阵发性洪水条件下辫状河型冲积扇构型研究:以准噶尔盆地西北缘现代白杨河冲积扇为例*
纪友亮1,2, 张月1,2,3, 周勇1,2, 计璐璐1,2, 任红燕1,2, 郭姗姗1,2, 高晨曦1,2, 马铮涛1,2, 刘笑语1,2, 刘大卫1,2, 段小兵1,2, 桓芝俊1,2, 高崇龙1,2, 郭瑞婧1,2, 庞传梦1,2, 孙佳1,2, 杨栋吉1,2

Architecture of braided river alluvial fan under episodic flood conditions: a case study of modern Baiyang River alluvial fan in northwestern margin of Junggar Basin
JI Youliang1,2, ZHANG Yue1,2,3, ZHOU Yong1,2, JI Lulu1,2, REN Hongyan1,2, GUO Shanshan1,2, GAO Chenxi1,2, MA Zhengtao1,2, LIU Xiaoyu1,2, LIU Dawei1,2, DUAN Xiaobing1,2, HUAN Zhijun1,2, GAO Chonglong1,2, GUO Ruijing1,2, PANG Chuanmeng1,2, SUN Jia1,2, YANG Dongji1,2
准噶尔盆地西北缘白杨河冲积扇岩相/沉积物照片精选(据 张月等,2020 ; Zhang et al ., 2021 ) A—块状砾岩C1,点位11;B—片流砾岩C2,点位15;C—低角度交错层理砾岩C3,点位20;D—大型交错层理砾岩C4,点位52;E—簇状砾岩C5,点位64;F—平行层理砂岩S1,点位21;G—大型交错层理砂岩S2,点位54;H—风成交错层理砂岩S3,点位52;I—波纹层理砂岩S4,点位64;J—块状砂/泥岩S-M1,点位57