1.
Evaluation on the Water-retention Properties of Eroded Soil Developed from Quaternary Red Clay Region
第四纪红粘土区侵蚀土壤持水性能的评价
2.
Aeolian-genesis comparability of aggraded red earth in south China with loess in north China;
第四纪加积型红土与黄土的风成相似性探讨
3.
COMPARATIVE STUDY ON QUATERNARY RED EARTH AND XIASHU LOESS IN PHYSICAL AND CHEMICAL CHARACTERISTICS
第四纪加积型红土与下蜀黄土理化特征比较
4.
On the red earth platform of Quaternary period,average permu growth volume is 0.39m~3,output value is 43.05 yuan.
第四纪红土台地上,亩年平均生长量0.391立方米,产值43.05元;
5.
Aggradation Red Earth Sediments in Mid-subtropics of China and Their Recorded Environmental Changes during Quaternary;
中亚热带加积型红土及其所记录的第四纪环境变化探讨
6.
The Physical and Chemic Characters of Ferromanganese Nodules in the Quaternary Red Earth in Southern China;
中国南方第四纪红土中结核的理化特征及形成环境
7.
Basic Properties and Genetic Characteristic Research of Quaternary Paleosolin Chaoyang City of Liaoning
辽宁省朝阳市第四纪古红土基本性状与发生学特征研究
8.
Clay Mineral Composition and Surface Electric Characteristics of Quatemary Red Soils with Different AgriculturalUtilization Pattems in Southem Hunan Province
不同农业利用方式下湘南第四纪红壤的粘粒矿物学组成与表面电荷特性
9.
The Origin of Neogene's Red Clay in the Middle Reaches of Yellow River;
中国黄河中游地区新近纪红粘土的成因
10.
THE STUDY ON THE RED SOIL OF NEOGENE IN XIAN AND BAODE OF SHANXI
西安、山西保德第三纪晚期红土的研究
11.
State Key Laboratory of Loess and Quaternary Geology
黄土与第四纪地质国家重点实验室
12.
SOME PROOFS ABOUT EOLIAN ORIGIN OF QUATERNARY OLD RED SANDS IN EASTERN GUANGDONG AND NORTHEASTERN HAINAN
粤东及琼东北第四纪老红砂风成的若干证据
13.
The Engineering Geology of Gray Clay of Zhangjiang Group of Quaternary System in Haikou District
海口地区第四系湛江组灰色粘土的工程地质特性
14.
Nanominerals of the Loess-red Clay Sequences in Chinese Loess Plateau
中国黄土高原土—红粘土纳米矿物研究
15.
The court, clay, had come through its first winter pitted and windswept bare of redcoat
球场上的粘土经过第一个冬天以后，变得坑坑洼洼，表面的红土都给风刮去了。
16.
The Cenozoic Era is composed of Tertiary Period followed by Quaternary Period.
新生代是由第三纪和第四纪组成的。
17.
The second period of the Cenozoic Era and its system of deposits.
第四纪新生代第二纪及沉积系
18.
But you have obviously never been exposed to fourth-level geology; you're still quite a stranger to loess.
但是你显然根本没有摸过第四纪地质学，你对黄土还很陌生。