陇中盆地及周边地区主夷平面演化与高原隆升
马振华,彭廷江,李小苗,冯展涛,郭本泓,李孟,张军,宋春晖

Evolution of the main planation surfaces in the Longzhong Basin and its surrounding areas and its significance for the uplift of the Tibetan Plateau
Zhenhua MA,Tingjiang PENG,Xiaomiao LI,Zhantao FENG,Benhong GUO,Meng LI,Jun ZHANG,Chunhui SONG
图6 马衔山主夷平面(a)和达坂山主夷平面(b)上覆红黏土剖面岩性柱及磁性地层序列(黑色条带代表的正极性事件,白色条带代表的负极性事件)(据文献[1423]修改)
Fig.6 Lithology and magnetostratigraphy for the red clay borehole core on the Maxianshan main planation surface (a) and Dabanshan main planation surface (b) (Black represents the normal polarity and white represents the reversed polarity) (Modified from References [14,23])