Geochronology of the Yangchuling tungsten-molybdenum depoist in Duchang County, Jiangxi Province
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摘要:
江西省都昌县阳储岭钨钼矿床位于江南造山带东段，为准确厘定阳储岭钨钼矿床的成岩成矿时代，本次在详实的野外地质调查基础上，对阳储岭成矿花岗闪长斑进行锆石U-Pb定年工作，同时开展辉钼矿Re-Os同位素定年研究。LA-ICP-MS锆石U-Pb年龄为（145.08±0.35）Ma（MSWD=0.51，n=7）；辉钼矿Re-Os模式年龄为（143.3±2.0）Ma~（145.5±2.2）Ma，等时线年龄为（145.4±1.0）Ma。阳储岭成矿花岗闪长斑岩锆石U-Pb年龄与辉钼矿Re-Os等时线年龄基本一致，表明阳储岭钨钼矿床成岩成矿时代约为145 Ma。辉钼矿中Re含量为16.62×10-6~87.76×10-6，平均值为44.68×10-6，与壳幔混源岩浆热液矿床中Re的含量相似，指示阳储岭钨钼矿床成矿物质来源于壳幔混源。
Abstract:The Yangchuling tungsten-molybdenum deposit in Duchang County, Jiangxi Province, is located in the eastern part of the Jiangnan orogenic belt. In order to accurately define the diagenetic and mineralization ages of the Yangchuling W-Mo deposit, the authors carried out the zircon U -Pb dating of mineralization -associated granodiorite porphyry and Re -Os isotope dating of molybdenite in the Yangchuling deposit based on detailed field geological studies. The zircon LA-ICP-MS U-Pb age is (145.08±0.35)Ma (MSWD=0.03, n=22), the Re-Os model ages of molybdenite range from (143.3±2.0)Ma to (145.5±2.2)Ma, and the Re-Os isochron age is (145.4±1.0)Ma. The geochronological consistency between the ore-bearing porphyry and molybdenite indicates that the diagenesis and mineralization ages of the Yangchuling tungsten-molybdenum deposit are about 145 Ma. The ω(Re) values of molybdenite range from 16.62×10-6 to 87.76×10-6, averaging 44.68×10-6, similar to Re content in crust -mantle mixed source magmatic hydrothermal deposits, indicating that the ore-forming materials of the Yangchuling W-Mo deposit should have come from crust-mantle mixed source.
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Keywords:
- Yangchuling /
- zircon U-Pb /
- molybdenite Re-Os /
- tungsten-molybdenum deposit /
- Jiangxi
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致谢: 本文得到了中国地质科学院地球深部探测中心曹殿华的指导, 在此深表谢意。
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图 1 阳储岭钨钼矿区地质略图(江西省地质矿产勘查开发区, 2015)
1—花岗闪长岩; 2—花岗闪长斑岩; 3—二长花岗斑岩; 4—花岗斑岩; 5—爆破角砾岩; 6—矿体; 7—断层及编号/破碎带; 8—地质界线/蚀变界线; 9—角岩/角岩化板岩; 10—新元古界双桥山群; 11—花岗闪长斑岩采样位置及样品编号/辉钼矿采样位置及样品编号
Figure 1. Simplified geological map of the Yangchuling tungsten-molybdenum deposit (after Jiangxi Bureau of Geological and Mineral Exploration and Development, 2015)
1-Granodiorite; 2-Granodiorite porphyry; 3-Monzogranite porphyry; 4-Granite porphyry; 5- Blasting breccia; 6-Orebody; 7-Fault and number; 8-Geological boundary/alteration boundary; 9-Hornstone/ Hornfelsed slate; 10-Shuangqiaoshan Group of Neoproterozoic; 11- Sampling location and its number of granodiorite/sampling location and its number of molybdenite
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图 2 阳储岭矿区锆石U-Pb与辉钼矿Re-Os样品照片
a—含矿花岗闪长斑岩照片; b—花岗闪长斑岩镜下照片; c—花岗闪长斑岩内脉状辉钼矿; d—花岗闪长斑岩外接触带角岩内辉钼矿脉
Figure 2. Photographs of zircon U-Pb and molybdenite Re-Os samples in Yangchuling deposit
a-Photographs of ore-bearing granodiorite porphyry; b-Microscopic photos of granodiorite porphyry; c-Vein molybdenite in granodiorite porphyry; d-Molybdenite veins in hornstone at the outer contact zone of granodiorite porphyry
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图 3 阳储岭矿区黑云母花岗岩锆石阴极发光及测点位置图
Figure 3. Zircon cathodoluminescence photos of biotite granite in Yangchuling mining area and the position of measuring point
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图 4 阳储岭黑云母花岗岩LA-ICP-MS锆石U-Pb年龄谐和图
Figure 4. LA-ICP-MS zircon U-Pb Age concordia diagram of biotite granite in Yangchuling mining area
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图 5 阳储岭钨钼矿Re-Os加权平均年龄和等时线年龄
(a—等时线年龄; b—加权平均年龄)
Figure 5. Re-Os weighted average age and isochron age of Yangchuling tungsten-molybdenum deposit
(a-Isochrone age; b-Weighted average age)
表 1 阳储岭矿区LA-ICP-MS锆石U-Pb同位素测年
Table 1 LA-ICP-MS zircon U-Pb Isotope chronology of Yangchuling mining area
下载: 导出CSV
表 2 阳储岭钨钼矿床辉钼矿Re-Os同位素测试成果表
Table 2 Re-Os isotope results of molybdenite in Yangchuling tungsten-molybdenum deposit
下载: 导出CSV
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