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naseri N, Zarei Sahamieh R, Leybourne M, Costa dos Santos A, Ahmadi Khalaji A. Geochemical characteristics of potassic alkaline magmatism of the northeastern Qazvin (Pargeh area). www.ijcm.ir 2024; 32 (1) :61-74
URL: http://ijcm.ir/article-1-1856-fa.html
URL: http://ijcm.ir/article-1-1856-fa.html
ناصری ناهید، زارعی سهامیه رضا، لیبورن متیو، کاستادوس سانتوس آندرسون، احمدی خلجی احمد. ویژگی‌های زمین‌شیمیایی فعالیت ماگمایی قلیایی پتاسیمی شمال شرق قزوین (منطقه پرگه). مجله بلورشناسی و کانی شناسی ایران. 1403; 32 (1) :61-74
1- گروه زمین شناسی، دانشکده علوم پایه، دانشگاه لرستان، خرم آباد، ایران
2- گروه علوم زمین شناسی و زمین شناسی مهندسی، دانشگاه کوئینز، کینگستون، کانادا
3- گروه پترولوژی و کانی شناسی، دانشکده علوم، دانشگاه ریودژانیرو،ریودژانیرو، برزیل
2- گروه علوم زمین شناسی و زمین شناسی مهندسی، دانشگاه کوئینز، کینگستون، کانادا
3- گروه پترولوژی و کانی شناسی، دانشکده علوم، دانشگاه ریودژانیرو،ریودژانیرو، برزیل
چکیده: (880 مشاهده)
توده نفوذی پرگه در شمال شرق قزوین واقع شده است. سنگهای نفوذی این توده بیشتر شامل مونزوگابرو و الیوین گابرو بوده که از نظر کانیشناسی در بردارنده الیوین، کلینوپیروکسن، پلاژیوکلاز، بیوتیت و فلدسپار قلیایی هستند. از نظر زمین شیمیایی، این سنگها دارای ویژگی ماگماهای قلیایی پتاسیمی با غنی‌شدگی در عناصر سنگ دوست بزرگ یون ( Ba،U ،Pb ، Sr LILE:) و تهی شدگی در عناصر با شدت میدان بالا (HFSE: Nb, Ti, Zr) بوده که از این نظر شبیه فعالیت ماگمایی منطقه فرورانش و ماگماهای برآمده از گوشته هستند. الگوهای خاکی نادر (REE) بهنجار شده با کندریت غنی شدگی در عناصر خاکی نادر سبکLREE) )، با (La/Yb)N در گستره 58/8-43/4، و ناهنجاری‌های منفی جزئی (Eu/Eu* = 0.82-0.99) Eu را نشان می‌دهند. سنگهای گابرویی مورد بررسی برآمده از جدایش ماگمای اولیه ای هستند که از ذوب بخشی گوشته سنگ کره ای تهی شده با ترکیب اسپینل-پریدوتیت تشکیل شده‌اند. نسبتهای اولیه 87Sr/86Sr و 143Nd/144Nd به ترتیب، (70493/0- 70525/0 و 51272/0-51269/0) با تشکیل ماگمای مادر در گوه گوشتهای همخوانی دارند. مقادیرɛNd(i) (47/1تا 92/1) در گستره مذابهای برآمده از گوشته قرار دارند. بر پایه نتایج این پژوهش، پیشنهاد می‌شود که سنگهای نفوذی پرگه بخشی از کمربند ماگمایی البرز هستند که براساس دادههای زمین شیمیایی، محیط تشکیل آنها با یک محیط کششی پس از برخورد و پشت کمان همخوانی دارد.
