دوره 31، شماره 1 - ( 1-1402 )
جلد 31 شماره 1 صفحات 74-59 |
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Tajbakhsh G, Khodami M, Monsef R. Mineral chemistry and geothermo-barometry based on amphibole of alkali gabbro dykes of Zarigan, northeast of Bafq. www.ijcm.ir 2023; 31 (1) :59-74
URL: http://ijcm.ir/article-1-1738-fa.html
URL: http://ijcm.ir/article-1-1738-fa.html
تاج بخش غلامرضا، خدامی مهناز، منصف رضا. شیمی کانی و زمین دما-فشارسنجی بر پایه کانی آمفیبول دایک‌های قلیایی گابرویی زریگان،
شمال شرق بافق. مجله بلورشناسی و کانی شناسی ایران. 1402; 31 (1) :59-74
غلامرضا تاج بخش*1 
، مهناز خدامی1 ، رضا منصف2
، مهناز خدامی1 ، رضا منصف2
1- دانشگاه یزد
2- دانشگاه آزاد اسلامی
2- دانشگاه آزاد اسلامی
چکیده: (1430 مشاهده)
دایک‌های مافیک بسیاری با سن پالئوزوئیک پیشین در توده گرانیتوئیدی زریگان و واحدهای رسوبی میزبان آن در شمال شرق شهر بافق نفوذ کردهاند. این دایک‌ها از نظر سنگشناسی، قلیایی گابرو تا مونزوگابرو با بافت‌های دانه متوسط تا ریز بین دانهای تا دانهای هستند. کانی‌های اصلی کلینوپیروکسن، آمفیبول و پلاژیوکلاز به همراه مقادیر کمتری بیوتیت، الیوین، فلدسپار قلیایی و نفلین در این سنگ‌ها دیده میشوند. آمفیبول‌ها از گروه کلسیمی و از نوع کرسوتیت - کرسوتیت پتاسیمی هستند. محاسبات زمین دما-فشارسنجی بر پایه این کانی، فشار و دمای تبلور کرسوتیت را 2/8-3/6 کیلوبار و 1113-1040 درجه سانتیگراد مشخص کردهاند. براساس ترکیب زمین شیمیایی، کرسوتیت‌ها در گستره آمفیبول‌های قلیایی، برآمده از گوشته و مربوط به محیط‌های زمینساختی کشش درون قارهای قرار دارند. با توجه به شواهد، این کانیها در ماگماهای برآمده از خیز سست کرهای آغاز کافت پالئوتتیس به همراه عملکردهای کششی گسل‌های بنیادی قطعه پشت بادام متبلور شدهاند.
واژه‌های کلیدی: آمفیبول، کرسوتیت، زمین دما-فشارسنجی، پالئوتتیس کافت، بافق.
فهرست منابع
1. [1] Martin R. F., "Amphiboles in the igneous environment, Reviews in Mineralogy and Geochemistry", 67 (2007) 323-358. [DOI:10.2138/rmg.2007.67.9]
2. [2] Mutch E. J. F., Blundy J. D., Tattitch B. C., Coope, F. J., Brooker R. A., "An experimental study of amphibole stability in low-pressure granitic magmas and a revised Al-in-hornblende geobarometer", Contributions to Mineralogy and Petrology, 171 (2016) (10) 1-27. [DOI:10.1007/s00410-016-1298-9]
3. [3] Ridolfi F., Renzulli A., Puerini M., "Stability and chemical equilibrium of amphibole in calc-alkaline magmas: an overview, new thermobarometric formulations and application to subduction-related volcanoes", Contribution to Mineralogy and petrology, 160(2010) 45-66. [DOI:10.1007/s00410-009-0465-7]
4. [4] Putirka K., "Amphibole thermometers and barometers for igneous systems and some implications for eruption mechanisms of felsic magmas at arc volcanoes", Am. Mineral., 101 (2016) 841-858. [DOI:10.2138/am-2016-5506]
5. [5] Hagen E., "A Comparative Study of Kaersutite in the Egersund Dikes and SNC Meteorites" Doctoral dissertation", The Ohio State University (2017) 42 p.
6. [6] Balaghi Z., Sadegheian M., Ghasemi, H., "Petrogenesis of the lower Paleozoic igneous rocks, south of Bahabad (bafq, Central Iran): implication for rifting", Iranian Journal of Petrology, 1 (2011) 45-64.
7. [7] Rajabi A., Canet C., Rastad E., Alfonso, P., "Basin evolution and stratigraphic correlation of sedimentary-exhalative Zn. Pb deposits of the Early Cambrian Zarigan. Chahmir Basi Central Iran", Ore Geology Reviews, 64 (2015) 328-353. [DOI:10.1016/j.oregeorev.2014.07.013]
8. [8] Niktabar S. M., Rashidnejad Omran N., "Geochemistry and petrology of rift-related mafic sills and arc-related Gabbro-Diorite bodies, Northern Bafq District, Central Iran", Acta Geochim 37 (2018) 180-192. [DOI:10.1007/s11631-017-0191-1]
9. [9] Tajbakhsh G., "Petrography, geochemistry and tectonic setting of mafic dyke swarms of Zrigan granitoid, north of Bafq (Central Iran)", Geosciences 30 (2020) 175-188.
