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- rubified paleosol 网纹红土
- The evening glow rubified the sky. 晚霞染红了天空。
- Because of the characteristic of paleosol's distribution of double-apices, the differences between high-order skewness and kurtosis are obvious. 偏态注重粒度分布的尾部，峰态关注峰的宽窄，且由于古土壤呈明显的双峰分布，因而高阶偏态和峰态差异显著。
- The bottom boundary of Malan loess or the development of the first paleosol is chronologically different from place to place. 马兰黄土底界或第1古土壤层的发育是穿时的。
- In the loess, the S 1 paleosol and a weaker paleosol, properly the L 1SS 1 and just below the aeolian sands, can be distinguished. 在黄土地层中可以识别出S1古土壤和位于风沙堆积下面的可能为L1SS1的弱成土层。
- The grain size of loess and paleosol sequence is regarded as one of the most important proxies to reconstruct paleoenvironment. 摘要黄土、古土壤剖面中物质粒度是恢复古环境的重要指标之一。
- This paper tallied up that the distribution of plinthitic red paleosol is just coincide with the tea in the area north of Yantze River(Fig. 1). 摘要本文总结了全国网纹红土分布与长江以北大部茶树分布恰相符合；
- Carbon isotopic composition of modern soil and paleosol as a response to vegetation change on the Chinese Loess Plateau. 黄土高原现代土壤和古土壤有机碳同位素对植被的响应","Liu, WG;Ning, YF;An, ZS;Wu, ZH;
- Li Xuyong ,Li Baoguo and Guo Zhengtang ,1998 .A Soil Development Index for Paleosol Research. In: Paleosoil and Climatic Change. Paleopedology Commission, INQUA/ISSS, p.206. 胡克林，李保国，林启美，李贵桐，陈德立，1999;农田土壤养分的空间变异性特征;农业工程学报，15(3):33-38.
- The results show that grain-size fractal dimension is related to loess and paleosol closely, which can be regarded as good indictor of deposition and pedogenic environment. 计算结果表明：粒度的分形维数与黄土和古土壤层位具有良好的对应关系，对沉积和成壤环境具有很好的指示意义。
- Li Xuyong, Li Baoguo, Guo Zhengtang, Zhao Chengyi and Shi Yuanchun. 1999. A Soil Morphological Index for Paleosol Research. Chinese Science Bulletin， 44(supp.):218-222. 李卫东，李保国，石元春，1999,区域化土壤质地剖面的概念和确定方法,地理科学，
- ZHANG Jia-qiang,LI Cong-xian,CONG You-zi.Magnetic fabric characteristics of hydraulic deposit,eolian deposit and paleosol[J].Marine Geology &Quaternary Geology,1999,19 (2):85-94. [9]张家强;李从先;丛友滋.;水成沉积与风成沉积及古土壤的磁组构特征[J]
- The number of loess and paleosol units in Quaternary sequences of the Middle Danubian Basin is often closely related to the geological and geomorphological position of the sediment series. 文章叙述了多瑙河中游盆地的第四系黄土与古土壤层序。
- The study on the magnetic fabric of the Late Quaternary hydraulic deposit,eolian deposit and paleosol shows that each type of the deposits has different magnetic fabric characteristics. 晚第四纪水成沉积、风成沉积、古土壤等的磁组构研究表明，不同成因的沉积物具有明显不同的磁组构特征。
- Among the loess, paleosol and red clay, there are differences in magnetic mineral composition, which strongly indicates the paleoclimate characteristics from the loess, paleosol to the red clay stage. 黄土、古土壤和红粘土磁性矿物组成差异，反映了其形成期不同的古气候特性以及不同气候条件下生物地球化学作用强度的差异。
- The Climatic Record of Organic Matter in the Paleosol from the Yuanbao Holocene Profile 临夏塬堡全新世黄土剖面古土壤有机质碳同位素的气候记录
- Particle -size Features of Chuodun Paleosol and Identification of Its Parent Material 昆山绰墩古土壤粒度特征及母质判别
- The Discovery and Research on the Ferriferous Clay Nodules of 5th Paleosol Layer in Xi'an and Baoji 西安和宝鸡第5层古土壤铁质粘土结核的发现与研究
- Study on Magnetic Susceptibility of Loess and Paleosol Sequences in Westerly Region of Xinjiang 新疆西风区黄土与古土壤磁化率变化特点
- 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
