白杨河阶地揭示的北祁连山西段晚第四纪构造变形
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THE LATE QUATERNARY TECTONIC DEFORMATION REVEALED BY THE TERRACES ON THE BAIYANG RIVER IN THE NORTHERN QILIAN MOUNTAINS
LIU Rui1,2, LI An2, ZHANG Shi-min2, CHEN Zhi-dan3, GUO Chang-hui2
老君庙背斜地质简图及阶地变形特征 a 老君庙背斜地质简图; b 地质剖面A—A', 位置见图a; c 老君庙背斜区影像解译图, 白色虚线为背斜轮廓, 位置见图a;d 老君庙背斜区T5阶地变形特征, ▽ H 为水平缩短量, ▽ V 为垂直隆升量(长高比1︰10)