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南海北部琼东南盆地HQ-1PC沉积物孔隙水的地球化学特征及其对天然气水合物的指示意义
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  • 作者:杨涛 ; 蒋少涌 ; 葛璐 ; 杨競红 ; 吴能友 ; 张光学 ; 刘坚 ; 陈道华
  • 关键词:孔隙水 ; 地球化学 ; 天然气水合物 ; 琼东南
  • 中文刊名:JDXK
  • 英文刊名:Scientia Sinica(Terrae)
  • 机构:南京大学地球科学系内生金属矿床成矿机制研究国家重点实验室;南京大学海洋地球化学研究中心;中国科学院广州能源研究所;国土资源部广州海洋地质调查局;
  • 出版日期:2013-03-20
  • 出版单位:中国科学:地球科学
  • 年:2013
  • 期:v.43
  • 基金:国家重点基础研究发展计划(编号:2009CB219506);; 国家自然科学基金(批准号:40773029,40903002,40772073);; 教育部博士点基金(批准号:20090091120046)资助
  • 语种:中文;
  • 页:JDXK201303002
  • 页数:10
  • CN:03
  • ISSN:11-5842/P
  • 分类号:5-14
摘要
HQ-1PC站位位于琼东南盆地中部,对该站位沉积物孔隙水的地球化学分析发现其3~4m处有明显的盐度异常,说明该站位在沉积物浅表层有明显的高盐度流体加入.其他地球化学特征也显示在该深度有一亏损硫酸盐、富含碘的流体加入,这种流体特征与水合物形成时排放的高盐流体相似.在4m以下,HQ-1PC站位则表现出了明显的甲烷厌氧氧化特征,主要表现为浅的硫酸盐还原界限、高硫酸盐通量、高自生碳酸盐沉积等特征,同时在该深度以下碘也表现出了异常高的通量,暗示HQ-1PC站位所在区域具有高的有机质含量,微生物活动强烈,可为水合物的形成提供充足的气源.再结合明显的盐度异常特征,推测在该站位浅表层附近很有可能有天然气水合物生成,水合物在形成过程中排出的高盐流体及散逸出的甲烷气引起了一系列的地球化学异常现象.
        
引文
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