The Zn-Pb sulfide and Pb-Zn-Ag non-sulfide Kuh-e-Surmeh ore deposit, Zagros Belt, Iran: Geologic, mineralogical, geochemical, and S isotopic constraints

[1]  H. Gilg,et al.  Nature and origin of the nonsulfide zinc deposits in the Sierra Mojada District, Coahuila, Mexico: constraints from regional geology, petrography, and isotope analyses , 2018, Mineralium Deposita.

[2]  Abdorrahman Rajabi,et al.  A review of major non-sulfide zinc deposits in Iran , 2018 .

[3]  M. Joachimski,et al.  New CO isotopic data on supergene minerals from the Skorpion and Rosh Pinah ore deposits (Namibia): Genetic and paleoclimatic constraints , 2017 .

[4]  M. Karimpour,et al.  Nakhlak carbonate-hosted Pb(Ag) deposit, Isfahan province, Iran: a geological, mineralogical, geochemical, fluid inclusion, and sulfur isotope study , 2017 .

[5]  A. Griera,et al.  Mineralogical and geochemical characterization of the Riópar non-sulfide Zn-(Fe-Pb) deposits (Prebetic Zone, SE Spain) , 2016 .

[6]  N. Cook,et al.  Partitioning of trace elements in co-crystallized sphalerite-galena-chalcopyrite hydrothermal ores , 2016 .

[7]  G. Markl,et al.  Redistribution of silver during supergene oxidation of argentiferous galena: A case study from the Schwarzwald, SW Germany , 2016 .

[8]  A. Somarin,et al.  Geological, geochemical, and fluid inclusion evidences for the origin of the Ravanj Pb?Ba?Ag deposit, north of Delijan city, Markazi Province, Iran , 2016 .

[9]  M. Bird,et al.  Mineralogy, Geochemistry and Stable Isotope Studies of the Dopolan Bauxite Deposit, Zagros Mountain, Iran , 2016 .

[10]  G. Simandl,et al.  Carbonate-Hosted Nonsulfide Pb-Zn Deposits of the Quesnel Lake District, British Columbia, Canada , 2016 .

[11]  S. Radosavljević,et al.  (Pb–Sb)-bearing sphalerite from the Čumavići polymetallic ore deposit, Podrinje Metallogenic District, East Bosnia and Herzegovina , 2016 .

[12]  M. Boni,et al.  The “Calamines” and the “Others”: The great family of supergene nonsulfide zinc ores , 2015 .

[13]  B. Taghipour,et al.  Geological and geochemical implications of the genesis of the Qolqoleh orogenic gold mineralisation, Kurdistan Province (Iran) , 2015 .

[14]  P. Alfonso,et al.  The early Cambrian Chahmir shale-hosted Zn–Pb deposit, Central Iran: an example of vent-proximal SEDEX mineralization , 2015, Mineralium Deposita.

[15]  I. Villa,et al.  The Yanque prospect (Peru): from polymetallic Zn-Pb mineralization to a nonsulfide deposit , 2014 .

[16]  M. Joachimski,et al.  The Jabali nonsulfide Zn–Pb–Ag deposit, western Yemen , 2014 .

[17]  Taghipour Batoul,et al.  ZN-PB MINERALIZATION AT THE KUH-E-SURMEH DEPOSIT FIRUZABAD, FARS PROVINCE: GEOCHEMICAL AND FLUID INCLUSION EVIDENCE , 2014 .

[18]  Yan Chen,et al.  Non-sulfide zinc deposits of the Moroccan High Atlas: Multi-scale characterization and origin , 2014 .

[19]  J. Ringenbach,et al.  STRUCTURAL STYLE AND KINEMATIC EVOLUTION OF THE HIGH ZAGROS, IRAN , 2013 .

[20]  M. Boni,et al.  The Hakkari nonsulfide Zn–Pb deposit in the context of other nonsulfide Zn–Pb deposits in the Tethyan Metallogenic Belt of Turkey , 2013 .

[21]  M. Tichomirowa,et al.  Oxygen and sulfur isotope investigations of the oxidation of sulfide mixtures containing pyrite, galena, and sphalerite , 2013 .

[22]  Abdorrahman Rajabi,et al.  Metallogeny of Permian–Triassic carbonate-hosted Zn–Pb and F deposits of Iran: A review for future mineral exploration , 2013 .

[23]  P. Alfonso,et al.  Geology, ore facies and sulphur isotopes of the Koushk vent-proximal sedimentary-exhalative deposit, Posht-e-Badam Block, Central Iran , 2012 .

[24]  P. Afzal,et al.  Delineation of mineralization zones using concentration–volume fractal method in Pb–Zn carbonate hosted deposits , 2012 .

[25]  B. Mayer,et al.  Oxygen and sulfur isotope systematics of sulfate produced during abiotic and bacterial oxidation of sphalerite and elemental sulfur , 2012 .

