土耳其中东部Çöpler (İliç - Erzincan)斑岩型金矿流体包裹体显微温度及稳定同位素(O、H)特征

Oktay Canbaz, A. Gökce
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引用次数: 5

摘要

Çöpler金矿床赋存于Çöpler花岗岩类(Eosen)和周围克班变质岩(晚古生代—早中生代)和蒙祖尔灰岩(晚石炭世—早白垩世)变质岩的石英网中。在网状矿脉中伴生有少量黄铜矿、黄铁矿、磁铁矿、磁赤铁矿、赤铁矿、铁锌矿、菱锌矿、方铅矿、闪锌矿、镜面赤铁矿、针铁矿、绢云母、黄铁矿等原生金。此外,在矽卡岩带的细脉中还发现了绿帘石(开介石-黝帘石)、石榴石、橄榄石、绿泥石、透闪石/放光石、白云母和不透明矿物。石英脉状流体包裹体研究表明,热液流体中含有CaCl2、MgCl2和NaCl,两相(L+V)包裹体的盐度为1.7 ~ 20.6% NaCl当量。在含三相包裹体的岩盐中测定了高达44%的盐度值。它们的均一化温量值在145.0 ~ 380.0℃范围内,显示了变热/低温到低温的条件。Çöpler花岗岩类流体包裹体水的δ18O和δD值与原生岩浆水的δ18O和δD值相对应,而克班变质岩变质沉积层流体包裹体水的δ18O和δD值则落在原生岩浆外,处于变质水场内。蒙祖尔灰岩赋存的夕卡岩带石英脉样品的δD值特别低。结果表明,花岗岩类流体与克班变质岩和蒙祖尔灰岩的变质沉积物混合,形成了石英细脉,形成了网状矿石。鉴于这种情况,本研究领域所描述的特征和设想的过程可能适用于类似的情况。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Microthermometric and stable isotopic (O and H) characteristics of fluid inclusions in the porphyry related Çöpler (İliç - Erzincan) gold deposit, central eastern Turkey
The Çöpler gold deposit occurs within the stockwork of quartz hosted by the Çöpler granitoid (Eosen) and by surrounding metasediments of Keban metamorphic (Late Paleozoic - Early Mesozoic) and the Munzur limestones (Late Carboniferous - Early Cretaceous).Native gold accompanied by small amounts of chalcopyrite, pyrite, magnetite, maghemite, hematite, fahlerz, marcasite, bornite, galena, sphalerite, specular hematite, goethite, lepidochrosite and bravoitic pyrite within the stockwork ore veinlets. In addition, epidote (pistazite - zoisite), garnet, scapolite, chlorite, tremolite/actinolite, muscovite and opaque minerals were determined within the veinlets occurred in skarn zones.The study of fluid inclusions in quartz veinlets showed that the hydrothermal fluids contain CaCl2, MgCl2 and NaCl and the salinities of the two phases (L+V) inclusions range from 1.7 to 20.6% NaCl equivalent. Salinity values up to 44% were determined within the halite bearing three phases inclusions. Their homogenization temperature values have a wide range from 145.0 to 380.0°C, indicative of catathermal/hypothermal to epithermal conditions. The δ18O and δD values of the fluid inclusion waters from the Çöpler granitoid correspond to those assigned to Primary Magmatic Water, those from the metasediments of Keban metamorphics fall outside of the Primary Magmatic and are within the Metamorphic Water field. A sample from a quartz vein within the skarn zone hosted by the Munzur limestones has a particularly low δD value.The results suggest that fluids derived from the granitoids were mixed with those derived from the metasediments of Keban metamorphics and the the Munzur limestones and resulting in quartz veinlets in these lithologies and the formation of stockwork ores. In view of the occurrence, the features described and processes envisaged for this study area may be applicable in similar settings.
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Central European Journal of Geosciences
Central European Journal of Geosciences GEOSCIENCES, MULTIDISCIPLINARY-
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