فهرست منابع
1. [1] Di Giuseppe P., Agostini S., Manetti P., Savas¸çın M.Y., Conticelli S., " Sublithospheric origin of Na-alkaline and calc-alkaline magmas in a post-collisional tectonic regime: Sr-Nd-Pb isotopes in recent monogenetic volcanism of Cappadocia, Central Turkey", Lithos 316 (2018) 304-322. [DOI:10.1016/j.lithos.2018.07.018]
2. [2] Jacques G., Hoernle K., Gill J., Wehrmann H., Bindeman I., & Lara L. E., "Geochemical variations in the Central Southern Volcanic Zone, Chile (38-43 S): The role of fluids in generating arc magmas", Chemical Geology 371 (2014) 27-45. [DOI:10.1016/j.chemgeo.2014.01.015]
3. [3] Xu Y., Wang Q., Tang G., Wang J., Li H., Zhou J., Li Q., Qi Y., Liu P., Ma L., Fan J., "The origin of arc basalts: new advances and remaining questions", Science China Earth Sciences 63 (2020) 1969-1991. [DOI:10.1007/s11430-020-9675-y]
4. [4] Sander M., Olivier N., Paul R.D., Mason B. D., Benoît S., "Trace element partitioning in silica-undersaturated alkaline magmatic systems", Geochimica et Cosmochimica Acta 346 (2023) 29-53. [DOI:10.1016/j.gca.2023.01.025]
5. [5] Rostami-Hossouri M., Ghasemi H., Pang K.N., Shellnutt J.G., Rezaei-Kahkhaei M., Miao L., Mobasheri M., Iizuka Y., Lee H.Y., Lin T.H., "Geochemistry of continental alkali basalts in the Sabzevar region, northern Iran: implications for the role of pyroxenite in magma genesis", 175 Contributions to Mineralogy and Petrology 175 (2020) 1-22. [DOI:10.1007/s00410-020-01687-z]
6. [6] Salehi N, Torkian A, Furman T, le Roux P., "Petrogenesis and geochemical characteristics of Plio-Quaternary alkali basalts from the Qorveh-Bijar volcanic belt, Kurdistan Province, NW Iran", Geological Magazine 160 (2023) 888-904. [DOI:10.1017/S0016756823000018]
7. [7] Gill R.C.O., Aparicio A., El Azzouzi M., Hernandez J., Thirlwall M.F., Bourgois J., Marriner G.F., "Depleted arc volcanism in the Alboran Sea and shoshonitic volcanism in Morocco: Geochemical and isotopic constraints on Neogene tectonic processes", Lithos 78 (2004) 363-388. [DOI:10.1016/j.lithos.2004.07.002]
8. [8] Verma SP and Molaei-Yeganeh T., "Tectonic settings of the PlioQuaternary volcanism in Iran from multidimensional and multielement solutions", Geological Journal 57 (2022) 410-24. [DOI:10.1002/gj.4305]
9. [9] Schaarschmidt A., Klemd R., Regelous M., Voudouris P.C., Melfos V., and Haase K.M., "The formation of shoshonitic magma and its relationship to porphyry-type mineralisation: The Maronia pluton in NE Greece", Lithos 380-381 (2021) 105911. [DOI:10.1016/j.lithos.2020.105911]
10. [10] Ferreira V.P., Sial A.N., Pimentel M.M., Armstrong R., Guimarães I.P., Filho A.F.D.S., Lima M.M.C.D., and Silva T. R.D., "Reworked old crust-derived shoshonitic magma: The Guarany pluton, Northeastern Brazil", Lithos 232(2015) 150-161. [DOI:10.1016/j.lithos.2015.06.030]
11. [11] Feng W., Zhu Y., "Petrogenesis and tectonic implica tions of the late Carboniferous calc-alkaline and shoshonitic magmatic rocks in the Awulale mountain, western Tianshan", Gondwana Research 76 (2019) 44-61. [DOI:10.1016/j.gr.2019.05.009]
12. [12] Ahmadzadeh G., Jahangiri A., Lentz D., Mojtahedi M., "Petrogenesis of PlioQuaternary post collisional ultrapotassic volcanism in NW of Marand, NW Iran", Journal of Asian Earth Sciences 39 (2010) 37-50. [DOI:10.1016/j.jseaes.2010.02.008]
