Beukes N J, Gutzmer J and Mukhopadhyay J. 2002. The geology and genesis of high-grade iron ore deposits, Iron Ore 2002. Australasian Institute of Mining and Metallurgy, Perth: 23？29.
[36]
Birkeland A, Ihlen P M and Bjorlykke A. 1993. The sources of metals in sulfide deposits in the Helgeland nappe complex, North-Central Norway: Pb isotope evidence. Economic Geology, 88(7): 1810？1829.
[37]
Ji S C. 2008. Deformation Mechanisms, Rheology, and Seismic Properties of Rocks. Beijing: Geological Publ?ishing House: 1？539.
[38]
Ji S C and Xia B. 2002. Rheology of Polyphase Earth Materials. Polytechnic International Press, Montreal (Canada): 1？260.
[39]
Ji S C and Zhao P L. 1994. Layered rheological structure of subducting oceanic lithosphere. Earth and Planetary Science Letters, 124(1-4): 75？94.
[40]
Jin Z M, Zhang J F, Green H W and Jin S Y. 2002. Rheological properties of deep subducted oceanic lithosphere and their geodynamic implications. Science in China (series D-Earth Sciences), 45(11): 969？977.
[41]
Karato S L and Wu P. 1993. Rheology of the upper？mantle: A synthesis. Science, 260(5109): 771？778.
[42]
Kaufman A J. 1996. Geochemical and mineralogic effects of contact metamorphism on banded iron-formation: An example from the Transvaal Basin, South Africa. Precambrian Research, 79: 171？194.
[43]
Khan R M K and Naqvi S M. 1996. Geology, geochemistry and genesis of BIF of Kushtagi schist belt, Archaean Dharwar Craton, India. Mineralium Deposita, 31: 123？133.
[44]
Kirby S H. 1983. Rheology of the lithosphere. Reviews of Geophysics, 21(6): 1458？1487.
[45]
Powell C M, Oliver N H S, Li Z X, Martin D M and Ronaszecki J. 1999. Synorogenic hydrothermal origin for giant Hamersley iron oxide ore bodies. Geology, 27: 175？178.
[46]
Ramsay J G. 1967. Folding and fracturing of rocks. New York: McGraw-Hill: 1？568.
[47]
Ranalii G. 1997. Rheology of the lithosphere in space and time // Orogeny through time. Geological Society Special Publications, 121: 19？37.
[48]
Ranalli G and Murphy D C. 1987. Rheological stratification of the lithosphere. Tectonophysics, 132(4): 281？295.
[49]
Rasmussen B, Fletcher I R, Muhling J R, Thorne W S and Broadbent G C. 2007. Prolonged history of episodic fluid flow in giant hematite ore bodies: Evidence from in situ U？Pb geochronology of hydrothermal xenotime. Earth and Planetary Science Letters, 258(1？2): 249？259.
[50]
Rickard D T, Willdén M Y, Marinder N-E and Donnelly T H. 1979. Studies on the Genesis of the Laisvall Sandstone Lead-Zinc Deposit, Sweden. Economic Geology, 74(5): 1255？1285.
[51]
Storti F, Holdsworth R E and Salvini F. 2003. Intraplate strike-slip deformation belts // Storti F, Holdsworth R E and Salvini F. Intraplate strike-slip deformation belts. Geological Society Special Publications: 210: 1？14.
[52]
Sun H, Wu J, Yu P and Li J. 1998. Geology, geochemistry and sulfur isotope composition of the Late Proterozoic Jingtieshan (Superior-type) hematite-jasper-barite iron ore deposits associated with stratabound Cu mineral?ization in the Gansu Province, China. Minera?lium Dep?osita, 34(1): 102？112.
[53]
Sundblad K and Stephens M B. 1983. Lead isotope system?atics of strata-bound sulfide deposits in the Higher Nappe Complexes of the Swedish Caledonides. Econo?mic Geology, 78(6): 1090？1107.
[54]
Taylor D, Dalstra H J, Harding A E, Broadbent G C and Barley M E. 2001. Genesis of high-grade hematite ore bodies of the Hamersley province, Western Australia. Economic Geology, 96(4): 837？873.
