دوره 29، شماره 4 - ( 10-1400 )                   جلد 29 شماره 4 صفحات 746-733 | برگشت به فهرست نسخه ها


XML English Abstract Print


Download citation:
BibTeX | RIS | EndNote | Medlars | ProCite | Reference Manager | RefWorks
Send citation to:

Poormoradian Barfeh, brahimi, Nabatian, Moradian, Abbaslu. Petrology of rocks in the Karik area, east of Meiduk mine of volcanic. www.ijcm.ir 2021; 29 (4) :733-746
URL: http://ijcm.ir/article-1-1676-fa.html
پورمرادیان برفه علیرضا، ابراهیمی محمد، نباتیان قاسم، مرادیان عباس، عباسلو زهرا. سنگ‌شناسی سنگ‌های آتشفشانی منطقه کاریک، شرق معدن مس میدوک. مجله بلورشناسی و کانی شناسی ایران 1400; 29 (4) :746-733

URL: http://ijcm.ir/article-1-1676-fa.html


1- دانشگاه زنجان
2- دانشگاه شهید باهنر کرمان
3- معدن مس میدوک
چکیده:   (442 مشاهده)
پیرامون روستای کاریک در شرق معدن مس میدوک، سنگ­های آتشفشانی (بازالت آندزیتی، آندزیت، داسیت و ریولیت) و سنگ­های آذرآواری (آگلومرا و توف) ائوسن رخنمون دارند. این سنگ‌ها با تعدادی دایک‌ با ترکیبب آندزیتی قطع شده‌اند. بافت­های اصلی سنگ­های آتشفشانی پورفیری و جریانی هستند. کانی­های پلاژیوکلاز، فلدسپار قلیایی، کوارتز، کلینوپیروکسن، آمفیبول، بیوتیت و کانی‌های کدر در سنگ‌های مورد بررسی به صورت درشت‌بلور و بلورهای ریز وجود دارند. همچنین، فلدسپار (بیشتر پلاژیوکلاز) به صورت ریزبلورهای میله­ای جهت‌یافته دیده می‌شود. گاهی در درشت‌بلورهای پلاژیوکلاز، بافت­های غیرتعادلی چون بافت غربالی، تحلیل‌یافتگی و منطقه‌بندی مشاهده می‌گردند. کوارتزها لبه­های تحلیل یافته دارند. آمفیبول­ها و بیوتیت­ها از لبه‌ها به اکسیدهای آهن و تیتانیم تبدیل شده‌اند. تشکیل این بافت­ها را می­توان به فرایندهایی چون آمیختگی ماگمایی، تغییرات فشار بخار آب و کاهش فشار ناشی از صعود سریع ماگما مربوط دانست. سنگ­های آتشفشانی منطقه کاریک از سری ماگمایی آهکی قلیایی و بیشتر متاآلومین هستند. نمودارهای چندعنصری سنگ‌های مورد بررسی بهنجار شده‌ نسبت به کندریت و گوشته اولیه دارای ناهنجاری منفی عناصر با شدت میدان بالا چون P، Nb،Ta  و Ti هستند که از ویژگی‌های ماگماهای وابسته به مناطق فرورانش است. ناهنجاری مثبت شدید Pb در سنگ‌های مورد بررسی ناشی از آلایش پوسته‌ای است. الگوی عناصر خاکی نادر بهنجار شده به کندریت سنگ­های آذرین منطقه کاریک به نسبت هموار و دارای غنی‌شدگی عناصر خاکی نادر سبک (LREE) نسبت به عناصر خاکی نادر سنگین بوده که به احتمال بسیار به دلیل فراوانی LREE ها در خاستگاه و یا آلایش پوسته‌ای است. بر اساس شواهد سنگ‌شناسی و زمین شیمیایی، سنگ‌های آتشفشانی منطقه کاریک در یک محیط کمان فعال کرانه قاره‌ای و بر اثر فرورانش سنگ کره اقیانوسی نئوتتیس به زیر خرده‌قاره ایران مرکزی تشکیل شده‌اند.    
متن کامل [PDF 5907 kb]   (119 دریافت)    
نوع مقاله: پژوهشي | موضوع مقاله: تخصصي