13. [13] Dabiri R., Emami M.H., Mollaei H., Chen B., Abedini M.V., Rashidnejad N., Ghaffari M., "Quaternary post-collision alkaline volcanism NW of Ahar (NW Iran): geochemical constraints of fractional crystallization process", Geologica Carpathica 62(2011) 547-562. [DOI:10.2478/v10096-011-0039-2]
14. [14] Shafaii-Moghadam H.S., Ghorbani G., Khedr M.Z., Fazlnia N., Chiaradia M., Eyuboglu Y., Santosh M., Francisco C.G., Martinez M.L., Gourgaud A., Arai S., "Late Miocene K-rich volcanism in the Eslamieh peninsula (Saray), NW Iran: implications for geodynamic evolution of the Turkish-Iran", Gondwana Research 26 (2014) 1028-1050. [DOI:10.1016/j.gr.2013.09.015]
15. [15] Prelević D., Akal C., Romer R.L., Mertz-Kraus R., Helvacı C., "Magmatic response to slab tearing: constraints from the Afyon alkaline volcanic complex, Western Turkey", Journal of Petrology 56 (2015) 527-562. [DOI:10.1093/petrology/egv008]
16. [16] Morit, R., Rezeau H., Ovtcharova M., Tayan R., Melkonyan R., Hovakimyan S., Ramazanov V., Selby D., Ulianov A., Chiaradia M., Putlitz B., "Long-lived, stationary magmatism and pulsed porphyry systems during Tethyan subduction to post-collision evolution in the southernmost Lesser Caucasus, Armenia and Nakhitchevan", Gondwana Research 37 (2016b) 465-503. [DOI:10.1016/j.gr.2015.10.009]
17. [17] Rezeau H., Moritz R., Leuthold J., Moritz R., Hovakimyan S., Tayan R., Chiaradia M., "30 Myr of Cenozoic magmatism along the Tethyan margin during Arabia-Eurasia accretionary orogenesis (Meghri-Ordubad pluton, southernmost Lesser Caucasus)", Lithos 288 (2017) 108-124. [DOI:10.1016/j.lithos.2017.07.007]
18. [18] Berberian M., 'The southern Caspian: A compressional depression floored by a trapped, modified oceanic crust", Canadian Journal of Earth Sciences 20 (1983) 163-183. [DOI:10.1139/e83-015]
19. [19] Agard P., Omrani J., Jolivet L., Whitechurch H., Vrielynck B., Spakman W., Monie P., Meyer B., Wortel R., "Zagros orogeny: a subduction-dominated process", Geological Magazine 148 (2011) 692-725. [DOI:10.1017/S001675681100046X]
20. [20] Asiabanha A., Foden J., "Post-collisional transition from an extensional volcanosedimentary basin to a continental arc in the Alborz Ranges, N-Iran", Lithos 148 (2012) 98-111. [DOI:10.1016/j.lithos.2012.05.014]
21. [21] Castro A., Aghazadeh M., Badrzadeh Z., Chichorro M., "Late Eocene-Oligocene post-collisional monzonitic intrusions from the Alborz magmatic belt, NW Iran. An example of monzonite magma generation from a metasomatized mantle source", Lithos 180 (2013) 109-127. [DOI:10.1016/j.lithos.2013.08.003]
22. [22] Aghazadeh M., Castro A., Omran N. R., Emami M. H., Moinvaziri H., & Badrzadeh Z., "The gabbro (shoshonitic)-mon- zonite-granodiorite association of Khankandi pluton, Alborz Mountains, NW Iran", Journal of Asian Earth Sciences 38 (5) (2010) 199-219. [DOI:10.1016/j.jseaes.2010.01.002]
23. [23] Aghazadeh M., Castro A., Badrzadeh Z., Vogt K., "Post-collisional polycyclic plutonism from the Zagros hinterland. The Shaivar-Dagh plutonic complex Alborz belt, Iran", Geological Magazine 148 (2011) 980-1008. [DOI:10.1017/S0016756811000380]
24. [24] Annels R.N., Arturton R.S., Bazley R.A.B., Davis R.C., Hamedi M., Rahimzahed F., Rashtian K., "Explanatory text of the Qazvin and Rasht quadrangle map", Geological Survey of Iran (1985) 94.
