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1)  fans sedimentation
扇体沉积演化
2)  Sedimentary evolution
沉积演化
1.
The Tertiary sedimentary evolution of the Qaidam Basin, Northwest China;
柴达木第三纪湖盆沉积演化史
2.
Tectonic-sedimentary evolution of the first and second members of the Kongdian Formation in southern Kongdian,Huanghua depression;
黄骅坳陷孔南地区孔一、孔二段构造沉积演化
3.
Discussion on relationship between sedimentary evolution of the Triassic Yanchang Formation and the Early Indosinian Movement in Ordos Basin;
鄂尔多斯盆地三叠系延长组沉积演化及其与早印支运动关系的探讨
3)  depositional evolution
沉积演化
1.
The Depositional Evolution of Neozoic Basin in Tianshui-Qin an Area;
秦安—天水地区新生代盆地沉积演化
2.
Methods Disscuss the basin evolvement phases according to the characteristic of the basin stratum,fault activity and depositional evolution.
方法通过盆地断裂活动特征、沉积演化特征探讨盆地演化阶段。
3.
The Okinawa Trough (OT) is a back-arc basin related with the plate subduction since the late Miocene (9 to 6 Ma), and its depositional evolution can be divided into 3 stages, stage Ⅰ from the late Miocene (9 to 6 Ma) to the late Pliocene (2 Ma), stage Ⅱ from the late Pliocene (2 Ma) to the late Pleistocene (130 ka) and stage Ⅲ from the Pleistocene to the present.
将冲绳海槽的沉积演化分成3个阶段:中新世晚期(9~6Ma)—上新世末期(2Ma)、上新世末期—晚更新世(130ka)、晚更新世—现在。
4)  fan sediment body
扇型沉积体
5)  fan_shaped sedimentary body
扇形沉积体
1.
The growth process of a fan_shaped sedimentary body is a complex nonlinear dynamic process.
扇形沉积体是我国内陆及近海中、新生代含油气盆地的重要油气聚集体 ,如何定量地表征沉积体的分布状况及内部结构参数的空间变化规律 ,对指导油气勘探具有重要意义 。
6)  alluvial fan sedimentary system
冲积扇沉积体系
补充资料:扇和
1.宣扬附和。
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