10. [10] Mehdipour Ghazi J., Moazzen, M., Rahgoshay M., Wilde S. A., "Zircon U-Pb-Hf isotopes and whole rock geochemistry of magmatic rocks from the Posht-e-Badam Block: A key to tectonomagmatic evolution of Central Iran", Gondwana Research 87 (2020) 162-187. [DOI:10.1016/j.gr.2020.06.010]
11. [11] Alavi M., "Sedimentary and structural characteristics of the paleo-tethys remnants in northern Iran", Geological Society of American Bulletin 103 (1991) 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]
12. [12] Majidi J., Babakhani A.R., "Geological map of Ariz", Tehran. Geological survey of Iran, scale 1:100000, (2000).
13. [13] Ramezani J.,Tucker R., "The Saghand region, Central Iran: U/Pb geochronology, petrogenesis and implication for Gondwana tectonics", American Journal of Science, 303 (2003) 622-665. [DOI:10.2475/ajs.303.7.622]
14. [14] Jami M., "Geology, Geochemistry Esfordi Phosphate-Iron Deposit, Bafq Area, Central Iran", PhD thesis, The University of new South wallets, (2005) 384 p..
15. [15] Leake B.E., Woolley A. R., Arps C. E., Birch W. D., Gilbert M. C., Grice, J. D., Youzhi, G., "Nomenclature of amphiboles: report of the subcommittee on amphiboles of the international mineralogical association", American Mineralogist 83 (1997) 1019-1037.
16. [16] Giret A., Bonin B., Léger J.M., "Amphibole compositional trends in oversaturated and undersaturated alkaline plutonic ring complexes", The Canadian Mineralogist, 18 (1980) 481-495.
17. [17] Plat R.G., "The ijolite-series rocks. In: Mitchell, R.H. Eds., Undersaturated Alkaline Rocks: Mineralogy, Petrogenesis and Economic Potential", Mineralogical Association of Canada Short Course 24 (1996) 101-122.
18. [18] Nachit H., Ibhi A., Abia E.H., Ohoud M.B., "Discrimination between primary magmatic biotites, reequilibrated biotites and neoformed biotites", Comptes rendus Geoscience, 337, (2005) 1415-1420. [DOI:10.1016/j.crte.2005.09.002]
19. [19] Foster M. D., ''Interpretation of the composition of the trioctahedral micas'', United States Geological Survey Professional Paper, 354 (1960) 11-49. [DOI:10.3133/pp354B]
20. [20] Hollister L.S., Grissom G.C., Peters E.K., Stowell H.H., Sisson V.B., "Confirmation of the empirical correlation of Al in hornblende with pressure of solidification of calc-alkaline plutons", American Mineralogist, 72 (1987) 231-239.
21. [21] Hammarstrom J.M., Zen E.A., "Aluminum in hornblende: An empirical igneous geobarometer", American Mineralogist, 71 (1986) 1297-1313.
22. [22] Johnson M.C., Rutherford M.J., "Experimental calibration of the aluminum-in hornblende geobarometer with application to Long Valley (California) volcanic rocks", Geology, 17 (1989) 837-841.
https://doi.org/10.1130/0091-7613(1989)017<0837:ECOTAI>2.3.CO;2 [DOI:10.1130/0091-7613(1989)0172.3.CO;2]
23. [23] Schmidt M. W., "Amphibole composition in tonalite as a function of pressure: an experimental calibration of the Al -in hornblende barometer", Contribution to Mineralogy and Petrology, 110 (1992) 304-310. [DOI:10.1007/BF00310745]
24. [24] Colombi A., "Me ́tamorphism et ge ́ochimie des rochesmafiques des Alpesouest-centrales (géoprofil Vie'ge-Domodosso la Locarno)", Mem Geol Lausanne 4 (1989).