25. [25] Asiabanha A., Ghasemi H., & Meshkin M., "Paleogene continental‐arc type volcanism in North Qazvin, North Iran: Facies analysis and geochemistry", Neues Jahrbuch Fur Mineralogie Abhandlungen 186 (2) (2009) 201-214. [DOI:10.1127/0077-7757/2009/0144]
26. [26] Nabatian G, Giang S Y, Honarmand M and Neubauer F., "Zircon U-Pb ages, geochemical and Sr-Nd-Pb-Hf isotopic constraints on petrogenesis of the Tarom-Olya pluton, Alborz magmatic belt", Lithos 244 (2016) 43-58. [DOI:10.1016/j.lithos.2015.11.020]
27. [27] Sepidbar F., Shafaii Moghadam H., Zhang L., Li JW., Jinlong Ma., Stern RJ., Lin C., "Across-arc geochemical variations in the Paleogene magmatic belt of Iran", Lithos 344-345 (2019) 280-296. [DOI:10.1016/j.lithos.2019.06.022]
28. [28] Shafaii Moghadam H., Rossetti F., Lucci F., Chiaradia M., Gerdes, A., Lopez Martinez M.,
29. Ghorbani G., Nasrabad M., "The calcalkaline and adakitic volcanism of the Sabzevar
30. structural zone (NE Iran): implications for the Eocene magmatic flare-up in Central Iran", Lithos
31. 251 (36) (2016) 517-535.
32. [29] Whitney D.L. and Evans B.W., "Abbreviations for names of rock-forming minerals", American Mineralogist 95 (1) (2010) 158- 187. [DOI:10.2138/am.2010.3371]
33. [30] Middlemost E.A.K., "Naming materials in the magma/igneous rock system", Earth Science Reviews 37 (3-4) (1994) 215-224. [DOI:10.1016/0012-8252(94)90029-9]
34. [31] Zheng Y.F., "Subduction zone geochemistry", Geoscience Frontiers 10 (4) (2019) 1223-1254. [DOI:10.1016/j.gsf.2019.02.003]
35. [32] Henderson P., "Rare Earth Element Geochemistry", Amsterdam: Elsevier (1983) 510 pp.
36. [33] Kharbish S., "Geochemistry and magmatic setting of wadi El- Markh Island are gabbro- diorite centeral- eastern Desert, Egype", Chemie der Erode 70 (3) (2010) 257-266. [DOI:10.1016/j.chemer.2009.12.007]
37. [34] Middlemost, E.A.K., "The basalt clan", Earth Science Reviews 11(1975) 337-364. [DOI:10.1016/0012-8252(75)90039-2]
38. [35] Peccerillo A., Taylor S., "Geochemistry of Upper Cretaceous volcanic rocks from the Pontic chain, Northern Turkey", Bulletin Volcanologique 39 (2) (1975) 557-569. [DOI:10.1007/BF02596976]
39. [36] McDonough W.F., Sun, S.S., "The composition of the Earth", Chemical geology 120 (1995) 223-253. [DOI:10.1016/0009-2541(94)00140-4]
40. [37] Nakamura N., "Determination of REE, Ba, Fe, Mg, Na and K in carbonaceous ordinary Chondrites", Geochimica et Cosmochimica Acta 38 (5) (1974)757-775. [DOI:10.1016/0016-7037(74)90149-5]
41. [38] White W. M., "Geochemistry", Chichester: John Wiley and Sons, (2013) 660 p.
42. [39] Spandle C., Pirard C., "Element recycling from subducting slabs to arc crust: A review", Lithos 170-171 (2013) 208-223. [DOI:10.1016/j.lithos.2013.02.016]
43. [40] Zheng Y. F., "Metamorphic chemical geodynamics in continental subduction zones", Chemical Geology 328 (2012) 5-48. [DOI:10.1016/j.chemgeo.2012.02.005]
44. [41] Hawkesworth C.J., Turner S.P., Peate D.W., McDermott F., and van Calsteren P., "U-Th isotopes in arc magmas: Implications for element transfer from the subducted crust", Science 276 (1997) 551-555. [DOI:10.1126/science.276.5312.551]
45. [42] Fanchao M., Yulu T., Yaoqi Z., Jiaqi L., Gengchao Z., Qing D., "Cenozoic potassic volcanic rocks from the Keluo and Wudalianchi volcanic districts, northeast China: origin from the new sub-continental lithospheric mantle (SCLM) metasomatized by potassium-rich fluids from delaminated lower crust", Frontiers of Earth Science 16 (2022) 989-1004. [DOI:10.1007/s11707-021-0960-3]
46. [43] Thompson RN, Morrison MA., "Asthenospheric and lower lithospheric mantle contributions to continental extension magmatism: an example from the British Tertiary Province", Chemical Geology 68 (1988) 1-15. [DOI:10.1016/0009-2541(88)90082-4]
47. [44] Eby G.N., "Chemical subdivision of the A-type granitoids: Petrogenetic and tectonic implications", Geology 20 (1992) 641-644.
