1.
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;
2.
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
3.
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;
4.
Most loess is considered to be an eolian deposit.
大多数黄土被认为是一种风成沉积。
5.
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。
6.
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
7.
Luminescence Dating of Aeolian Sediments Using Single Aliquot Technique
风成沉积石英绿光释光测年的单片技术
8.
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
9.
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
10.
Changes in Eastern Asian Winter Monsoon Recorded by Aeolion Deposits at the Southeastern Margin of Qaidam Basin Over the Past 5000 Years
近5000a来柴达木盆地东南缘风成沉积记录的冬季风演化
11.
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。
12.
AEOLIAN DEPOSIT EVIDENCE FOR FORMATION AND EVOLUTION OF THE TENGGER DESERT IN THE NORTH OF CHINA SINCE EARLY PLEISTOCENE
早更新世以来腾格里沙漠形成与演化的风成沉积证据
13.
ROCK MAGNETISM OF THE HOLOCENE EOLIAN DEPOSITS IN ?THE LOESS PLATEAU: EVIDENCE FOR PEDOGENESIS
黄土高原全新世风成沉积的岩石磁学性质及其古气候意义
14.
a fine-grained unstratified accumulation of clay and silt deposited by the wind.
一种风沉积而成的颗粒细
15.
A buff to gray windblown deposit of fine-grained, calcareous silt or clay.
黄土一种风沉积而成的颗粒细
16.
THE OLDEST EOLIAN LOESS DEPOSITION IN LONGXI BASIN-YANDONGGOU PROFILE IN LANZHOU
陇西盆地最老的风成黄土沉积——兰州烟洞沟剖面
17.
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。
18.
The weathered and eroded residue of any family of rock can be observed today being transported to the sea for deposition and conversion into sedimentary rocks.
今天我们能见到任何一类岩石经风化、剥蚀而搬运到海里而沉积形成沉积岩。