دوره 28، شماره 4 - ( 10-1399 )
جلد 28 شماره 4 صفحات 1022-1009 |
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Esna-Ashari, Tiepolo, Ghorbani. On the use of major and trace elements composition of pyroxene and amphibole in the genesis of Boroujerd quartz-diorite. www.ijcm.ir 2020; 28 (4) :1009-1022
URL: http://ijcm.ir/article-1-1564-fa.html
URL: http://ijcm.ir/article-1-1564-fa.html
اثنی عشری امیر، تیه پولو ماسیمو، قربانی قاسم. سنگ‌زایی کوارتز دیوریت بروجرد بر پایه زمین‌شیمی عناصر اصلی و کمیاب کانی‌های پیروکسن و آمفیبول. مجله بلورشناسی و کانی شناسی ایران. 1399; 28 (4) :1009-1022
امیر اثنی عشری*1 
، ماسیمو تیه پولو2 ، قاسم قربانی3
، ماسیمو تیه پولو2 ، قاسم قربانی3
1- دانشگاه پیام نور
2- دانشگاه میلان
3- دانشگاه دامغان
2- دانشگاه میلان
3- دانشگاه دامغان
چکیده: (1880 مشاهده)
مجموعه آذرین بروجرد (گرانیت، گرانودیوریت و کوارتزدیوریت) در نیمه شمالی نوار سنندج-سیرجان واقع است. در این پژوهش، فراوانی عناصر اصلی و کمیاب در کلینوپیروکسن و آمفیبول موجود در کوارتزدیوریت اندازه‌گیری و ترکیب شیمیایی مذاب اولیه‌ای که این کانی‌ها از آن متبلور شده‌اند، محاسبه گردید. ترکیب شیمیایی این مذاب با کوارتز دیوریت بروجرد و همچنین کوارتز دیوریت و سنگ فرامافیک الیگودرز در کنار مجموعه بروجرد مقایسه شد. نتیجه این مقایسه به همراه مدلسازی‌های شیمیایی نشان می‌دهند که ماگمایی مشابه با کوارتز دیوریت الیگودرز دستخوش تبلور بخشی و هضم همزمان سنگ فرامافیک شده است. پیروکسن و آمفیبول از این ماگمای دگرگونه متبلور شده‌اند. سپس این ماگما با ماگمایی مشابه با کوارتز دیوریت الیگودرز آمیخته شده و کوارتز دیوریت بروجرد به وجود آمده است. نقش سنگ‌های فرامافیک در تشکیل کوارتز دیوریت بروجرد نشان می‌دهد که آنها با وجود رخنمون کم در سطح زمین، حجم قابل توجهی در اعماق دارند.
واژه‌های کلیدی: کوارتزدیوریت، سنگ فرامافیک، آمیختگی ماگمایی، هضم و تبلور بخشی، بروجرد، سنندج-سیرجان.
فهرست منابع
1. [1] Tiepolo M., Langone A., Morishita T., Yyhara M., "On the recycling of amphibole-rich ultramafic intrusive rocks in the arc crust: evidence from Shikanoshima island (Kyushu, Japan)", Journal of Petrology 53 (2012) 1255-1285. [DOI:10.1093/petrology/egs016]
2. [2] Aliani F., Younessi R., Mücke A., Miri M., "Geochemistry and mineralogy of hornblendite horizons in the Galali and Baba-Ali Iron deposits and their comparison (in Persian)", Iranian Journal of Crystallography and Mineralogy 19 (2011) 385-398.
3. [3] Esna-Ashari A., Sarjoughian F., "Origin of olivine in Molataleb ultramafic rocks and the role of olivine on magma evolution (in Persian)", Iranian Journal of crystallography and mineralogy 24 (2016) 145-154.
4. [4] Esna-Ashari A., Sarjoughian F., "Contribution of ultramafic rocks in central Sanandaj-Sirjan zone to the characterizing of physio-chemical condition during initiation of subduction (in Persian)", Petrology 32 (2018) 45-66.
5. [5] Ravankhah A., Moayyed M., Hosseinzadeh M.R., Azimzadeh A.M., Hassanzadeh J., Amel N., "Petrographical, mineral chemical and geochemical studies of the lamprophyric bodies and alkaline gabbro from the Houway area (NE Hourand-NW Iran) (in Persian)", Iranian Journal of crystallography and mineralogy 23 (2015) 555-568.