https://doi.org/10.1130/0091-7613(1992)020<0641:CSOTAT>2.3.CO;2 [DOI:10.1130/0091-7613(1992)0202.3.CO;2]
48. [45] Green T.H., "Signifcance of Nb/Ta as an indicator of geochemical processes in the crust-mantle system", Chemical Geology 120 (1995) 347-359. [DOI:10.1016/0009-2541(94)00145-X]
49. [46] Morata D., Oliva C., de la Cruz R., Suarez M., "The Bandurrias gabbro; late Oligocene alkaline magmatism in the Patagonian cordillera", Journal of South American Earth Sciences 18 (2005) 147-162. [DOI:10.1016/j.jsames.2004.09.001]
50. [47] McDonough W.F., Sun S.S., Ringwood A.E., Jagoutz E., Hofmann A.W., "K, Rb and Cs in the Earth and moon and the evolution of the Earth's mantle", Geochimica et cosmochimica acta 56 (1992) 1001-1012. [DOI:10.1016/0016-7037(92)90043-I]
51. [48] Falloon T.J., Green D.H., Danyushevsky L.V., Mcneill A.W., "The composition of near-solidus partial melts of fertile peridotite at 1 and 1.5 GPa: implications for the petrogenesis of MORB", Journal of Petrology 49 (2008) 591-613. [DOI:10.1093/petrology/egn009]
52. [49] Foley S.F., Venturelli G., Green D.H., Toscani L., "The ultrapotassic rocks: Characteristics, classifcation and constraints for petrogenetic models", Earth Science Reviews 24 (1987) 81-134. [DOI:10.1016/0012-8252(87)90001-8]
53. [50] Lustrino M., Wilson M., "The circum-Mediterranean anorogenic Cenozoic igneous province", Earth Science Reviews 81 (2007) 1-65. [DOI:10.1016/j.earscirev.2006.09.002]
54. [51] Mouthereau F., Lacombe O., Vergés J., "Building the Zagros collisional orogen: Timing, strain distribution and the dynamics of Arabia/Eurasia plate convergence", Tectonophysics 532-535 (2012) 532-560. [DOI:10.1016/j.tecto.2012.01.022]
55. [52] Verdel C., Wernicke B.P., Hassanzadeh J., Guest B., "A Paleogene extensional arc flare-up in Iran", Tectonics 30 (2011) TC3008. [DOI:10.1029/2010TC002809]
56. [53] Pearce J.A.,"Geochemical fingerprinting of oceanic basalts with applications to ophiolite classification and the search for Archean oceanic crust", Lithos 100 (2008) 14-48. [DOI:10.1016/j.lithos.2007.06.016]
57. [54] Azizi H., Jahangiri A., "Cretaceous Subduction-Related Volcanism in the Northern
58. Sanandaj-Sirjan Zone, Iran", Journal of Geodynamics 45 (2008) 178-190. [DOI:10.1016/j.jog.2007.11.001]
59. [55] Shaw D.M., "Trace element fractionation during anatexis", Geochimica et Cosmochimica Acta 34 (1970) 237-243. [DOI:10.1016/0016-7037(70)90009-8]
60. [56] Sun C.H., Stern R., "Genesis of Mariana shoshonites: contribution of the subduction
61. component", Journal of Geophysical Research 106 (2001) 589-608. [DOI:10.1029/2000JB900342]
62. [57] Floyd P., Kelling G., Gökçen S., Gökçen N., "Geochemistry and tectonic environment of basaltic rocks from the Misis ophiolitic mélange, south Turkey", Chemical Geology 89 (1991) 263-280. [DOI:10.1016/0009-2541(91)90020-R]
63. [58] Shervais J.W., "Ti-V plots and the petrogenesis of modern and ophiolitic lavas", Earth and planetary science letters 59 (1982) 101-118. [DOI:10.1016/0012-821X(82)90120-0]
64. [59] 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 (1992) 259-289. [DOI:10.1007/BF01173568]
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