فهرست منابع
1. [1] Berberian M., King G.C.P., "Towards a paleogeography and tectonic evolution of Iran", Canadian Journal of Earth Sciences, 18 (1981) 210-265. [DOI:10.1139/e81-019]
2. [2] Shahabpour J., "Island-arc affinity of the Central Iranian volcanic belt", Journal of Asian Earth Sciences, 30 (2007) 652-665. [DOI:10.1016/j.jseaes.2007.02.004]
3. [3] Moradian A., "Geochemistry, geochronology and petrography of feldspathoid-bearing rocks in the Urumieh-Dokhtar volcanic belt, Iran", PhD thesis, University of Wollongong, New South Wales, Australia, (1997).
4. [4] Amidi S.M., "Étude géologique de la région de Natanz-Surk (Iran, Central)", Stratigraphie et petrologie. Geological Survey and Mineral Exploration of Iran, (1977).
5. [5] Aftabi A., Atapour H., "Regional aspects of shoshonitic volcanism in Iran", Episodes, 23 (2000) 119-125.
6. [6] Torabi Gh., "Subduction-related Eocene shoshonites from the Cenozoic Urumieh-Dokhtar magmatic arc (Qaleh-Khargooshi area, western Yazdprovince, Iran)", Turkish Journal of Earth Sciences 18 (2009) 583-613.
7. [7] Ebrahimi M., Esmaeili R., Aouizerat A., "New geodynamical model for regional Tertiary extension during the Zagros orogeny: A transtensional arc?", Iranian Journal of Earth Sciences, 9(2) (2017) 115-120.
8. [8] Dimitrijevic M.I., "Geology of Shar-e-Babak region", Institute for Geological and Mining Exploration and Institution of Nuclear and Other Mineral Raw Materials, Beograd-Yugoslavia, Report Yu/52, (1973).
9. [9] Dimitrijevic M.I., Dimitrijevic M.D., Djokovic, M. " Shar-e-Babak 1:100000 Geologic map", Geological Survey and Mineral Exploration of Iran, (1971).
10. [10] Hassanzadeh J., "Metallogenic and tectono-magmatic events in SE sector of the Cenozoic active continental margin of Central Iran (Shahr-Babak, Kerman province)", Ph.D thesis, University of California, (1993) 204 p.
11. [11] Shafiei B., "Exploration assessment and geodynamic model for the Kerman Cu metallogenic belt", Ph.D. thesis, Kerman Shahid Bahonar University, (1387) (in Persian).
12. [12] Taghipur N., "Application of isotopic and fluid inclusion geochemistry in as an exploration index in the Meiduk copper mine, Shahr-e-Babak", (1386) (in Persian).
13. [13] Hibbard M.J., "The magma mixing origin of mantled feldspars", Contribution to Mineralogy and Petrology, 76 (1981) 158-170. [DOI:10.1007/BF00371956]
14. [14] Kuscu G.G., Floyd P.A., "Mineral compositional and textural evidence for magma mingling in the Saraykent volcanics", Lithos, 56(2) (2001) 207-230. [DOI:10.1016/S0024-4937(00)00051-7]
15. [15] Raymond L.A., "The study of igneous sedimentary and metamorphic rocks", McGraw-Hill, (2002) 720 p.
16. [16] Kawabata H., Shuto K., "Magma mixing recorded in intermediate rocks associated with high-Mg andesites from the Setouchi volcanic belt, Japan: implications for Archean TTG formation", Journal of Volcanology and Geothermal Research, 140(4) (2005) 241-271. [DOI:10.1016/j.jvolgeores.2004.08.013]
17. [17] Nelson S.T., Montana A., "Sieve textured plagioclase in volcanic rocks produced by rapid decompression", American Mineralogist, 77 (1992) 1242-1249.
18. [18] Tsuchiyama A., "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 (1985) 1-16. [DOI:10.1007/BF01177585]
19. [19] Stormer J.C., "Mineralogy and petrology of the Raton-Clayton volcanic field northeastern New Mexico", Geologic. Soci. America. Bull., 83 (1972) 3299-3322. [DOI:10.1130/0016-7606(1972)83[3299:MAPOTR]2.0.CO;2]
