Volume 26, Issue 2 (7-2018)                   www.ijcm.ir 2018, 26(2): 287-300 | Back to browse issues page

XML Persian Abstract Print

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

Distribution of trace and rare earth elements among metamorphic phases and relict clinopyroxenes in epidote- amphibolites from the North of Urmia, NW Iran. www.ijcm.ir. 2018; 26 (2) :287-300
URL: http://ijcm.ir/article-1-1098-en.html
Abstract:   (173 Views)
Rare earth and trace element concentrations of mineral assemblages including amphibole, plagioclase, epidote group minerals (zoisite and clinozoisite) and relict clinopyroxenes from parental rock of epidote amphibolite from north of Urumia were obtained in situ by LA-ICP-MS analysis. The obtained data were used to study distribution of trace elements among metamorphic phases and relict clinopyroxenes from parental rock. In the studied rocks, compatible elements (Sc, V, Ni and Cr), HSFE (Ti, Ta, Hf and Nb) and MREE were concentrated in amphibole, LREE and LILE were collected into plagioclase and epidote group minerals were gathered HREE accompanied with Eu. The observed REE trends in epidote group minerals in north of the Urmia epidote- amphibolites are unlike to common reported trends for this mineral group in the other parts of the world. Rare earth element geochemistry of the epidote group minerals from the north of Urmia indicates enrichment of HREE and MREE relative to LREE. Relative similarities for rare earth and trace element concentrations of amphibole and relict clinopyroxenes from parental rock indicates that the geochemical features of amphibole were inherited probably from primary clinopyroxenes.
Full-Text [PDF 121 kb]   (62 Downloads)    
Type of Study: Research | Subject: Special
Received: 2018/07/7 | Accepted: 2018/07/7 | Published: 2018/07/7