[55]
Travé A, Calvet F, Sans M, Vergé J and Thirlwall M. 2000. Fluid history related to the Alpine compression at the margin of the south-Pyrenean Foreland basin: the El Guix anticline. Tectonophysics, 321(1): 73？102.
[56]
Venera Z, Schulmann K and Kroener A. 2000. Intrusion within a transtensional tectonic domain, the Cista Granodiorite (Bohemian Massif): Structure and rheological modeling. Journal of Strucrural Geology, 2(10): 1437？1454.
[57]
Zhang Z C, Hou T, Santosh M, Li H M, Li J W, Zhang Z H, Song X Y and Wang M. 2014. Spatio-temporal distrib?ution and tectonic settings of the major iron deposits in China: An overview. Ore Geology Reviews, 57: 247？263.
[58]
Zhong Z Q and You Z D. 1995. Compositional variation and volume loss of a shear zone-Hetai shear zone as a case history. Chinese Science Bulletin, 40(19): 1638？1641.
Barley M E, Pickard A L, Hagemmann S G and Folkert S L. 1999. Hydrothermal origin for the 2 billion year old Mount Tom Price giant iron ore deposit, Hamersley Province, Western Australia. Mineralium Deposita, 34(8): 784？789.
[100]
Bellot J P. 2007. Extensional deformation assisted by mineralised fluids within the brittle-ductile transition: Insights from the southwestern Massif Central, France. Journal of Structural Geology, 29(2): 225？240.
[101]
Belykh V I, Dunai E I and Lugovaya I P. 2007. Physicochemical formation conditions of banded iron formations and high-grade iron ores in the region of the Kursk magnetic anomaly: Evidence from isotopic data. Geology of Ore Deposits, 49 (2): 147？159.
[102]
Bozkurt E and Park R G. 1997. Microstructures of deformed grains in the Augen gneisses of southem Menderes Massif (western Turkey) and their tectonic significance. Geologische Rundschau, 86(1): 103？119．
[103]
Brown M C, Oliver N H S and Dickens G R. 2004. Veins and hydrothermal fluid flow in the Mt. Whaleback Iron Ore District, eastern Hamersley Province, Western Australia. Precambrian Research, 128(3-4): 441？474.
[104]
Burov E B and Watts A B. 2006. The long-term strength of continental lithosphere: “jelly sandwich” or “crème br?lée”? GSA Today, 16 (1): 4？10.
[105]
Cameron E M. 1989. Derivation of gold by oxidative metamorphism of a deep ductile shear zone: Part 1. Conceptual model. Journal of Geochemical Explor?ation, 31(2): 135？147.
[106]
Campana B. 1966. Stratigraphic-structural-paleoclimatic co?nt?r?ols of the newly discovered iron ore deposits of West?ern Australia. Mineralium Deposita, 1: 53？59.
[107]
Chauvet A, Onézime J, Charvet J, Barbanson L and Faure M. 2004. Syn- to late-tectonic stockwork emplacement within the Spanish section of the Iberian pyrite belt: Structural, textural, and mineralogical constraints in the Tharsis and Lazarza areas. Economic Geology, 99(8): 1781？1792.
[108]
Coppola V, Boni M, Gilg H A, Balassone G and Dejonghe L. 2008. The “calamine” nonsulfide Zn-Pb deposits of Belgium: Petrographical, mineralogical and geochem?ical characterization. Ore Geology Reviews, 33(2): 187？210.
[109]
Corti G, Ranalli G, Mulugeta G, Agostini A, Sani F and Zugu A. 2010. Control of the rheological structure of the lithosphere on the inward migration of tectonic activity during continental rifting. Tectonophysics, 490: 165？172.
[110]
Craw D. 2000. Fluid flow at fault intersections in an active oblique collision zone, Southern Alps, New Zealand. Journal of Geochemical Exploration, 69: 523？526
[111]
Craw D, Koons P O, Horton T and Chamberlain C P. 2002. Tectonically driven fluid flow and gold mineralization in active collisional orogenic belts: Comparison betw?een New Zealand and western Himalaya. Tecton?op?hysics, 348(1？3): 135？153.