20. [20] Renjith M.L., "Micro-textures in plagioclase from 1994-1995 eruption, Barren Island Volcanoe: Evidence of dynamic magma plumbing system in the Andaman subduction zone", Geoscience Frontiers, 5 (2014) 113-126. [DOI:10.1016/j.gsf.2013.03.006]
21. [21] Best M.G., Christiansen E.H., "Igneous petrology", Blackwell, (2001) 458 pp.
22. [22] Best M.G., "Igneous and metamorphic petrology", Blackwell Science, (2003) 729 pp.
23. [23] Stephen T., Nelson A.M., "Sieve-textured plagioclase in volcanic rocks produced by rapid decompression", American Mineralogist, 77 (1992) 1242-1249.
24. [24] Shelley D., "Igneous and metamorphic rocks under the microscope", Chapman and Hall, (1993) 445 p.
25. [25] Ruprecht P., Bergantz G.W., Cooper K.M., Hildreth W., "The crustal magma storage system of Volcán Quizapu, Chile, and the effects of magma mixing on magma diversity", Journal of Petrology, 53(4) (2012) 801-840. [DOI:10.1093/petrology/egs002]
26. [26] Browne B.L., Eichelberger J.C., Patino L.C., Vogel T.A., Uto K., Hoshizumi H., "Magma mingling as indicated by texture and Sr/Ba ratios of plagioclase phenocrysts from Unzen volcano, SW Japan", Journal of volcanology and geothermal research, 154(1) (2006) 103-116. [DOI:10.1016/j.jvolgeores.2005.09.022]
27. [27] Humphreys M.C., Blundy J.D., Sparks R.S.J., "Magma evolution and open-system processes at Shiveluch Volcano: Insights from phenocryst zoning", Journal of Petrology, 47(12) (2006) 2303-2334. [DOI:10.1093/petrology/egl045]
28. [28] Feely T. C., Sharp I. D., "Chemical and hydrogen isotope evidence for in situ dehydrogenation of biotite in silicic magma chambers", Geology, 24 (1996) 1021-1024. https://doi.org/10.1130/0091-7613(1996)024<1021:CAHIEF>2.3.CO;2 [DOI:10.1130/0091-7613(1996)0242.3.CO;2]
29. [29] Rutherford M.J., Hill P.M., "Magma ascent rates from amphibole breakdown: An experimental study applied to the 1980-1986 Mount St. Helens eruptions", Journal of Geophysical Research, 98 (1993) 19667-19685. [DOI:10.1029/93JB01613]
30. [30] Donaldson C.H., Henderson C.M.B., "A new interpretation of round embayment quartz crystals", Mineralogical Magazine, 52 (1988) 27-33. [DOI:10.1180/minmag.1988.052.364.02]
31. [31] Vernon R. H., "A Practical Guide to Rock Microstucture", Cambridge University Press, Cambridge, (2004) 336 pp.
32. [32] Plechov P.Y., Tsai A.E., Shcherbakov V.D., Dirksen O.V., "Opacitization conditions of hornblende in Bezymyannyi volcano Andesites (March 30, 1956 Eruption) ", Petrology, 16(1) (2008) 19-35. [DOI:10.1134/S0869591108010025]
33. [33] Gill J.B., "Orogenic andesites and plate tectonics", Springer-Verlag, Berlin, (1981) 358 pp. [DOI:10.1007/978-3-642-68012-0]
34. [34] Le Bas M., Le Maitre R., Streckeisen A., Zanettin B., nd IUGS Subcommission on the Systematics of Igneous Rocks, "A chemical classification of volcanic rocks based on the total alkali-silica diagram", Journal of Petrology, 27(3) (1986) 745-750. [DOI:10.1093/petrology/27.3.745]
35. [35] Rollinson H.R., "Using geochemical data: Evaluation, presentation, interpretation", New York, John Wiley and Sons, (1993) 352 pp.
36. [36] Hastie A.R., Kerr A.C., Pearce J.A., Mitchell S.F., "Classification of altered volcanic island arc rocks using immobile trace elements: Development of the Th-Co discrimination diagram", Journal of Petrology, 48 (2007) 2341-2357. [DOI:10.1093/petrology/egm062]
37. [37] Shand S.J., "Eruptive rocks: Their genesis, composition, classification and their relation to ore-deposits with a chapter on meteorite", No. 552.1 S43 (1943).