1. [1] Spandler C., Hermann J., Arculus R., Mavrogenes J., "Redistribution of trace elements during prograde metamorphism from lawsonite blueschist to eclogite facies; implications for deep subduction-zone processes" Contributions to Mineralogyand Petrology 146(2) (2003), 205-222. [DOI:10.1007/s00410-003-0495-5]
2. [2] Xiao Y., Niu Y., Li H., Wang H., Liu X., Davidson J., "Trace element budgets and (re-) distribution during subduction-zone ultrahigh pressure metamorphism: Evidence from Western Tianshan, China" Chemical Geology, 365 (2014), 54-68. [DOI:10.1016/j.chemgeo.2013.12.005]
3. [3] Sassi R., Harte B., Carswell D.A., Yujing H., "Trace element distribution in Central Dabie eclogites" Contributions to Mineralogy and Petrology 139(3) (2000), 298-315. [DOI:10.1007/s004100000133]
4. [4] El Korh A., Schmidth S.T., Ulianov A., Potel S., "Trace element partitioning in HP-LT metamorphic assemblages during subduction-related metamorphism, Ile de Groix, France: a detailed LA-ICPMS study" Journal of Petrology 50 (2009) 1107-1148. [DOI:10.1093/petrology/egp034]
5. [5] Mulrooney D., Rivers T., "Redistribution of the rare-earth elements among coexisting minerals in metamafic rocks across the epidote-out isograd: an example from the St. Anthony Complex, northern Newfoundland, Canada" The Canadian Mineralogist, 43 (2005), 263-294. [DOI:10.2113/gscanmin.43.1.263]
6. [6] Bea F., Montero P., Garuti G., Zacharini F., "Pressure-Dependence of Rare Earth Element Distribution in Amphibolite- and Granulite- Grade Garnets. A LA-ICP-MS Study" Geostandards Newsletter, 21 (1997), 253-270. [DOI:10.1111/j.1751-908X.1997.tb00674.x]
7. [7] Feineman M. D., Ryerson F. J., DePaolo D. J., Plank T., "Zoisite-aqueous fluid trace element partitioning with implications for subduction zone fluid composition" Chemical Geology 239(3–4) (2007), 250-265. [DOI:10.1016/j.chemgeo.2007.01.008]
8. [8] Brunsmann A., Franz G., Erzinger J., "REE mobilization during small-scale high-pressure fluid–rock interactionand zoisite/fluid partitioning of La to Eu" Geochimica et Cosmochimica Acta 65(4) (2001), 559-570. [DOI:10.1016/S0016-7037(00)00544-5]
9. [9] Brunsmann A., Franz G., Erzinger J., Landwehr D., "Zoisite- and clinozoisite-segregations in metabasites (Tauern Window, Austria) as evidence for high-pressure fluid–rock interaction" Journal of Metamorphic Geology 18(1) (2000), 1-21. [DOI:10.1046/j.1525-1314.2000.00233.x]
10. [10] Zack T., Foley S.F., Rivers T., "Equilibrium and Disequilibrium Trace Element Partitioning in Hydrous Eclogites (Trescolmen, Central Alps)" Journal of Petrology 43(10) (2002), 1947-1974. [DOI:10.1093/petrology/43.10.1947]
11. [11] Alavi M., "Tectonics of Zagros Orogenic belt of Iran, new data and interpretation" Tectonophysics 229 (1994), 211-238. [DOI:10.1016/0040-1951(94)90030-2]
12. [12] Nabavi M.H., "An introduction to the geology of Iran" Geological survey of Iran (in Farsi) (1976).
13. [13] Stocklin J., "Structural history and tectonics of Iran, A review" AAPG Bulletin 52 (1968), 1229-1258.
14. [14] Berberian M., King G. C. P., "Towards a palegeography and tectonic evolution of Iran" Canadian Journal of Earth Sciences 18 (1981), 210-265. [DOI:10.1139/e81-019]
15. [15] Sabzehi M., Mohammadiha K., "Geological map of Gangejin (Serow), Scale 1:100000" Geological Survey of Iran (2003).
16. [16] Khodabandeh A.A., Soltanni G. A., Sartipi A. H., Emami M. H., "Geological map of Iran, 1:100,000 series sheet Salmas" Geological Survey of Iran, Tehran (2002).
17. [17] Haghipour A., Aghanabati A., "Explanatory text of the Serow quadrangle map, 1:250,000" Geological survey of Iran (1988).
18. [18] Moazzen M., "Protolith nature and tectonomagmatic features of amphibolites from The Qushchi area, West Azerbaijan, NW Iran" Bulletin of the Mineral Research and Exploration 149 (2014), 139-152. [DOI:10.19111/bmre.89886]
19. [19] Ahangari M., Moazzen M., "Mineralogy of amphibolites and epidote amphibolites from South of Salmas, NW of Iran; Constraining thermodynamic conditions of epidote amphibolite to amphibolite sub-facies transformation". Iranian Journal of Geology 5 (2011), 93-106.