25. [25] Helz R.T., "Phase rections of basaltsin their meling range at PH2O=5kb. Part II. Melt composition", Journal of Petrology, 17 (1973) 139-193. [DOI:10.1093/petrology/17.2.139]
26. [26] Ernst W. G., Liu J., "Experimental phaseequilibrium study of Al- and Ti-contents of calcicamphibole in MORB- A semiquantitative thermobarometer", American Mineralogist, 83 (1998) 952-969. [DOI:10.2138/am-1998-9-1004]
27. [27] Liao Y., Wei C., Rehman H. U., Titanium in calcium amphibole: Behavior and thermometry. American Mineralogist Materials, 106 (2021) 180-191. [DOI:10.2138/am-2020-7409]
28. [28] Humphreys M.C.S., Edmonds M., Christopher T., Hards V., "Chlorine variations in the magma of Soufrie're Hills Volcano,Montserrat: Insights from Cl in hornblende and melt inclusions", Geochimica et Cosmochimica Acta 73 (2009) 5693-5708. [DOI:10.1016/j.gca.2009.06.014]
29. [29] Frost D.J., "The stability of hydrous mantle phases", Reviews in Mineralogy and Geochemistry 62 (2006) 243-271. [DOI:10.2138/rmg.2006.62.11]
30. [30] Douce A. E. P., "Titanium substitution in biotite: an empirical model with applications to thermometry, O2 and H2O barometries, and consequences for biotite stability", Chemical Geolog, 108 (1993) 133-162. [DOI:10.1016/0009-2541(93)90321-9]
31. [31] Henry D.J., Guidotti C.V., Thomson J.A., "The Ti-saturation surface for low-to-medium pressure metapelitic: Implications for geothermometry and Ti-substitution mechanisms", American Mineralogist 90 (2005) 316-328. [DOI:10.2138/am.2005.1498]
32. [32] Mann U., Marks M., & Markl G., "Influence of oxygen fugacity on mineral compositions in peralkaline melts: The Katzenbuckel volcano, Southwest Germany", Litho, 91 (2006) 262-285. [DOI:10.1016/j.lithos.2005.09.004]
33. [33] Wones D. R., "Significance of the assemblage titanite+magnetite+quartz in granitic rocks", American Mineralogist, 74 (1989) 744-749.
34. [34] Anderson J. L., Smith D. R., "The effects of temperature and fO2 on the Al-in-hornblende barometer", American Mineralogist, 80 (1995) 549-559. [DOI:10.2138/am-1995-5-614]
35. [35] Jiang C.Y., An S.Y., "On chemical characteristics of calcic amphiboles from igneous rocks and their petrogenesis significance (in Chinese with English abstract)", Journal of Mineralogy and Petrology, 3 (1984) 1-9.
36. [36] Coltorto M., Bondaiman C., Faccini B., Geogoire M., O'Reilly S.Y., Powell W., "Amphibol from suprasubduction and intraplate lithospheric mantle", Lithos, 99 (2007) 68-84. [DOI:10.1016/j.lithos.2007.05.009]
37. [37] Mayer B., Jung S., Romer R. L., Pfänder J. A., Klügel A., Pack A., Gröner E., "Amphibole in alkaline basalts from intraplate settings: implications for the petrogenesis of alkaline lavas from the metasomatised lithospheric mantle", Contributions to Mineralogy and Petrology 167 (2014) 1-22. [DOI:10.1007/s00410-014-0989-3]
38. [38] Ulrych J., Krmíček L., Teschner C., Skála R., Adamovič J., Ďurišová J., Radoň M., "Chemistry and Sr-Nd isotope signature of amphiboles of the magnesio-hastingsite-pargasite-kaersutite series in Cenozoic volcanic rocks: Insight into lithospheric mantle beneath the Bohemian Massif", Lithos 312 (2018) 308-321. [DOI:10.1016/j.lithos.2018.05.017]
39. [39] McSween Jr H. Y., "What we have learned about Mars from SNC meteorites", Meteoritics 29 (1994) 757-779. [DOI:10.1111/j.1945-5100.1994.tb01092.x]
40. [40] Chiu H. Y., Chung S. L., Zarrinkoub M. H., Melkonyan R., Pang K. N., Lee H. Y., Khatib M. M., "Zircon Hf isotopic constraints on magmatic and tectonic evolution in Iran: Implications for crustal growth in the Tethyan orogenic belt" Journal of Asian Earth Sciences 145 (2017) 652-669. [DOI:10.1016/j.jseaes.2017.06.011]
41. [41] Lasemi Y., "Depositional environments of the Ordovician rocks of Iran (syn-rift sequence) and formation of the Paleotethys passive margin" Proceedings of the 17th annual meeting of the Geological Survey of Iran Tehran, Iran (in Persian) (1999).
42. [42] Ghasempour M. R., Davoudian A. R., Shabanian N., Moeinzadeh H., Nakashima K., "Geochemistry and mineral chemistry of gabbroic rocks from Horjand of Kerman province, Southeast of Iran: Implications for rifting along the northeastern margin of Gondwana", Journal of Geodynamics 133 (2020): 101675. [DOI:10.1016/j.jog.2019.101675]
43. [43] Golestani M., "Characteristics of tectono-magmatic alkali gabbros in northern Fathabad, Zarand (NW Kerman): based on the pyroxene mineral chemistry", Iranian Journal of Crystallography and Mineralogy 28 (2020) 311-328. [DOI:10.29252/ijcm.28.2.311]
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