40Ar/39Ar geochronology of supergene alunite-group minerals

被引:0
作者
Yang, Jing [1 ]
Zheng, De-Wen [1 ]
Wu, Ying [1 ]
机构
[1] State Key Laboratory of Earthquake Dynamics, Institute of Geology, China Earthquake Administration
来源
Dizhen Dizhi | 2013年 / 35卷 / 01期
关键词
!sup]40[!/sup]Ar/[!sup]39[!/sup]Ar dating; Alunite-group minerals; Paleoclimate;
D O I
10.3969/j.issn.0253-4967.2013.01.015
中图分类号
学科分类号
摘要
Recently the successful application of laser heating 40Ar/39Ar dating to supergene alunite-group minerals demonstrates the applicability of the method to dating minerals existing in the oxidation zones of sulfur rich ore deposits. Laser-heating 40Ar/39Ar method not only reduces the amount of samples, but also the system background level; In addition, 40Ar/39Ar step-heating dating method can test for the presence of hypogene contaminants, the excess/inherited Ar, and the multiple generations of supergene minerals. Although problems remain in isotopic dating of supergene alunite-group minerals, the systematic sampling and reasonable analysis process, combined with a variety of detection methods, can yield meaningful weathering ages, which will provide a new approach for the research on the timing of continental weathering, the formation of oxidization zones, and climatic desiccation of Northwest China.
引用
收藏
页码:177 / 187
页数:10
相关论文
共 43 条
  • [1] Han Z.-X., Luan L.-J., Wang C.-Y., Sinificance of oxidized zone mineral in Kanggu'er tage gold deposit, Journal of Xi'an University of Science and Technology, 24, 3, pp. 324-327, (2004)
  • [2] He W., Zheng D.-W., Li D.-M., Et al., K-Ar dating of jarosite in eastern Tianshan and its environmental significance, Seismology and Geology, 31, 3, pp. 415-423, (2009)
  • [3] Qin K.-Z., Ding K.-S., Xu Y.-X., Et al., Tremendous crystal-paracoquimbite and its polytype coquimbite found for the first time in Hongshan Hs-epithermal Cu-au deposit, Eastern Tianshan, NW China, and its signifance, Acta Petrologica Sinica, 24, 5, pp. 1112-1122, (2008)
  • [4] San J.-Z., Hui W.-D., Qin K.-Z., Et al., Geological characteristics of Tulargen magmatic Cu-ni-co deposit in eastern Xinjiang and its exploration direction, Mineral Deposits, 26, 3, pp. 307-316, (2007)
  • [5] Tu G.-Z., Li X.-L., Studies on the characteristic features of the oxidation zone of the sulphite deposites in arid to extremely arid regions: With special reference to observations obtained from five sulphide deposits in the Northwestern China, Acta Geologica Sinica, 43, 4, pp. 361-377, (1963)
  • [6] Song S.-H., The characteristics and ore-forming regularity of pyrite-type copper in Qilian Mountains, Acta Geologica Sinica, 35, 1, pp. 1-23, (1955)
  • [7] Wen C.-Q., Xu X.-H., Mao Y.-S., A study of ore-forming process of the Xiaorequanzi copper deposit, Xinjiang, J Mineral Petrol, 22, 3, pp. 29-32, (2002)
  • [8] Wu X.-J., Mineralizing geological features of Matoutan gold deposit in east Tianshan, Xinjiang Geology, 25, 3, pp. 267-273, (2006)
  • [9] Xu Y.-X., Qin K.-Z., Ding K.-S., Et al., Geochronology evidence of Mesozoic metallogenesis and Cenozoic oxidation at Hongshan HS-epithermal Cu-au deposit, Kalatage region, eastern Tianshan, and its tectonic and paleoclimatic signifance, Acta Petrologica Sinica, 24, 10, pp. 2371-2383, (2008)
  • [10] Alpers C.N., Brimhall G.H., Middle Miocene climatic change in the Atacama Desert, northern Chile: Evidence from supergene mineralization at La Escondida, Geological Society of America Bulletin, 100, pp. 1640-1656, (1988)