...
首页> 外文期刊>Current Science: A Fortnightly Journal of Research >Sulphur isotopic study on barite mineralization of the Tons valley, Lesser Himalaya, India: Implication for source and formation process
【24h】

Sulphur isotopic study on barite mineralization of the Tons valley, Lesser Himalaya, India: Implication for source and formation process

机译:印度小喜马拉雅山Tons山谷重晶石矿化的硫同位素研究:对来源和形成过程的影响

获取原文
获取原文并翻译 | 示例
           

摘要

Sulphur isotopic study on barite (BaSO_4) mineralization, located about 65 km NW of Dehra Dun in the Tons valley, Lesser Himalaya, has shown that d d 34 S values of barite vary from +26.5 to +29.5‰. The data, coupled with earlier published abnormallyhigh value of 87 Sr/86 Sr in barite (0.720448 to 0.728637), have demonstra-ted that sulphur was derived from Proterozoic sea water and Ba was obtained from the radiogenic crustal source. These isotopic signatures suggest mixing of sea water sulphate with Ba-carrying crustal fluid for barite formation, with its initial deposition linked to diagene-sis of the host rocks.
机译:位于小喜马拉雅山通斯谷德赫拉敦西北约65公里处的重晶石(BaSO_4)矿化的硫同位素研究表明,重晶石的d d 34 S值在+26.5至+ 29.5‰之间变化。该数据,再加上较早发表的重晶石中异常高的87 Sr / 86 Sr值(0.720448至0.728637),证明了硫来自元古代海水,而Ba则来自放射地壳来源。这些同位素特征表明,将海水硫酸盐与携带Ba的地壳流体混合以形成重晶石,其初始沉积与基质岩的成岩作用有关。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号