6. [6] Tiepolo M., Tribuzio R., "Petrology and U-Pb zircon geochronology of amphibole-rich cumulates with sanukitic affinity from Husky Ridge (Northern Victoria Land, Antarctica): insights into the role of amphibole in the petrogenesis of subduction-related magmas", Journal of Petrology 49 (2008) 937-970. [DOI:10.1093/petrology/egn012]
7. [7] Khalilzadeh H., Alipour S., Abedini A., "Investigation of adakitic feature and magmatic origin of mineralized monzonitic stock in the Niza area, northwest Iran (in Persian)", Iranian Journal of crystallography and mineralogy 28 (2020) 3-16. [DOI:10.29252/ijcm.28.1.3]
8. [8] Gardideh S., Ghasemi H., Sadeghian M., "U-Pb age dating on zircon crystals, Sr-Nd isotope ratios and geochemistry of Neogene adakitic domes of Quchan-Esfarayen magmatic belt, NE Iran (in Persian)", Iranian Journal of crystallography and mineralogy 26 (2018) 455-478. [DOI:10.29252/ijcm.26.2.455]
9. [9] Torkian A., "Textural and mineral chemistry features of the Qorveh granitoid complex (Kurdistan): evidence for magma mingling/mixing processes (in Persian)", Iranian Journal of crystallography and mineralogy 20 (2012) 331-342. [DOI:10.1007/978-3-642-12496-9_20]
10. [10] Esna-Ashari A., Tiepolo M., Valizadeh M.V., Hassanzadeh J., Sepahi A.A., "Geochemistry and zircon U-Pb geochronology of Aligoodarz granitoid complex, Sanandaj-Sirjan Zone, Iran", Journal of Asian Earth Sciences 43 (2012) 11-22. [DOI:10.1016/j.jseaes.2011.09.001]
11. [11] Sahandi M.R., Radfar J., Hoseinidoust J., Mohajjel M., "Geologic map of the Shazand, scale 1:100000", Geological Survey of Iran (2006).
12. [12] Ahmadi Khalaji A.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]
13. [13] Esna-Ashari A., Tiepolo M., Hassanzadeh J., "On the occurrence and implications of Jurassic primary continental boninite-like melts in the Zagros orogen", Lithos 258-259 (2016) 37-57. [DOI:10.1016/j.lithos.2016.04.017]
14. [14] Esna-Ashari A., Hassanzadeh J., "Arc-type magmatism in middle part of the Sanandaj-Sirjan Zone (western Iran) and geochemical characterization of the granitoids of this area (in Persian)", Iranian Journal of Geology 8 (2014) 85-96.
15. [15] Agard A., Omrani J., Jolivet L., Whitechurch H., Vrielynck B., Spakman W., Monte P., Meyer B., Wortel R., "Zagros orogeny: a subduction-dominated process", Geological Magazine 148 (2011) 692-725. [DOI:10.1017/S001675681100046X]
16. [16] Arvin M., Pan Y., Dargahi S., Malekizadeh A., Babaei, A., "Petrochemistry of the Siah-Kuh granitoid stock southwest of Kerman, Iran: implications for initiation of Neotethys subduction", Journal of Asian Earth Sciences 30 (2007) 474-489. [DOI:10.1016/j.jseaes.2007.01.001]
17. [17] Shakerardakani F., Neubauer F., Masoudi F., Mehrabi B., Liu X., Dong Y., Mohajjel M., Monfaredi B., Friedl G., "Panafrican basement and Mesozoic gabbro in the Zagros orogenic belt in the Dorud-Azna region (NW Iran): laser-ablation ICP-MS zircon ages and geochemistry", Tectonophysics 647-648 (2015) 146-171. [DOI:10.1016/j.tecto.2015.02.020]
18. [18] Allen M.B., "Discussion on the Eocene bimodal Piranshahr massif of the Sanandaj-Sirjan zone, west Iran: a marker of the end of collision in the Zagros orogen", Journal of the Geological Society of London 166 (2009) 981-982. [DOI:10.1144/0016-76492009-020]
19. [19] 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 (2003) 397-412. [DOI:10.1016/S1367-9120(02)00035-4]
20. [20] Ahmadi Khalaji A., "Petrology of the granitoid rocks of the Boroujerd area (in Persian)", Ph.D Thesis (2006) University of Tehran, Tehran, Iran.
21. [21] Esna-Ashari A., Valizadeh M.V., Soltani A., "Petrogenesis of microgranular enclaves in Aligoudarz granodiorite (in Persian)", Iranian Journal of crystallography and mineralogy 22 (2014) 521-534.