38. [38] Dargahi S., "Miocene post collisional magmatism in Sarcheshmeh¬¬¬¬-Shahr-e-Babak area, northeast of Kerman: isotopic data, petrogenetic interpretation and geodynamic model for granitoid intrusions and the role of adakitic magmatism in Cu mineralization", Ph.D. thesis, Kerman Shahid Bahonar University, (1386) 311 pp. (in Persian).
39. [39] Lang J.R., "Isotopic and geochemical characteristics of Laramid igneous rocks in Arizona", Ph.D. thesis, University of Arizona (1991) 20 pp.
40. [40] Wood D.A., "The application of a Th-Hf-Ta diagram to problems of tectonomagmatic classification and to establishing the nature of crustal contamination of basaltic lavas of the British Tertiary volcanic province", Earth and planetary science letters, 50(1) (1980) 11-30. [DOI:10.1016/0012-821X(80)90116-8]
41. [41] Müller D., Rock N.M.S., Groves D.I., "Geochemical discrimination between shoshonitic and potassic volcanic rocks in different tectonic settings: A pilot study", Mineralogy and Petrology, 46(4) (1992) 259-289. [DOI:10.1007/BF01173568]
42. [42] Thompson R.N., "Magmatism of the British Tertiary volcanic province", Scottish Journal of Geology, 18(1) (1982) 49-107. [DOI:10.1144/sjg18010049]
43. [43] Glenn A.G., "The influence of melt structure on trace element partitioning near the peridotite solidus", Contributions to Mineralogy and Petrology, 147 (2004) 511-527. [DOI:10.1007/s00410-004-0575-1]
44. [44] Temizel İ., Arslan M.E.H.M.E.T., "Petrology and geochemistry of Tertiary volcanic rocks from the Likizce (ordu) area, NE Turkey: Implications for the evolution of the eastern Pontide paleo-magmatic arc", Journal of Asian Earth Scicencs, 31(4-6) (2008) 439-463. [DOI:10.1016/j.jseaes.2007.05.004]
45. [45] Kuster D., Harms U., "Post-collisional potassic granitoids form the southern and northwestern parts of the Late Neoproterozoic East African Orogen: A review", Lithos, 45 (1988) 177-195. [DOI:10.1016/S0024-4937(98)00031-0]
46. [46] Wilson M., "Igneous petrogenesis: A global tectonic approach", Unwin Hyman Ltd, (1989) 466 pp. [DOI:10.1007/978-1-4020-6788-4]
47. [47] Wu F., Jahnb B., Wildec S.A., Lod C.H., Yuie T.F., Lina Q., Gea W., Suna D., "Highly fractionated I-type granites in NE China: Isotopic geochemistry and implications for crustal growth in the Phanerozoic", Lithos 67(3-4) (2003) 191-204. [DOI:10.1016/S0024-4937(03)00015-X]
48. [48] Sun S.S., Mc Donough W.F., "Chemical and isotopic systematic of oceanic basalts: Implication for mantle composition and processes. In: Saunders, A. D. and Norry, M. J. (Eds.), magmatism in the ocean basins", Geological Society of London, Special Publications, 42 (1989) 313-345. [DOI:10.1144/GSL.SP.1989.042.01.19]
49. [49] Kamber B.S., Ewart A., Collerson K.D., Bruce M.C., McDonald G.D., "Fluid-mobile trace element constraints on the role of slab melting and implications for Archaean crustal growth models", Contributions to Mineralogy and Petrology, 144 (2002) 38-56. [DOI:10.1007/s00410-002-0374-5]
50. [50] Srivastava R.K., Singh R.K., "Trace element geochemistry and genesis of Precambrian sub-alkaline mafic dikes from the central Indian craton evidence for mantle metasomatism", Journal of Asian Earth Sciences, 23 (2004) 373-389. [DOI:10.1016/S1367-9120(03)00150-0]
51. [51] Boynton W.V., "Cosmochemistry of the rare earth elements: Meteorite studies", Developments in Geochemistry, 2 (1984) 63-114. [DOI:10.1016/B978-0-444-42148-7.50008-3]
52. [52] Kurum S., Onal A., Boztug D., Sper T., Arslan M., "Ar40/Ar39 age and geochemistry of the post-collisional Miocene Yamadag volcanics in the Arapkir area (Malatya province), eastern Anatolia, Turkey", Journal of Asian Earth Scicencs, 33 (2008) 229-251. [DOI:10.1016/j.jseaes.2007.12.001]
