1.
Wind-deposited sediment called loess occurs in many places.
被称为黄土的风成沉积物，在许多地区均有。
2.
COMPARISON OF IRSL AND GLSL DATING OF AEOLIAN SEDIMENTS
风成沉积物红外及绿光释光测年比较研究
3.
Analysis of Grain-size Populations With Environmentally Sensitive Components in Aeolian Deposits and Their Implications
风成沉积物环境敏感粒度指标的提取及意义
4.
A STUDY ON THE RELATIONSHIP BETWEEN MAGNETIC ANISOTROPY OF MODERN EOLIAN SEDIMENTS AND WIND DIRECTION
现代风成沉积物磁化率各向异性与风向关系的研究
5.
Study on Grain-size of the Aeolian Sediments in the Northern Fringe of Xiangshan Mountain During the Last Glacial
香山北麓末次冰期风成沉积物粒度的空间变化研究
6.
Grain Size P?arameters of Loess-palaeosol Deposits from Graphic and Moment Methods: A Comparative Study;
末次冰期旋回风成沉积物图解法与矩值法粒度参数的对比
7.
resembling or containing or formed by the accumulation of sediment.
类似于沉积物的，包含沉积物的，或由沉积物沉积形成的。
8.
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;
9.
Loose sediments may be changed into solid sedimentary rocks.
松散的沉积物可以变成坚硬的沉积岩。
10.
MAGNETIC FABRIC CHARACTERISTICS OF HYDRAULIC DEPOSIT, EOLIAN DEPOSIT AND PALEOSOL
水成沉积与风成沉积及古土壤的磁组构特征
11.
organically formed sedimentart rock
生物作用形成的沉积岩
12.
The studies of Mongolian Holocene climate changes mainly focused on the records of tree-rings, eolian sediments and lacustrine sediments.
蒙古全新世气候变化研究侧重于对树轮、风成沉积和湖泊沉积物的研究。
13.
THE SEDIMENTARY STRUCTURES AND THE FACIES MODEL OF THE LATE PLEISTOCENE EOLIAN BIOCALCARENITES IN SHIDAO ISLAND OF XISHA ARCHIPELAGO
西沙石岛晚更新世风成生物砂屑灰岩的沉积构造和相模式
14.
Substance Source of the Holocene Aeolian Loess-soil and Its Depositional Dynamics in Yuzhou, Henan Province;
河南禹州全新世风成黄土—土壤物质来源与沉积动力研究
15.
clay soil formed by sedimentary deposits.
由沉积的沉淀物形成的粘土。
16.
a sedimentary rock formed from clay deposits.
一种由粘土沉淀物形成的沉积岩。
17.
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;
18.
Numerical Simulation and Analysis of Particle Deposition in Rectangular Ventilation Ducts
矩形风管内颗粒物沉积的模拟与分析