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EPR 9°~10°N L喷口黑烟囱体形成环境重建:来自矿物学及铅-210年龄的限制

姚会强 周怀阳 彭晓彤 周新茂 董从芳 吴自军 李江涛

姚会强, 周怀阳, 彭晓彤, 周新茂, 董从芳, 吴自军, 李江涛. EPR 9°~10°N L喷口黑烟囱体形成环境重建:来自矿物学及铅-210年龄的限制[J]. 海洋学报, 2009, 31(5): 48-57.
引用本文: 姚会强, 周怀阳, 彭晓彤, 周新茂, 董从芳, 吴自军, 李江涛. EPR 9°~10°N L喷口黑烟囱体形成环境重建:来自矿物学及铅-210年龄的限制[J]. 海洋学报, 2009, 31(5): 48-57.
YAO Hui-qiang, ZHOU Huai-yang, PENG Xiao-tong, ZHOU Xin-mao, DONG Cong-fang, WU Zi-jun, LI Jiang-tao. Restructuring the formation conditions of black smoker chimney from L vent EPR 9°~10°N:constraints from mineralogy and lead-210 age[J]. Haiyang Xuebao, 2009, 31(5): 48-57.
Citation: YAO Hui-qiang, ZHOU Huai-yang, PENG Xiao-tong, ZHOU Xin-mao, DONG Cong-fang, WU Zi-jun, LI Jiang-tao. Restructuring the formation conditions of black smoker chimney from L vent EPR 9°~10°N:constraints from mineralogy and lead-210 age[J]. Haiyang Xuebao, 2009, 31(5): 48-57.

EPR 9°~10°N L喷口黑烟囱体形成环境重建:来自矿物学及铅-210年龄的限制

基金项目: 国家自然科学基金重点项目(40532011);国家自然科学基金(40403004;40473032)

Restructuring the formation conditions of black smoker chimney from L vent EPR 9°~10°N:constraints from mineralogy and lead-210 age

  • 摘要: 为了重建EPR 9°~10°N L喷口的形成环境,采用矿物学、地球化学及年代学的方法,对黑烟囱体的矿物组成、矿物结构、元素剖面分布以及黑烟囱体内外层铅-210测年进行了研究。矿物学观察表明,该喷口烟囱体内壁主要由方黄铜矿组成,而外壁则主要由硬石膏组成。铅-210测年结果表明,烟囱体形成于EPR 9°~10°N区域内1991年的火山喷发事件之后,并有较低的生长速率,约为0.3cm/a。结合该喷口及其附近A喷口已发表资料认为,该烟囱体开始生长是由于蒸气相流体引起的,其后期受到卤水相流体的影响,而且流体温度应不小于330℃。
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  • 收稿日期:  2009-02-22
  • 修回日期:  2009-04-28

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