvetiae 37: 37–81.
    36.
  36. Shabani AAT, Masoudi F, Tecce F (2010) An investigation on biotite composition from Mashhad granitoid rocks, NW Iran, Journal of Science of Islamic Republic of Iran 21: 321-331.
    37.
  37. Singer BS, Dungan MA, Layn GD (1995) Textures and Sr, Ba, Mg, Fe, K, and Ti compositional profiles in volcanic plagioclase: clues to the dynamics of calcalkaline magma chambers, American Mineralogist 80: 776-798.
    38.
  38. Smith VC, Blundy JD, Arce JL, (2009) Atemporal record of magma accumulation and evolution beneath Nevado de Toluca, Mexico, preserved in plagioclase phenocrysts, Journal of Petrology 50: 405-426.
    39.
  39. Soesoo A (1997) A multivariate statistical analysis of clinopyroxene composition: empirical coordinates for the crystallisation PT-estimations, Geological Society of Sweden (Geologiska Föreningen) 119: 55-60.
    40.
  40. Spear JA (1984) Micas in igneous rocks, In: Micas, Bailey, S.W., (ed); Mineralogical Society of America, Review in Mineralogy 13: 299-356.
    41.
  41. Stone D (2000) Temperature and pressure variations in suites of Archean felsic plutonic rocks, Berens river area, northwest superior province, Ontario, Cananda, The Canadian Mineralogist 38: 455-470.
    42.
  42. Tarabi (2018) The Study of Petrology of,  Geochemistry and Alteration of Momen Abad Area (North_East of Sarbisheh) with Reference to the Formation of Bentonite Deposits and their Industrial Application, PhD Thesis Islamic Azad University, Tehran Science and Research Branch 345p (in Persian).
    43.
  43. Tarabi S, Emami M, Modabberi S, Sheikh Zakariaee SJ (2019) Eocene-Oligocene volcanic units of momen abad, east of Iran: petrogenesis and magmatic evolution,  Iranian Journal of Earth Sciences 11(2): 126-140.
    44.
  44. Tirrul R, Bell IR, Griffis RJ, Camp VE (1983) The Sistan suture zone of eastern Iran, Geological Society of America Bulletin 94: 134–150.
    45.
  45. Tsuchiyama A (1985) Dissolution kinetics of plagioclase in the melt of the system diopside-albite-anorthite, and origin of dusty plagioclase in andesites, Contributions to Mineralogy and Petrology 89 (1): 1-16.
    46.
  46. Uchida E, Endo S, Makino M (2007) Relationship between solidification depth of granitic rocks and formation of hydrothermal ore deposits, Resource Geology 57: 47-56.
    47.
  47. Verdel C, Wernicke BP, Hassanzadeh J, Guest B (2011) A Paleogene extensional arc flare-up in Iran, Tectonics 30 (TC3008):1-20.
    48.
  48. Vernon RH, Johnson SE, Melis EA (2004) Emplacement-related microstructures in the margin of a deformed pluton:the San Jose´ tonalite, Baja California, Me´xico, Journal of Structural Geology  26: 1867–1884.
    49.
  49. Viccaro M, Calcagno R, Garozzo I (2015) Continuous magma recharge at Mt. Etna during the 2011–2013 period controls the style of volcanic activity and compositions of erupted lavas, Mineralogy and Petrology 109: 67-83.
    50.
  50. Viccaro M, Giacomoni PP, Ferlito C, Cristofolini R (2010) Dynamics of magma supply at Mt. Etna volcano (Southern Italy) as revealed by textural and compositional features of plagioclase phenocrysts, Lithos 116 (1-2): 77-91.
    51.
  51. Waight TE, Maas R, Nicholls IA (2000) Fingerprinting feldspar phenocrysts using crystal isotopic composition stratigraphy: implications for crystal transfer and magma mingling in S-type granites, Contributions to Mineralogy and Petrology 139: 227–39.
    52.
  52. Walker R, Gans P, Allen MB, Jackson J, Khatib M, Marsh N, Zarrinkoub M (2009) Late Cenozoic volcanism and rates of active faulting in eastern Iran, Geophysical Journal International 177: 783–805.
    53.
  53. Walker R, Jackson J (2002) Offset and evolution of the Gowk fault, S.E. Iran: a major intra-continental strike-slip system, Journal of Structural Geology 24: 1677–1698.
    54.
  54. Whitney DL, Evans BW (2010) Abbreviations for names of rock-forming minerals, American Mineralogist 95: 185–187.
    55.
  55. Yazdi A, Ashja-Ardalan A, Emami MH, Dabiri R,  Foudazi M (2017) Chemistry of Minerals and Geothermobarometry of Volcanic Rocks in the Region Located in Southeast of Bam, Kerman Province, Open Journal of Geology 7: 1644-1653.
    56.
  56. Yazdi A, Shahhosini E, Dabiri R,  Abedzadeh H (2019) Magmatic Differentiation Evidences And Source Characteristics Using Mineral Chemistry In The Torud Intrusion (Northern Iran), Revista GeoAraguaia 9(2): 6-21.
    57.
  57. Yu H, Xu J, Lin C, Shi L, Chen X (2012) Magmatic processes inferred from chemical composition, texture and crystal size distribution of the Heikongshan lavas in the Tengchong volcanic field, SW China, Journal of Asian Earth Sciences 58: 1-15.
    58.
  58. Zarrinkoub MH, Pang KN, Chung SL, Khatib MM, Mohammadi SS, Chiu HY, Lee HY (2012) Zircon U\Pb age and geochemical constraints on the origin of the Birjand ophiolite, Sistan suture zone, eastern Iran, Lithos 154: 392–405.
    59.

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