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机译:青藏高原东北部柴达木盆地更新世湖相沉积物中磁记录的环境意义
Department of Geosciences, University of Tubingen, Hb'lderlinstr. 12, 72074 Tubingen, Germany;
Department of Geosciences, University of Tubingen, Hb'lderlinstr. 12, 72074 Tubingen, Germany,Institute of Tibetan Plateau Research, Chinese Academy of Sciences, P.O. Box 2871, Beijing 100085, China;
Paleoenvironmental Dynamics Group, Institute of Geosciences, University of Frankfurt, Altenhoferallee 1, 60438 Frankfurt, Germany;
Department of Geosciences, University of Tubingen, Hb'lderlinstr. 12, 72074 Tubingen, Germany;
Institute of Tibetan Plateau Research, Chinese Academy of Sciences, P.O. Box 2871, Beijing 100085, China;
Paleoenvironmental Dynamics Group, Institute of Geosciences, University of Frankfurt, Altenhoferallee 1, 60438 Frankfurt, Germany;
机译:柴达木盆地西部(青藏高原东北部)后期上新世更新世湿度波动通过湖相沉积物的综合磁孢粉学记录揭示
机译:青藏高原东北部柴达木盆地西部更新世湖相沉积物的粘土矿物和同位素
机译:在柴达特盆地西部柴达丁盆地的连续全茂 - 第四纪湖沉积物记录中记录的岩散和晶粒尺寸记录
机译:西藏高原QAIDAM盆地砂汉盐湖的盐水和现代水循环贡献的起源
机译:在新生代藏高原藏边缘的构造与气候之间的相互作用:西藏高原和西北地区西北地区的案例研究促进了自新世纪以来中纬度亚洲