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琼大村韧性变形带地质地球化学特征

Geological and geochemical characteristics of Dacun ductile deformable zone in Hainan Island

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【作者】 李孙雄谢盛周莫位明周进波

【Author】 LI Sun-xiong, XIE Sheng-zhou, MO Wei-ming, ZHOU Jin-bo (Hainan Institute of Geological Survey,Haikou 570226,China)

【机构】 海南省地质调查院海南省地质调查院 海南 海口 570206海南 海口 570206海南 海口 570206

【摘要】 大村韧性变形带主要由糜棱岩系列岩石组成,其强应变带和弱变形域分带明显。发育线理、面理、褶皱构造。变形差应力为34.1~62.2 MPa。微量元素地球化学特征表明Au,Ag,Pb,Zn和As等亲硫元素组合于构造带中贫化,Cu含量变化不明显,Sb,Sn和Bi等“中高温”元素则富集,反映了构造带大致形成于中高温环境,与矿物变形相分析一致。

【Abstract】 The Dacun ductile deformable zone consists mainly of mylonites with obvious zoning of strong and weak strain bands and widespread lineation,foliation,fold structure. The differential stress for deformation is 34. 1 - 62. 2 MPa. Trace-element geochemical characteristics indicate that sulphophile elements (Au, Ag,Pb,Zn, As) are depleted and mesothermal and hyperthermal elements (Sb,Sn,Bi) enriched in the structure zone, inflecting that the structure zone was formed in a mesothermal and hyperthermal environment,which is consistent with the deformation temperature of minerals.

  • 【文献出处】 华南地质与矿产 ,Geology and Mineral Resources of South China , 编辑部邮箱 ,2004年01期
  • 【分类号】P594
  • 【下载频次】46
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