20. [20] Ahangari M., Moazzen M., "Investigations on coexistence of zoisite- clinozoisite in metamorphic rocks; An example from Salmas epidote- amphibolites- NW of Iran (in Farsi with English abstract)" Iranian Journal of Crystallography and Mineralogy 22 (2014), 27-36.
21. [21] 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]
22. [22] Skublov S., Drugova G., "patterns of trace-element distribution in calcic amphiboles as a function of metamorphic grade," The Canadian Mineralogist 41 (2003), 383-392. [DOI:10.2113/gscanmin.41.2.383]
23. [23] Frei D., Liebscher A., Franz G., Dulski P., "Trace Element Geochemistry of Epidote Minerals" Reviews in Mineralogy and Geochemistry 56(1) (2004), 553-605. [DOI:10.2138/gsrmg.56.1.553]
24. [24] Rollinson H., "Using geochemical data: Evalution, presentation, interpretation: Longman (1993).
25. [25] Nagasawa H., "Partitioning of Eu and Sr between coexisting plagioclase and K-feldspar" Earth and Planetary Science Letters 13 (1971), 139-144. [DOI:10.1016/0012-821X(71)90116-6]
26. [26] Bau M., "Rare-earth element mobility during hydrothermal and metamorphic fluid-rock interaction and the significance of the oxidation state of europium" Chemical Geology 93 (1991), 219-230. [DOI:10.1016/0009-2541(91)90115-8]
27. [27] Frei D., Liebscher A., Wittenberg A., Shaw C.J., "Crystal chemical controls on rare earth element partitioning between epidote-group minerals and melts: an experimental and theoretical study" Contributions to Mineralogy and Petrology 146(2) (2003), 192-204. [DOI:10.1007/s00410-003-0493-7]
28. [28] Spiegel C., Siebel W., Frisch W., Berner Z., "Nd and Sr isotopic ratios and trace element geochemistry of epidote from the Swiss Molasse Basin as provenance indicators: implications for the reconstruction of the exhumation history of the Central Alps" Chemical Geology 189(3–4) (2002), 231-250. [DOI:10.1016/S0009-2541(02)00132-8]
29. [29] Stone W.E., Crocket J.H., Fleet M.E., "Light-rare earth element-rich minerals associated with platinum-group element mineralization in the Archean Boston Creek Flow, Ontario" Mineralogy and Petrology 51 (1994), 85-109. [DOI:10.1007/BF01164916]
30. [30] Vlach S.R.F., "Micro-structural and compositional variations of hydrothermal epidote-groupminerals from a peralkaline granite, Corupá Pluton, Graciosa Province, South Brazil, and their petrological implications" Annals of the Brazilian Academy of Sciences 84 (2012), 407-425. [DOI:10.1590/S0001-37652012005000024]
31. [31] Gieré R., Sorensen S.S., "Allanite and other REE-rich epidote-group minerals" Reviews in Mineralogy and Geochemistry 56 (2004), 431-493. [DOI:10.2138/gsrmg.56.1.431]
32. [32] Sorensen S.S., Grossman J.N., "Enrichment of trace elements in garnet amphibolites from a paleo-subduction zone: Catalina Schist, southern California" Geochimica et Cosmochimica Acta 53(12) (1989), 3155-3177. [DOI:10.1016/0016-7037(89)90096-3]
33. [33] Thöni M., Jagoutz E., "Some new aspects of dating eclogites in orogenic belts: Sm-Nd, Rb-Sr, and Pb-Pb isotopic results from the Austroalpine Saualpe and Koralpe type-locality (Carinthia/Styria, southeastern Austria)" Geochimica et Cosmochimica Acta 56(1) (1992), 347-368. [DOI:10.1016/0016-7037(92)90138-9]
34. [34] Poli S., Schmidt M.W., "The high-pressure stability of zoisite and phase relationships of zoisite-bearing assemblage". Contributions to Mineralogy and Petrology 130 (1998), 162-175. [DOI:10.1007/s004100050357]
35. [35] skublov S.G., "REE pattern of amphibole replacing garnet" Twelfth Goldschmidt Conference Abstract, (2002) A271.
36. [36] Cortesogno L., Gaggero L., Zanetti A., "Rare earth and trace elements in igneous and high-temperature metamorphic minerals of oceanic gabbros (MARK area, Mid-Atlantic Ridge)" Contributions to Mineralogy and Petrology, 139 (2000), 373-393. [DOI:10.1007/s004100000147]
37. [37] Najorka J., Gottschalk M., Franz G., Heinrich W., "Ca-Sr distribution among amphibole, clinopyroxene, and chloride-bearing solutions" American Mineralogist 84 (1999), 596-606. [DOI:10.2138/am-1999-0413]

Add your comments about this article : Your username or Email:

© 2018 All Rights Reserved | Iranian Journal of Crystallography and Mineralogy

Designed & Developed by : Yektaweb