青藏高原东缘湖相沉积和黄土高原黄土沉积磁化率与粒度相关性对比*
时伟1,2, 蒋汉朝1

Comparison of correlation between magnetic susceptibility and grain size for lacustrine sediments in eastern Tibetan Plateau and loess deposits in Chinese Loess Plateau
Shi Wei1,2, Jiang Han-Chao1
青藏高原东缘2个湖相沉积剖面和蓝田剖面岩性柱 A—岷江上游流域地质简图(据 Zhang et al ., 2006 );B—新磨村湖相沉积剖面;C—理县湖相沉积剖面;D—蓝田黄土剖面B和C中的白框与数字代表样品位置与采样深度