[112]
Dalstra H J and Guedes S. 2004. Giant hydrothermal hematite deposits with Mg-Fe metasomatism: A comparison of the Carajas, Hamersley, and other iron ores. Economic Geology, 99(8): 1793？1800.
[113]
Dalstra H J and Rosière C A. 2008. Structural controls on high-grade iron ores hosted by banded iron formation: A global perspective. Reviews in Economic Geology, 15: 73?106.
[114]
Fan Z G, Huang X Z, Tan L, Yang X, Zhang H R, Zhou D Q, Liu Q K and Cao B B. 2014. A study of iron deposits in the Anshan area, China based on interactive inversion technique of gravity and magnetic anomalies. Ore Geology Reviews, 57: 618？627.
[115]
Fox J S, Farquhar R, Rui I and Cook N. 1988. Genesis of basalt-hosted massive sulphide deposits from the Trondheim and Sulitjelma districts, Norway: Ore lead isotopic considerations. Mineralium Deposita, 23(4): 276？285.
[116]
France-Lanord C, Derry L and Galy A. 1998. Continental erosion and CO (sub 2) uptake inferences from the Himalayan system. Mineralogical Magazine, 62(1): 466？467.
[117]
Fyfe W S. 1992. Metamorphic fluids. Earth Science Review, 32(1-2): 1？146.
[118]
Fyfe W S and Kerrich R. 1985. Fluids and thrusting. Chemical Geology, 49(1-3): 353？362.
[119]
Ghisetti F, Kirschner D and Vezzani L. 2000. Tectonic controls on large-scale fluid circulation in the Apennines (Italy). Journal of Geochemical Exploration, 69: 533？537.
[120]
Ghosh G and Mukhopadhyay J. 2007. Reappraisal of the structure of the Western Iron Ore Group, Singhbhum craton, eastern India: Implications for the exploration of BIF-hosted iron ore deposits. Gondwana Research, 12(4): 525？532.
[121]
Goldfarb R J, Groves D I and Gardoll S. 2001. Orogenic gold and geologic time: A global synthesis. Ore Geo?logy Reviews, 18(1-2): 1？75.
[122]
Gómez-Fernández F, Both R A, Mangas J and Arribas A. 2000. Metallogenesis of Zn-Pb carbonate？hosted mineralization in the southeastern region of the Picos de Europa (Central Northern Spain) Province: Geologic, fluid inclusion, and stable isotope studies. Economic Geology, 95(1): 19？39.
[123]
Gross G A. 1980. A classification of iron formations based on depositional environments. Canadian Mineralogist, 18: 215？222.
[124]
Groves D I. 1993. The crustal continuum model for late-Archaean lode-gold deposits of the Yilgarn Block, Western Australia. Mineralium Deposita, 28(6): 366？374.
[125]
Groves D I, Goldfarb R J, Gebre-Mariam M, Hagemann S G and Robert F. 1998. Orogenic gold deposits: A proposed classification in the context of their crustal distribution and relationship to other gold deposit types. Ore Geology Reviews, 13(1-5): 7？27.
[126]
Harker A. 1932. Study on metamorphism-rock transform?ation. Translated by Jiang Y C. 1981. Beijing: Geolog?ical Publishing House: 1？373.
[127]
He L Q, Song Y C, Chen K X, Hou Z Q, Yu F M, Yang Z S, Wei J Q, Li Z and Liu Y C. 2009. Thrust-controlled, sediment-hosted, Himalayan Zn-Pb-Cu-Ag deposits in the Lanping foreland fold belt, eastern margin of Tibetan Plateau. Ore Geology Reviews, 36(1-3): 106？132.
[128]
Hippertt J and Davis B. 2000. Dome emplacement and formation of kilometre-scale synclines in a granite？ greenstone terrain (Quadrilátero Ferrífero, southeastern Brazil). Precambrian Research, 102(1-2): 99？121.
[129]
Hitzman M W, Oreskes N and Einaudi M T. 1992. Geological characteristics and tectonic setting of Proterozoic iron oxide (Cu-U-Au-REE) deposits. Precambrian Research, 58(1-4): 241？287.
