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沉积环境中古盐度的恢复——以吐哈盆地西南缘水西沟群泥岩为例
Recovery Paleosalinity in Sedimentary Environment —An example of mudstone in Shuixigou group, southwestern margin of Turpan-Hami basin
【摘要】 用锶钡法、硼元素法、钾钠比值和沉积磷酸盐法推算了吐哈盆地西南缘水西沟群沉积古水介质环境。认为,在水西沟群沉积时期,古水介质总体为淡水环境[m(Sr)/m(Ba)<1、m(B)为12.30×10-6~64.20×10-6],且自八道湾组—西山窑组沉积时期古水介质逐渐变淡:八道湾组沉积时期,古水介质盐度平均为2.28‰;三工河组沉积时期,平均为2.23‰;西山窑组沉积时期,平均为2.07‰.此外,对恢复沉积环境古盐度的其他方法进行了讨论,并指出了各种方法的局限性。
【Abstract】 The paleoaqueous environment of Shuixigou group deposit in southwestern margin of Turpan-Hami basin is predicted by using Sr-Ba, B, K/Na and phosphate methods. The results show the fresh-water environment in the period of Shuixigou group with Sr/Ba ratio of less than 1 and B content ranging from 12.30ppm to 64.20ppm, and paleosalinity from 2.28‰ of J1b to 2.23‰ of J1x, averaging 2.07‰. Also, the other methods to recover paleosalinity in sedimentary environment are discussed and their limitations are presented in this paper.
【Key words】 paleosalinity; geochemistry; Turpan-Hami basin; sedimentary environment;
- 【文献出处】 新疆石油地质 ,Xinjiang Petroleum Geology , 编辑部邮箱 ,2005年06期
- 【分类号】P592;
- 【被引频次】65
- 【下载频次】763