تعیین مدل کانه‌زایی مگنتیت- اسپکیولاریت در کانسار آهن ده‌زمان، استان خراسان رضوی: کانی‌شناسی، ساخت و بافت و دگرسانی

[1] Nabatian Gh., Rastad E., Neubauer M., Honarmand M., Ghaderi M., “Iron and Fe-Mn mineralization in Iran: implication for Tethyan metallogeny”, Australian Jurnal of Earth Sciences 62 (2015) 211-241.

[2] Ghorbani M., “The economic geology of Iran, mineral deposits and natural resources”, Springer (2013) 569 p.

[3] Ramezani J., Tucker, R., “The saghand region, central Iran: U-Pb geochronology, prtrogenesis and implication for gondwana tectonics”, Amrican journal of science 303 (2003) 622-665.

[4] Daliran F., “The magnetite-apatite deposit of Mishdovan, East Central Iran. An alkali rhyolite hosted, ‘Kiruna type’ occurrence in the Infracambrian Bafg Metallotect (Mineralogic, Petro-graphic and geochemical study of the ores and the host rocks)”, Unpublished PhD thesis, University of Karlsruhe, Karlsruhe, Germany (1990) 248 p.

[5] Foster H., Jafarzadeh A., “The Bafq mining district in Central Iran—a highly mineralized Infracambrian volcanic field”, Economic Geology 89 (1994) 1697-1721.

[6] Daliran F., “Kiruna type iron oxide-apatite ores and apatities of the Bafq district, Iran, with an emphasis on the REE geochemistry of the their apatites”, in Porter, T. M. (eds.), Hydrothermal iron oxide copper gold and related deposits: a global perspective, PGC Publishing, Adelaide 2 (2002) 303-320.

[7] Moore F., Modabberi S., “Origin of choghart iron oxide deposit, Bafq mining district, central Iran: new isotopic and geochemical evidence”, Journal of Sciences, Islamic Republic of Iran 14 (2003) 259-269.

[8] Torab F.M., Lehmann B., “Magnetite-apatite deposits of the Bafq district, Central Iran: apatite geochemistry and monazite geochronology”, Mineral Magazine 71 (2006) 347–363.

[9] Jami M., Dunlop A. C., Cohen D. R., “Fluid inclusion and stabele isotope study of the Esfordi apatite-magnetite deposite, Central Iran”, Economic Geology 102 (2007) 1111-1128.

[10] Daliran F., Stosch H. -G., Williams P., “Multistage metasomatism and mineralization at hydrothermal Fe oxide-REE-apatite deposits and apatitites of the Bafq District, Central-East Iran”, in Andrew, C.J. et al. (eds), Digging deeper, Proceeding of the 9th Biennial SGA Meeting, Dublin (2007) 1501-1504.

[11] Daliran F., Stosch H. G., Williams P., “A review of the early Cambrian magmatic and metasomatic events and their bearing on the genesis of the Fe oxide-REE-apatite deposits (IOA) of the Bafq District, Iran”, In: Williams P. ed. Smart science for exploration and mining, Proceedings of the 10th Biennial of the SGA, Townsville, Qld, Australia (2009) 623-625.

[12] Daliran F., Stosch H. G., Williams P., “Lower Cambrian iron oxide–apatite-REE (U) deposits of the Bafq district, east- Central Iran”, in Corriveau, L. and Mumin, H. (eds.) Exploring for iron-oxide copper-gold deposits: Canada and global analogues. Published in partnership by Mineral Deposits Division, Geological Association of Canada and Geological Survey of Canada, Geol. Assoc. Can. short course notes, 20, Québec (2010) 143-155.

[13] Bonyadi Z., Davidson G. J., Mehrabi B., Meffre S., Ghazban, F., “Significance of apatite REE depletion and monazite inclusions in the brecciated Se-Chahun iron oxide–apatite deposit, Bafq district, Iran, insights from paragenesis and geochemistry”, Chemical Geology 281 (2011) 253–269.

[14] Nozaem R., Mohajjel M., Rossetti F., Della Seta M., Vignaroli G., Yassaghi A., Salvini S., Eliassi M., “Post-Neogene right-lateral strike–slip tectonics at the north-western edge of the Lut Block (Kuh-e-Sarhangi Fault), Central Iran”, Tectonophysics 589 (2013) 220–233.

[15] نوزعیم ر.، محجل م.، یساقی ع.، نصرآبادی م.، "تحلیل ساختاری و تعیین شرایط دگرشکلی پهنه برشی کوه سرهنگی در گرانیت ده زمان، شمال باختری بلوک لوت"، مجله بلورشناسی و کانی شناسی ایران، شماره1 (1393) 15-26.

[16] Momenzadeh M., Wauschkuhn A., “The Allahabad iron deposit and iron, lead, and turquoise occurrences in the Zeber-Kuh Sarhangi mountains SW Kashmar (NE Iran)”, In: Geodynamic project (geotraverse) in Iran (Ed. Almassi, A.) (1983) 185–204. Geological Survey of Iran, Tehran.

[17] ایمان‌پور ب.، کریم‌پور م.ح.، ملکزاده شفارودی الف.، بررسی کانه‌زایی و ژئوشیمی کانسار آهن ده‌زمان، (جنوب غرب بردسکن) و مقایسه آن با کانسارهای آهن نواری، مجله بلورشناسی و کانی شناسی ایران (1395) در حال چاپ.

