Geochemistry and genesis of sulphide ore deposits in Sharosh Village, Qandil Series, Kurdistan Region, NE Iraq
The low-grade base metal sulphide Cu–Zn–Pb and Fe mineralization of Qandil Series develop in shear zones that occur in formations of the north-western part of the Zagros Orogen. This sulphide mineralization occurs either as quartz vein type or disseminated type associated with metamorphic rocks (mar...
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| Veröffentlicht in: | Arabian journal of geosciences 2017-10, Vol.10 (19), p.1-19, Article 428 |
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| creator | Mirza, Tola A. Kalaitzidis, Stavros P. Mohammed, Sarkhel H. Rashid, Saman Gh Petrou, Xenia |
| description | The low-grade base metal sulphide Cu–Zn–Pb and Fe mineralization of Qandil Series develop in shear zones that occur in formations of the north-western part of the Zagros Orogen. This sulphide mineralization occurs either as quartz vein type or disseminated type associated with metamorphic rocks (marbles and phyllites). This study aims to characterize these sulphide-rich ores by means of their mineralogical and geochemical features, including also the features of the corresponded host formations and those of marbles (calcitic and dolomitic) and phyllites. Petrographical data indicate the presence of Cu, Zn, Pb and Fe sulphides in hydrothermal quartz (±calcite) veins of different generations. Geochemical data of surface samples indicate enrichment of Cu and Fe in shear zones with low concentrations in Zn and Pb. The REE data indicate that the genesis of these sulphide ores took place in a hydrothermal system and was generally attributed to high temperature (> 250 °C).The mineralization seems to be fault-controlled, which is favoured by the significant tectonic deformation of the area. |
| doi_str_mv | 10.1007/s12517-017-3210-y |
| format | Article |
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This sulphide mineralization occurs either as quartz vein type or disseminated type associated with metamorphic rocks (marbles and phyllites). This study aims to characterize these sulphide-rich ores by means of their mineralogical and geochemical features, including also the features of the corresponded host formations and those of marbles (calcitic and dolomitic) and phyllites. Petrographical data indicate the presence of Cu, Zn, Pb and Fe sulphides in hydrothermal quartz (±calcite) veins of different generations. Geochemical data of surface samples indicate enrichment of Cu and Fe in shear zones with low concentrations in Zn and Pb. 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The REE data indicate that the genesis of these sulphide ores took place in a hydrothermal system and was generally attributed to high temperature (> 250 °C).The mineralization seems to be fault-controlled, which is favoured by the significant tectonic deformation of the area.</description><subject>Base metal</subject><subject>Calcite</subject><subject>Copper</subject><subject>Data</subject><subject>Deformation</subject><subject>Earth and Environmental Science</subject><subject>Earth science</subject><subject>Earth Sciences</subject><subject>Geochemistry</subject><subject>Heavy metals</subject><subject>High temperature</subject><subject>Hydrothermal systems</subject><subject>Iron</subject><subject>Lead</subject><subject>Low concentrations</subject><subject>Magma</subject><subject>Metal sulfides</subject><subject>Metamorphic rocks</subject><subject>Mineral deposits</subject><subject>Mineralization</subject><subject>Minerals</subject><subject>Ores</subject><subject>Original Paper</subject><subject>Quartz</subject><subject>Shear</subject><subject>Sulfides</subject><subject>Sulphides</subject><subject>Zinc</subject><issn>1866-7511</issn><issn>1866-7538</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2017</creationdate><recordtype>article</recordtype><recordid>eNp1kL1OwzAURi0EEqXwAGyWWBvwTxI7I6qgVFQgKLBaTnKTuEqT1E6GvD2ughALg3U9fOe7ugeha0puKSHizlEWUREQ_zijJBhP0IzKOA5ExOXp75_Sc3Th3I6QWBIhZ6hZQZtVsDeutyPWTY5LaMAZh9sCu6HuKpMDbi3gHLrWmd5h0-BtpW3rKvxl6lqXsMBvnjQ13oI14Bb4ebC5b9QNfofStM0CvzzgtdWHS3RW6NrB1c-co8_Hh4_lU7B5Xa2X95tAc570AUspizXLSM7zmMU8ynhYpCTlRZQVLBEyD0MmGAmTpBC51jQtNAllKBIGUShTPkc3U29n28MArle7drCNX6loEkaSE0aFT9EplflrnIVCddbstR0VJeqoVU1aldeqjlrV6Bk2Mc5nmxLsn-Z_oW9Sqnqk</recordid><startdate>20171001</startdate><enddate>20171001</enddate><creator>Mirza, Tola A.</creator><creator>Kalaitzidis, Stavros P.</creator><creator>Mohammed, Sarkhel H.</creator><creator>Rashid, Saman Gh</creator><creator>Petrou, Xenia</creator><general>Springer Berlin Heidelberg</general><general>Springer Nature B.V</general><scope>AAYXX</scope><scope>CITATION</scope><scope>7UA</scope><scope>C1K</scope><scope>F1W</scope><scope>H96</scope><scope>L.G</scope></search><sort><creationdate>20171001</creationdate><title>Geochemistry and genesis of sulphide ore deposits in Sharosh Village, Qandil Series, Kurdistan Region, NE Iraq</title><author>Mirza, Tola A. ; 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This sulphide mineralization occurs either as quartz vein type or disseminated type associated with metamorphic rocks (marbles and phyllites). This study aims to characterize these sulphide-rich ores by means of their mineralogical and geochemical features, including also the features of the corresponded host formations and those of marbles (calcitic and dolomitic) and phyllites. Petrographical data indicate the presence of Cu, Zn, Pb and Fe sulphides in hydrothermal quartz (±calcite) veins of different generations. Geochemical data of surface samples indicate enrichment of Cu and Fe in shear zones with low concentrations in Zn and Pb. 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| subjects | Base metal Calcite Copper Data Deformation Earth and Environmental Science Earth science Earth Sciences Geochemistry Heavy metals High temperature Hydrothermal systems Iron Lead Low concentrations Magma Metal sulfides Metamorphic rocks Mineral deposits Mineralization Minerals Ores Original Paper Quartz Shear Sulfides Sulphides Zinc |
| title | Geochemistry and genesis of sulphide ore deposits in Sharosh Village, Qandil Series, Kurdistan Region, NE Iraq |
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