[130]
Hou Z Q and Cook N J. 2009. Metallogenesis of the Tibetan collisional orogen: A review and introduction to the special issue. Ore Geology Reviews, 36(1-3): 2？24.
[131]
James H L. 1983. Distribution of banded iron-formation in space and time // Trendall A F and Morris R C. Banded Iron-Formation: Facts and Problems. Amste?rdam: Elsevier: 471？490.
[132]
Klein C. 2005. Some Precambrian banded iron-formations (BIFs) from around the world: Their age, geological setting, mineralogy, metamorphism, geochemistry, and origin. American Mineralogist, 90: 1473？1499.
[133]
Koons P O, Craw D, Cox S C, Upton P, Templeton A S and Chamberlain C P. 1998. Fluid flow during active oblique convergence: A Southern Alps model from mechanical and geochemical observations. Geology, 26(2): 159？162.
[134]
Lagoeiro L E. 1998. Transformation of magnetite to hematite and its influence on the dissolution of iron oxide minerals. Journal of Metamorphic Geology, 16(3): 415？423.
[135]
Lascelles D F. 2006. The genesis of the Hope Downs iron ore deposit, Hamersley Province, Western Australia. Economic Geology, 101(7): 1359？1376.
[136]
Lawley C, Imber J and Selby D. 2013. Structural controls on orogenic Au mineralization during transpression: Lupa goldfield, Southwestern Tanzania. Economic Geology, 108(7): 1615？1640.
[137]
Leach D L and Sangster D F. 1993. Mississippi Valley-type lead zinc deposits. Geological Association of Canada Special Paper, 40: 289？314.
[138]
Li H M, Zhang Z J, Li L X, Zhang Z C, Chen J and Yao T. 2014. Types and general characteristics of the BIF？related iron deposits in China. Ore Geology Reviews, 57: 264？287.
[139]
Lister G S and Davis G A. 1989. The origin of metamorphic core complexes and detachment fault formed during Tertiary continental extension in the north Colorado River region, U. S. A. Journal of Structural Geology, 11(1？2): 65？94.
[140]
McCuaig T C and Kerrich R. 1998. P-T-t deformation-fluid characteristics of lode gold deposits: Evidence from alteration systematics. Ore Geology Review, 12(6): 381？453.
[141]
Molnar P. 1988. Continental tectonics in the aftermath of plate tectonics. Nature, 335(6186): 131？137.
[142]
Morris R C. 2002. Iron ore genesis and post？ore metasomatism at Mount Tom Price // Proceedings of the Iron Ore 2002 conference, Perth, 2002, Australasian Institute of Mining and Metallurgy: 3？13.
[143]
Nabelek P I, Liu M and Sirbescu M-L. 2001. Thermo-rheo logical, shear heating model for leucogranite generation, metamorphism, and deformation during the Proterozoic Trans-Hudson orogeny, Bloack Hills, South Dakota. Tectonophysics, 342(3？4): 371？388.
[144]
Paradis S, Chi G X and Lavoie D. 2004. Fluid inclusion and isotope evidence for the origin of the Upton Ba-Zn-Pb deposit, Quebec Appalachians, Canada. Economic Geology, 99(4): 807？817.
[145]
Porter T M. 2002. Hydrothermal iron oxide copper-gold & related deposits: A global perspective. Geoconsulting Publishing, Linden Park: 1？377.
[146]
Robl J, Fritz H, Stüwe K and Bernhard F. 2004. Cyclic fluid infiltration in structurally controlled Ag？Pb？Cu occurrences (Schladming, Eastern Alps). Chemical Geology, 205(1-2): 17？36.
[147]
Rosière C A and Rios F J. 2004. The origin of hematite in high-grade iron ores based based on infrared micro?scopy and fluid inclusion studies: The example of the conceicao mine, Quadrilatero Ferrifero, Brazil. Econo?mic Geology, 99(3): 611？624.
[148]
Rosière C A, Siemes H, Quade H, Brokmeier H G and Jansen E M. 2001. Microstructures, textures and deformation mechanisms in hematite. Journal of Structural Geology, 23: 1429？1440.
[149]
Schofield D I and D, Lemos R S. 1998. Relationships between syntectonic granite fabrics and regional PTtd paths: An example from the Gande-Avalon boundary of NE Newfoundland. Journal of Structural Geology, 20(4): 459？471.