[26]  K. Knöller,et al.  Weathering of the black limestone of historical monuments (Ljubljana, Slovenia): Oxygen and sulfur isotope composition of sulfate salts , 2011 .

[27]  F. Mouthereau.  Timing of uplift in the Zagros belt/Iranian plateau and accommodation of late Cenozoic Arabia–Eurasia convergence , 2011, Geological Magazine.

[28]  N. Bellahsen,et al.  Fracture patterns in the Zagros Simply Folded Belt (Fars, Iran): constraints on early collisional tectonic history and role of basement faults , 2011, Geological Magazine.

[29]  M. Boni,et al.  In search of the lost zinc: A lesson from the Jabali (Yemen) nonsulfide zinc deposit , 2011 .

[30]  M. Tichomirowa,et al.  The isotopic composition of sulfate from anaerobic and low oxygen pyrite oxidation experiments with ferric iron — New insights into oxidation mechanisms , 2011 .

[31]  M. Böttcher,et al.  Experimental investigation of sulphur isotope partitioning during outgassing of hydrogen sulphide from diluted aqueous solutions and seawater , 2010, Isotopes in environmental and health studies.

[32]  F. Pirajno,et al.  The Magellan Pb deposit, Western Australia; a new category within the class of supergene non-sulphide mineral systems , 2010 .

[33]  W. Shanks,et al.  Laboratory chalcopyrite oxidation by Acidithiobacillus ferrooxidans: Oxygen and sulfur isotope fractionation , 2010 .

[34]  M. Lotfi,et al.  Emarat carbonate-hosted Zn–Pb deposit, Markazi Province, Iran: A geological, mineralogical and isotopic (S, Pb) study , 2010 .

[35]  J. callot,et al.  The eastern termination of the Zagros Fold‐and‐Thrust Belt, Iran: Structures, evolution, and relationships between salt plugs, folding, and faulting , 2009 .

[36]  Bernhardt Saini-Eidukat,et al.  Trace and minor elements in sphalerite: A LA-ICPMS study , 2009 .

[37]  O. Pokrovsky,et al.  Calcite, dolomite and magnesite dissolution kinetics in aqueous solutions at acid to circumneutral pH, 25 to 150 °C and 1 to 55 atm pCO2: New constraints on CO2 sequestration in sedimentary basins , 2009 .

[38]  H. Gilg,et al.  Nonsulfide zinc deposits in the Silesia–Cracow district, Southern Poland , 2009 .

[39]  L. Benedetti,et al.  Thick- and thin-skinned deformation rates in the central Zagros simple folded zone (Iran) indicated by displacement of geomorphic surfaces , 2009 .

[40]  G. Borg.  The Influence of Fault Structures on the Genesis of Supergene Zinc Deposits , 2009 .

[41]  E. Carranza,et al.  Karst bauxite deposits in the Zagros mountain belt, Iran , 2008 .

[42]  E. Heydari,et al.  Tectonics versus eustatic control on supersequences of the Zagros Mountains of Iran , 2008 .

[43]  J. Reichert,et al.  Numerical simulation and a geochemical model of supergene carbonate-hosted non-sulphide zinc deposits , 2008 .

[44]  M. Alavi.  Structures of the Zagros Fold-Thrust Belt in Iran , 2007, American Journal of Science.

[45]  M. Alavi,et al.  Structures of the Zagros fold-thrust belt in Iran , 2007, American Journal of Science.

[46]  N. Bellahsen,et al.  Tertiary sequence of deformation in a thin‐skinned/thick‐skinned collision belt: The Zagros Folded Belt (Fars, Iran) , 2007 .

[47]  B. Mayer,et al.  Oxygen and sulfur isotope systematics of sulfate produced by bacterial and abiotic oxidation of pyrite , 2007 .

[48]  W. G. Wright,et al.  Aqueous-Sulfate Stable Isotopes-A Study of Mining-Affected and Undisturbed Acidic Drainage , 2007 .

[49]  O. Lacombe,et al.  The Zagros folded belt (Fars, Iran): constraints from topography and critical wedge modelling , 2006 .

[50]  C. J. Talbot,et al.  A new tectonic scenario for the Sanandaj–Sirjan Zone (Iran) , 2006 .

[51]  S. Sherkati,et al.  Detachment folding in the Central and Eastern Zagros fold-belt (Iran): salt mobility, multiple detachments and late basement control , 2005 .

[52]  J. Spangenberg,et al.  Sulfur speciation and stable isotope trends of water-soluble sulfates in mine tailings profiles. , 2005, Environmental science & technology.

[53]  F. Khormali,et al.  Late Mesozoic−Cenozoic clay mineral successions of southern Iran and their palaeoclimatic implications , 2005, Clay Minerals.

[54]  Oleg S. Pokrovsky,et al.  Dissolution kinetics of calcite, dolomite and magnesite at 25 °C and 0 to 50 atm pCO2 , 2005 .

