1.
Alluvial fan deposits in the Kongdian Formation,Huanghua depression
黄骅坳陷孔南地区孔店组冲积扇沉积特征及地质意义
2.
From Paleocene to Miocene, the sedimentary facies evolved from the extensive alluvial fan to the braided fluvial river environment.
从古新世到中新世，柴达木盆地北缘经历了由大规模冲积扇沉积到辫状河沉积的演化过程。
3.
braided-fan-delta deposit
网状冲积扇三角洲沉积
4.
Luohe formation mainly develops aeolian deposit, alluvial fan and braided deposit.
洛河组主要发育风成沉积、冲(洪)积扇、辫状河沉积;
5.
Discussion of the Sedimentary Characters of Alluvial-proluvial Fan of Bauxite Series,Jiujialu Formation in Central Guizhou
论贵州中部九架炉组铝矿系冲洪积扇沉积特征
6.
Major sedimentary facies in the Luohe Formation include alluvial fans facies, eolian facies,braided fluvial facies, and desert facies.
洛河组主要沉积了冲积扇相、风成沉积相、辫状河相和沙漠相;
7.
SEDIMENTARY FACIES FEATURES AND RECOG-NITION OF EOGENE SUBAQUEOUS ALLU-VIAL FANS IN DONGYING DEPRESSION
东营凹陷北带下第三系水下冲积扇的沉积相特征及其识别
8.
SEDIMENTARY CHARACTERISTICS OF ALLUVIAL FANS IN LOWER MEMBER OF YAGELIEM FORMATION (LOWER CRETACEOUS), KAPUSALION, BAICHENG
拜城县卡普沙良下白垩统亚格列木组下段冲积扇的沉积特征
9.
Alluvial Fan Conglomerate Reservoir Sedimentary Characteristics of Lower Karemary Formation in the 6th District of Karemary Oilfield
克拉玛依油田六区克下组冲积扇砾岩储层沉积特征
10.
There are two types of sedimentary facies in this region: the alluvial fan and the braided fluvial river.
结绿素－红山地区古新统至中新统发育2种沉积相类型，即冲积扇和辫状河。
11.
Small alluvial fans at mouths of wet weather drainage ways also are commonly intermixed indistinguishably.
潮湿气侯地区河道出口处的小冲积扇，其沉积物的混合通常也难以区别。
12.
STUDY ON SEDIMENTS AND SEDIMENTATION IN OKINAWA TROUGH
冲绳海槽沉积物及其沉积作用的研究
13.
shock wave induced by energy deposition
能量沉积产生冲击波
14.
Sedimentary characteristics and reservoir property of sublacustrine fan in Chexi Area
车西地区湖底扇沉积特征及储集物性
15.
Discrimination between the Features of Remote Sensing Images of Alluvial-diluvial Fan and Debris Flow Fan;
冲洪积扇与泥石流扇的遥感影像特征辨析
16.
The Sedimentary Characteristics and Its Control Factors of Nearshore Subaqueous Fan-Turbidite Fan in the Shahejie Formation of Chengbei Fault-step Zone;
埕北断阶区沙河街组近岸水下扇—浊积扇沉积特征及其控制因素
17.
fan-topped pediment
冲积扇覆盖的山前侵蚀平原
18.
These channels are most common near the apex of the alluvial fan body.
这些河道最常见于近冲积扇体的顶端。