22. [22] Esna-Ashari A., Valizadeh M.V., Soltani A., Sepahi A.A., "Petrology and Geochemistry of Aligoodarz Granitoid, Western Iran: implications for petrogenetic relation with Boroujerd and Dehno granitoids", Geopersia 1 (2011) 67-86.
23. [23] Mansouri Esfahani M., Khalili M., "Mineralogy and mineral - chemistry of tourmaline and garnet from Molataleb village granitoid (North of Aligudarz) NW of Isfahan (in Persian)", Iranian Journal of crystallography and mineralogy 22 (2014) 139-148.
24. [24] Salami S., Sepahi S.S., Maanijou M., "Petrography and mineral chemistry of layered pegmatite-aplite dykes from east of Boroujerd (in Persian)", Iranian Journal of crystallography and mineralogy 24 (2016) 19-32.
25. [25] Coltorti M., Bonadiman C., Faccini B., Grégoire M., O'Reilly S.Y., Powell W., "Amphiboles from suprasubduction and intraplate lithospheric mantle", Lithos 99 (2007) 68-84. [DOI:10.1016/j.lithos.2007.05.009]
26. [26] Nisbet E.G., Pearce J.A., "Clinopyroxene Composition in Marie Lavas from Different Tectonic Settings", Contributions to Mineralogy and Petrology 63 (1977) 149-160. [DOI:10.1007/BF00398776]
27. [27] Beccaluva L., Macciotta G., Piccardo G.B., Zeda O., "Clinopyroxene composition of ophiolite basalts as petrogenetic indicator", Chemical Geology 77 (1989) 165-182. [DOI:10.1016/0009-2541(89)90073-9]
28. [28] Peighambari S., "Tectonomagmatic characteristics of ophiolitic gabbroids from south Orzuieh (south of Baft, Kerman) ophiolite complex: insights from clinopyroxene chemistry (in Persian)", Iranian Journal of crystallography and mineralogy 26 (2018) 301-314. [DOI:10.29252/ijcm.26.2.301]
29. [29] Adam J., Green T., "Trace element partitioning between mica- and amphibole-bearing garnet lherzolite and hydrous basanitic melt: 1. Experimental results and the investigation of controls on partitioning behavior", Contributions to Mineralogy and Petrology 152 (2006) 1-17. [DOI:10.1007/s00410-006-0085-4]
30. [30] Tiepolo M., Oberti R., Zanetti A., Vannucci R., Foley S.F., "Trace-element partitioning between amphibole and silicate melt", Reviews in Mineralogy and Geochemistry 67 (2007) 417-452. [DOI:10.2138/rmg.2007.67.11]
31. [31] Dunn T., Sen C., "Mineral/matrix partition coefficients for orthopyroxene, plagioclase, and olivine in basaltic to andesitic systems: A combined analytical and experimental study", Geochimica et Cosmochimica Acta 58 (1994) 717-733. [DOI:10.1016/0016-7037(94)90501-0]
32. [32] Pearce J.A., Peate D.W., "Tectonic implication of the composition of volcanic arc magmas", Annual Review of Earth and Planetary Sciences 23 (1995) 251-285. [DOI:10.1146/annurev.ea.23.050195.001343]
33. [33] Sun S.S., McDonough W.F., "Chemical and isotopic systematics of oceanic basalts: implications for mantle composition and processes" Geological Society of London 42 (1989) 313-345. [DOI:10.1144/GSL.SP.1989.042.01.19]
34. [34] Esna-Ashari A., Tiepolo M., "Petrogenesis of gabbroic rocks from the Malayer plutonic complex (Sanandaj-Sirjan zone, west Iran)", PERIODICO di MINERALOGIA 89 (2020) 91-104.
35. [35] Ersoy Y., Helvacı C., "FC-AFC-FCA and mixing modeler: a Microsoft Excel spreadsheet program for modeling geochemical differentiation of magma by crystal fractionation, crustal assimilation and mixing", Computers and Geosciences 36 (2010) 383-390. [DOI:10.1016/j.cageo.2009.06.007]
36. [36] Chappell B.W., White A.J.R., Williams I.S., Wyborn D., "Low- and high-temperature granites", Transactions of the Royal Society of Edinburgh: Earth Sciences 95 (2004) 125-140. [DOI:10.1017/S0263593300000973]
37. [37] Ahmadi Khalaji A., Tahmasbi Z., Zarei Sahamieh R., "Petrography and mineral chemistry of the Boroujerd pluton (Sanandaj-Sirjan zone, western Iran)", Journal of Applied Sciences 9 (2009) 843-853. [DOI:10.3923/jas.2009.843.853]
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