| 凡口铅锌矿床同位素地球化学证据 |
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| 引用本文：汪礼明,徐文忻,李蘅,彭省临.2005.凡口铅锌矿床同位素地球化学证据[J].地球学报,26(z1):164-167. |
| DOI：10.3975/cagsb.2005.s1.53 |
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| 中文摘要:对凡口铅锌矿床不同成矿阶段进行矿物包裹体温度、硫和铅同位素测定，获得成矿第Ⅰ阶段温度为300±50℃，第Ⅱ、Ⅲ阶段温度为250±50℃；并获得矿床硫化物的S同位素组成为2.1‰～26.5‰，具有δ34SPy＞δ34SSp＞δ34SGn；第Ⅰ阶段硫化物的硫同位素组成随赋存层位由老到新硫同位素有逐渐减小趋势；第Ⅱ阶段硫化物的δ34S为14.3‰～23.8‰；第Ⅲ阶段硫化物的δ34S为5.7％~15.7‰，具有从早阶段至晚阶段硫同位素组成变化范围从大至小的减小趋势。分析获得68件铅同位素数据，其中硫化物的206Pb/204Pb比值为18.023～18.847；207Pb/204Pb比值为15.700～15.820；208Pb/204Pb比值为38.056～39.796。灰岩全岩的206Pb/204Pb比值为18.230～18.860；207Pb/204Pb比值为15.640～16.000；208Pb/204Pb比值为38.714～39.960。辉绿岩的206Pb/204Pb比值为18.570～18.650；207Pb/204Pb比值为15.260～15.620；208Pb/204Pb比值为38.650～38.960。第Ⅰ阶段δ34OH2O为13.3‰~13.1‰，δD为－50.2‰～－61.5‰；第Ⅱ阶段δ18OH2O为－2.4‰～＋10.8‰，δD为－50.2‰～－63.2‰；第Ⅲ阶段δ18OH2O为－4.9‰～－14.3‰，δD为－59.0‰～－61.0‰。 |
| 中文关键词:硫同位素 铅同位素 氢氧同位素 铅锌矿床 凡口 |
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| Isotope Geochemica Evidence of the Fankou Lead and Zinc Deposit |
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| Abstract:The determination of mineral inclusions for their temperature,sulfur and lead isotopes at different ore-forming stages in the Fankou lead and zinc deposit shows that the temperature are 300±50℃ at the first stage and 250±50℃ at the second and third stages. The isotope compositions are 2.1‰～26.5‰ with δ34SPy＞δ34SSp＞δ34SGn；The isotope compositions of sulfides at the first stage tend to decrease from the older to younger strata.δ34S values are 14.3‰～23.8‰ for sulfides at Stage Ⅱ，and δ34S are 5.7％～15.7‰ for sulfides at Stage I with the tendency of varying in a decreasing range and becoming smaller in value.The lead isotope obtained from 68 samples are 18.023～18.847；207Pb/204Pb ratios are 15.700～15.820,and 208Pb/204Pb ratios are 38.056～39.796.206Pb/204Pb ratios of the whole rock of limestone are 18.230～18.860；207Pb/204Pb ratios are 15.640～16.000；208Pb/204Pb ratios are 38.714～39.760. 206Pb/204Pb ratios of diabase are 18.570～18.650,207Pb/204Pb ratios are 15.260～15.620；and 208Pb/204Pb ratios are 38.650～38.960.δ18OH2Ovalues of the first stage are 12.3‰～13.1‰，and δD are －50.2‰～－61.5‰；δ18OH2O of the second stage are －2.4‰～＋10.8‰，and δD are－50.2‰～－63.2‰；δ18OH2O of the third stage are -4.9‰～－14.3‰，δD are －59.0‰～－61.0‰。 |
| keywords:sulfur isotope lead isotope oxygen and hydrogen isotope lead and zinc deposit Fankou |
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