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成果统计

合作作者[TOP 5]

访问统计


  总访问量
 589

  访问来源
    内部: 3
    外部: 586
    国内: 416
    国外: 173

  年访问量
 123

  访问来源
    内部: 0
    外部: 123
    国内: 98
    国外: 25

  月访问量
 8

  访问来源
    内部: 0
    外部: 8
    国内: 7
    国外: 1

访问量

访问量

1. 94–9ka察尔汗盐湖的气候环境演化过程 [386]
2. 云南江城与老挝他曲含盐系地层孢粉分析及对比 [329]
3. 青海大浪滩凹地梁中矿区软钾镁矾沉积元素和相化学分析 [209]
4. 青海察尔汗盐湖碳酸盐的硼同位素地球化学特征 [205]
5. A late Eocene palynological record from the Nangqian Basin, Tibeta.. [198]
6. Assessing the impact of human activities on surface pollen assembl.. [195]
7. Boron occurrence in halite and boron isotope geochemistry of halit.. [187]
8. 瞬变电磁法解释煤矿地下含水构造研究——以内蒙古东明露天矿为例 [161]
9. 海陆相蒸发岩硫同位素值变化和地球化学应用 [146]
10. Palynological Assemblage Age and Palaeoenvironment of the Cretaceo.. [139]
11. Sr isotope and major ion compositional evidence for formation of Q.. [111]
12. 盐湖沉积改造与地下卤水成因——以库车盆地和渤海湾盆地为例 [104]
13. 新疆库车盆地富钾盐泉水化学特征与成钾显示 [101]
14. Evaluation of boron isotopes in halite as an indicator of the sali.. [99]
15. Hydrochemistry, Distribution and Formation of Lithium-Rich Brines .. [96]
16. The Source, Distribution, and Sedimentary Pattern of K-Rich Brines.. [96]
17. Aridification signatures from fossil pollen indicate a drying clim.. [95]
18. Origin of Underground Brine in Potassium-Bearing Strata in Khammou.. [93]
19. “凹口凸”钾盐成矿模式与找钾方法 [91]
20. 柴达木盆地中部高Mg/Li盐湖卤水富镁物源探讨 [88]
21. Using coprophilous fungi to reconstruct the history of pastoralism.. [88]
22. 氯化钙型卤水成因的研究进展及其科学问题 [88]
23. Influence of non-marine fluid inputs on potash deposits in northea.. [87]
24. 柴达木盆地那棱格勒河及其尾闾盐湖锂成矿物源:来自水化学和锶、硫同位.. [86]
25. Fungal spore indicators of vegetation and highland pastoralism in .. [84]
26. Origin and recharge model of the Late Cretaceous evaporites in the.. [82]
27. Modern Pollen Assemblages in Typical Agro-Pastoral Ecotone in the .. [82]
28. Origin and circulation of saline springs in the Kuqa Basin of the .. [69]
29. 青海囊谦盆地始新世石膏层沉积环境研究 [68]
30. 柴达木盆地水—岩硼含量分布特征及其富集区域物源讨论 [68]
31. A late Eocene palynological record from the Nangqian Basin, Tibeta.. [64]
32. Boron isotope geochemistry of a brine-carbonate system in the Qaid.. [55]