[150]
Shimada M. 1993. Lithosphere strength inferred from fracture strength of rocks at high confining pressures and temperatures. Tectonophysics, 217(1？2): 55？64.
[151]
Sibson R H and Scott J. 1998. Stress-fault controls on the containment and release of overpressured fluids: Examples from gold-quartz vein systems in Juneau, Alaska; Victoria, Australia and Otago, New Zealand. Ore Geology Reviews, 13(1？5): 293？306.
[152]
Siemes H, Klingenberg B, Rybacki E, Naumann A, Sch?fer W, Jansen E and Kunze K. 2008. Glide systems of hematite single crystals in deformation experiments. Ore Geology Reviews, 33(3？4): 255？279.
[153]
Siemes H, Klingenberg B, Rybacki E, Naumann M, Schafer W, Jansen E and RosièreC A. 2003. Texture, microstru?cture, and strength of hematite ores experimentally deformed in the temperature range 600-1100°C and at strain rates between 10?4 and 10?6 s?1. Journal of Struct?ural Geology, 25(9): 1371？1391.
[154]
Sillitoe R H. 2003. Iron oxide-copper-gold deposits: An Andean view. Mineralium Deposita, 38(7): 787？812.
[155]
Spangenberg J E and Herlec U. 2006. Hydrocarbon biomarkers in the Topla-Me?ica zinc-lead deposits, Northern Karavanke/Drau Range, Slovenia: Paleoen?vironment at the site of ore formation. Economic Geology, 101(5): 997？1021.
[156]
Spencer J E and Welty J W. 1986. Possible controls of base-and precious-metal mineralization associated with Terriary detachment faults in the lower Colorado River Trough, Arizona and California. Geology, 14(3): 195？198.
[157]
Spier C A, de Oliveira Sonia M B and Rosière C A. 2003. Geology and geochemistry of the ?guas Claras Quadrilátero Ferrífero, Minas Gerais, Brazil. Miner?alium Deposita, 38(6): 751？774.
[158]
Spier C A, de Oliviera Sonia M B, Sial A N and Rios F J. 2007. Geochemistry and genesis of the banded iron formations of the Cauê Formation, Quadrilátero Ferrífero, Minas Gerais, Brazil. Precambrian Research, 152(3？4): 170？206.
[159]
Spry P G, Plimer I R and Teale G S. 2008. Did the giant Broken Hill (Australia) Zn-Pb-Ag deposit melt? Ore Geology Reviews, 34(3): 223？241.
[160]
Wang E D, Xia J M, Fu J F, Jia S S and Men Y K. 2014. Formation mechanism of Gongchangling high-grade magnetite deposit hosted in Archean BIF, Anshan- Benxi area, Northeastern China. Ore Geology Reviews, 57: 306？321.
[161]
Williams P J. 2010. Classifying IOCG deposits // Corriveau L and Mumin H. Exploring for iron-oxide copper-gold deposits: Canada and global analogues. Geological Association of Canada Short Course Notes, 20: 11？19.
[162]
Xu D R, Wang Z L, Cai J X, Wu C J, Bakun-Czubarow N, Wang L, Chen H Y, Baker M J and Kusiak M A. 2013. Geological characteristics and metallogenesis of the Shilu Fe-ore deposit in Hainan Province, South China. Ore Geology Reviews, 53: 318？342.
[163]
Xu D R, Wang Z L, Chen H Y, Hollings P, Jansen N H, Zhang Z C and Wu C J. 2014 Petrography and geochemistry of the Shilu Fe-Co-Cu ore district, South China: Implications for the origin of a Neoproterozoic BIF system. Ore Geology Reviews, 57: 322？350.
[164]
Xu G and Lin X. 2000. Geology and geochemistry of the Changlongshan skarn iron deposit, Anhui Province, China. Ore Geology Reviews, 16(1？2): 91？106.
[165]
Zhai M G and Windley B F. 1990. The Archaean and early Proterozoic banded iron formations of North China: Their characteristics, geotectonic relations, chemistry and implications for crustal growth. Precambrian Research, 48: 267？286.