53. [53] Temizel I., "Petrochemical evidence of magma mingling and mixing in the Tertiary monzogabbroic stocks around the Bafra (Samsun) area in Turkey: Implications of coeval mafic and felsic magma interactions", Mineralogy and Petrology, 108(3) (2014) 353-370. [DOI:10.1007/s00710-013-0304-4]
54. [54] Geng H., Sun M., Yuan C., Xiao W., Zhao G., Zhang L., Wong K., Wu F., "Geochemical, Sr-Nd and zircon U-Pb-Hf isotopic studies of Late Carboniferous magmatism in the West Junggar, Xinjiang: Implications for ridge subduction?", Chemical Geology, 266(3-4) (2009) 364-389. [DOI:10.1016/j.chemgeo.2009.07.001]
55. [55] Leeman W.P., Sisson V.B., "Geochemistry of boron and its implication for crustal and mantle processes", Reviews in Mineralogy and Geochemistry, 33(1) (1996) 645-707. [DOI:10.1515/9781501509223-014]
56. [56] Dostal J., Church B.N., Reynolds P.H., Hopkinson L., "Eocene volcanism in the Buck Creek basin, central British Columbia (Canada): Transition from arc to extensional volcanism", Journal of Volcanology and Geothermal Research, 170(1-3) (2001) 149-170. [DOI:10.1016/S0377-0273(00)00261-4]
57. [57] Nagudi N.O., Koberl C.H., Kurat G., "Petrography and geochemistry of the Sing granite, Uganda, and implication for its origin", Journal of African Earth Sciences, 35 (2003) 51-59.
58. [58] Shang G.K., Satir M., Siebel W., Nasifa E.N., Taubuld H., Liegeoise J.P., Tchoua F.M., "Geochemistry, Rb-Sr and Sm-Nd systematic: Case of the Sangmelima region, Ntem complex, southern Cameroon", Journal of African Earth Sciences, 40(1-2) (2004) 61-79. [DOI:10.1016/j.jafrearsci.2004.07.005]
59. [59] Barnes S.J., Acterberg E., Makovicky E., Li, C., "Proton probe results for partitioning of platinum group elements between mono-sulphide solid solution and sulphide liquid", South African Journal of Geology, 104 (2001) 337-351. [DOI:10.2113/gssajg.104.4.275]
60. [60] Zhou L., Mab C., She Z., "An Early Cretaceous garnet-bearing metaluminous A-type granite intrusion in the East Qinling Orogen, Central China: Petrological, mineralogical and geochemical constraints", Geoscience Frontiers, 3(5) (2012) 635-646. [DOI:10.1016/j.gsf.2011.11.011]
61. [61] Pearce J. A., "Role of sub-continental lithosphere in magma genesis at active continental margins.In: continental basalts and mantle xenoliths. Hawkesworth, C.J. and Norry, M.J. (eds)", Nantwich: Shiva, (1983) 230-249.
62. [62] Mohajjel M., Fergusson C.L., Sahandi M.R., "Cretaceous-Tertiary convergence and continental collision, Sanandaj-Sirjan Zone, Western Iran", Journal of Asian Earth Sciences, 21(4) (2003) 397-412. [DOI:10.1016/S1367-9120(02)00035-4]
63. [63] Alavi M., "Sedimentary and Structural characteristics of the Paleo-Tethys remnants in northeastern Iran", Geological Society of America Bulletin, 103 (1391) 983-992. https://doi.org/10.1130/0016-7606(1991)103<0983:SASCOT>2.3.CO;2 [DOI:10.1130/0016-7606(1991)1032.3.CO;2]
64. [64] Ghasemi A., Talbot C.J., "A new tectonic scenario for the Sanandaj-Sirjan Zone (Iran)", Journal of Asian Earth Sciences, 26 (2005) 683-693. [DOI:10.1016/j.jseaes.2005.01.003]

ارسال نظر درباره این مقاله : نام کاربری یا پست الکترونیک شما:
CAPTCHA

بازنشر اطلاعات
Creative Commons License این مقاله تحت شرایط Creative Commons Attribution-NonCommercial 4.0 International License قابل بازنشر است.

کلیه حقوق این وب سایت متعلق به مجله بلورشناسی و کانی شناسی ایران می باشد.

طراحی و برنامه نویسی : یکتاوب افزار شرق

© 2022 CC BY-NC 4.0 | Iranian Journal of Crystallography and Mineralogy

Designed & Developed by : Yektaweb