[55]  H. Rasa,et al.  FACIES, STABLE ISOTOPS, AND GENESIS OF KUH-E-SURMEHPB-ZN DEPOSIT (DALAN FORMATION) IN THE SOUTH OF FIROUZABAD, FARS PROVINCE , 2005 .

[56]  J. Rimstidt,et al.  Jarosite as an indicator of water-limited chemical weathering on Mars , 2004, Nature.

[57]  L. Yaozhong.  Laboratory study: simultaneous leaching silver-bearing low-grade manganese ore and sphalerite concentrate , 2004 .

[58]  N. McQuarrie,et al.  Crustal scale geometry of the Zagros fold–thrust belt, Iran , 2004 .

[59]  M. Alavi,et al.  Regional stratigraphy of the Zagros fold-thrust belt of Iran and its proforeland evolution , 2004 .

[60]  M. Hitzman,et al.  Classification, Genesis, and Exploration Guides for Nonsulfide Zinc Deposits , 2003 .

[61]  M. Boni,et al.  Nonsulfide Zinc Mineralization in Europe: An Overview , 2003 .

[62]  N. Reynolds,et al.  The Padaeng Supergene Nonsulfide Zinc Deposit, Mae Sod, Thailand , 2003 .

[63]  J. Brugger,et al.  Formation of Willemite in Hydrothermal Environments , 2003 .

[64]  C. Ayora,et al.  Oxidative dissolution of pyritic sludge from the Aznalcóllar mine (SW Spain) , 2002 .

[65]  K. Hessami,et al.  Progressive unconformities within an evolving foreland fold–thrust belt, Zagros Mountains , 2001, Journal of the Geological Society.

[66]  M. McBride,et al.  Cd, Cu, Pb, and Zn coprecipitates in Fe oxide formed at different pH: Aging effects on metal solubility and extractability by citrate , 2001, Environmental toxicology and chemistry.

[67]  G. Beaudoin.  ACICULAR SPHALERITE ENRICHED IN Ag, Sb, AND Cu EMBEDDED WITHIN COLOR-BANDED SPHALERITE FROM THE KOKANEE RANGE, BRITISH COLUMBIA, CANADA , 2000 .

[68]  F. Moore,et al.  The Kuh-e-Surmeh mineralization, a carbonate-hosted Zn-Pb deposit in the Simply Folded Belt of the Zagros Mountains, SW Iran , 2000 .

[69]  M. Bernroider,et al.  Colour, crystal chemistry, and mineral association of a green sphalerite from Steinperf, Dill Syncline, FRG , 1996 .

[70]  M. Berberian.  Master “blind” thrust faults hidden under the Zagros folds: active basement tectonics and surface morphotectonics , 1995 .

[71]  Robert H. McNutt,et al.  Genesis of sediment-hosted Zn-Pb-Ba deposits in the Irankuh District, Esfahan area, west-central Iran , 1994 .

[72]  O. Gallego,et al.  Conchostracos (Crustaceae-Conchostraca) paleozoicos de la Region de Antofagasta, norte de Chile , 1994 .

[73]  M. Alavi.  TECTONICS OF THE ZAGROS OROGENIC BELT OF IRAN - NEW DATA AND INTERPRETATIONS , 1994 .

[74]  J. Marcoux,et al.  Tethyan margins in space and time , 1991 .

[75]  N. Bortnikov,et al.  The nature of chalcopyrite inclusions in sphalerite; exsolution, coprecipitation, or "disease"? , 1991 .

[76]  Charles N. Alpers,et al.  Solubility of jarosite solid solutions precipitated from acid mine waters, Iron Mountain, California, U.S.A. Solubilité des solutions solides de jarosite précipitées à partir des eaux minières acides, Iron Mountain, Californie, U. S. A , 1989 .

[77]  F. Crundwell.  The influence of the electronic structure of solids on the anodic dissolution and leaching of semiconducting sulphide minerals , 1988 .

[78]  D. Sibley,et al.  Classification of dolomite rock textures , 1987 .

[79]  H. Barnes,et al.  Supergene processes in zinc-lead-silver sulfide ores in carbonates , 1983 .

[80]  M. Berberian,et al.  Towards a paleogeography and tectonic evolution of Iran: Reply , 1981 .

[81]  H. Sakai,et al.  The age curves of sulfur and oxygen isotopes in marine sulfate and their mutual interpretation , 1980 .

[82]  S. Colman-Sadd.  Fold Development in Zagros Simply Folded Belt, Southwest Iran , 1978 .

[83]  J. Stocklin.  Structural History and Tectonics of Iran: A Review , 1968 .

[84]  G. James,et al.  Stratigraphic Nomenclature of Iranian Oil Consortium Agreement Area , 1965 .

[85]  Taro Takahashi.  Supergene alteration of zinc and lead deposits in limestone , 1960 .