碎屑岩沉积构型研究若干进展*
吴胜和1, 岳大力1, 冯文杰2, 张佳佳1, 徐振华1

Research progress of depositional architecture of clastic systems
Wu Sheng-He1, Yue Da-Li1, Feng Wen-Jie2, Zhang Jia-Jia1, Xu Zhen-Hua1
典型的曲流河点坝平面演变模式(据 Ghinassi and Ielpi,2015 ) A—邻近意大利Imola的Santerno河(44°20'45.16″N, 11°43'17.32″E);B—侧向迁移型点坝(美国蒙大拿州Powder河,45°19'30″N,105°32'40″W);C—顺流迁移型点坝(阿根廷Chubut河, 43°50'19.71″S,67°54'41.18″W);D—旋转顺流迁移型点坝(阿根廷Rio Negro河40°13'30.90″S,64°7'50.84″W);E—顺流迁移型点坝与逆流加积的沉积物(美国阿拉斯加Koyukuk河,65°0'50.01″N,157°29'50.61″W); F—顺流迁移型点坝与反向坝沉积物(加拿大Beaver河,54°16'48.67″N,110°5'34.01″W)