[18] Rossetti F., Nozaem R., Lucci F., Vignaroli G., Gerdes A., Nasrabadi M., Theye T., “Tectonic setting and geochronology of the Cadomian magmatism in Central Iran, Kuh-e- Sarhangi region ( NW Lut Block”, Journal of Asian Earth Sciences 102 (2014) 24-44.

[19] سهندی م.ر، قاسمی م.ر، اختیارآبادی ی.، "نقشه زمین‌شناسی 1:100000 قاسم آباد"، سازمان زمین‌شناسی و اکتشافات معدنی کشور (1389).

[20] Horst Q., Rosiere C.A., Heinrich S., Brokmeier H.G., Janson E.M., “Microstructures, textures and deformation mechanisms in hematite”, Journal of Structural Geology 23(9) (2001) 1429–1440.

[21] Kontny A., Engelmann R., Grimmer J.C., Greiling R.O., Hirt A., “Magnetic fabric development in a highly anisotropic magnetite-bearing ductile shear zone (Seve Nappe Complex, Scandinavian Caledonides)”, International Journal of Earth Sciences 101(3) (2012) 671–692.

[22] Whitney D. L., Evans B. W., “Abbreviations for names of rock-forming minerals”, American Mineralogist 95 (2010) 185–187.

[23] Williams P., “Classifying IOCG deposies”, in Exploring for iron oxide copper-gold deposits: Canada and global analogues, (2008) 11-19.

[24] شعبانی س.، کریم‌پور م.ح.، ملکزاده شفارودی ا، "مطالعات کانی‌شناختی و ژئوشیمیایی در کانسار آهن دلکن، استان‌خراسان‌رضوی"، هشتمین همایش انجمن زمین‌شناسی اقتصادی ایران، دانشگاه زنجان.

[25] Frietsch R., “On the chemical composition of the ore breccia at Luoassavaara, northern Sweden”, Mineralium Deposita 17 (1982) 239-243.

[26] Lundbohm H., Backstrom H., “Geology of the Kirunavaara district”, Geologisks Foreningensi Stockholm Forhandlingar 20 (1989) 63-74.

[27] Hitzman M. W., Oreskes N., Einaudi M. T., “Geological characteristics and tectonic setting of Perotrozoic iron oxide (Cu-U-Au-LREE) deposits”, Precambrian Research 58 (1992) 241-287.

[28] Barton M. D., Johnson D. A., “An evaporitic source model for igneous-related Fe oxide (Cu-Au-U-REE) mineralization”, Geology 24 (1996) 259-262.

[29] Barton M. ., Johnson D. A., “Footprints of Fe oxide (-Cu-Au) system”, SEG 2004: Predictive Mineral Discovery under Cover. Center for Global Metallogeny, Spec. Pub. 33, University of Western Australia, (2004) 112-116.

[30] Gandhi S. S., Bell R. T., “Kiruna/Olympic Dam-type iron, copper, uranium, gold, silver”, in Geology of Canadian mineral deposit types (eds.) O.R. Eckstrand, W.D. Sinclair, and R.I. Thorpe”, Geological Survey of Canada, Geology of Canada, 8 (1996) 513- 522 (also Geological Survey of America, The geology of North America).

[31] Hitzman M. W., “Iron oxides Cu-Au Deposits: What, Where, When and Why”, In porter, T. M. (eds.), Hydrothermal Iron oxide copper-gold and related deposits: A Global perspective, Australian mineral foundation, Adelaide (2001) 9-25.

[32] Frietsch R., Perdahl J. A., “Rare earth elements in apatite and magnetite in Kiruna-type iron ores and some other iron ore types”, Ore Geology Reviews 9 (1995) 489-510.

[33] Yu J., Chen Y., Mao J., Pirajno F., Duan C., “Review of geology, alteration, and origin of iron oxide- apatite deposits in the Cretaceous Ninguw basin, lower Yangtze river valley, eastern china: implication for ore genesis and geodynamic setting”, Ore Geology Reviews 43 (2011) 170-181.

[34] Williams P.J., Barton M.D., Fontboté L., de Haller A., Mark G., Oliver N.H.S., Marschik R., “Iron-oxide-copper gold deposits: geology, space-time distribution, and possible modes of origin. Society of Economic Geologists”, Economic Geology 100th Anniversary Volume, Denver (2005) 371–405.

[35] Stocklin J., “Structural history and tectonics of Iran: A review”, American Association of Petrology and Geology Bulletin 52 (1968) 1229–1258.

[36] سامانی ب.، "سازند ساغند، یک واحد ریفتوژنیک پرکامبرین فوقانی در ایران مرکزی"، مجله علوم زمین، شماره6 (1371) 32-45.

[37] Hildebrand R. S., “Kiruna type deposits: their origin and relationship to intermediate subvolcanicplutons in the Great Bear magmatic zone, northwest Canada”, Economic Geology 81 (1986) 640-659.

[38] Ray G. E., Lefebure D. V., “A synopsis of iron oxide ± Cu ± Au ± P ± REE deposits of the Candelaria-Kiruna-Olympic Dan family”, Geological Fieldwork (2001) 267-272.

[39] Dupuis C., Beaudoin G., “Discriminant diagrams for iron oxide trace element finterprinting of mineral deposit types”, Mineralium Deposita 46 (2011) 319-335.