[1] Chun Chang Huang, Jiangli Pang, et al. High-resolution studies of the oldest cultivated soils in the southern Loess Plateau of China. Catena, 2002, (47):29～42.
[2] Chun Chang Huang, Jiangli Pang,et al. An early Holocene erosion phase on the Loess tablelands in the southern Loess Plateau of China . Geomorphology, 2002, (43):3～4,209～218.
[3] 刘东生,等. 黄土与环境. 北京: 科学出版社, 1985. 92～99[Liu Tungsheng, et al. Loess and Environmental. Beijing: Science Press, 1985. 92～99]
[4] Zhou W J, An Z S, Jull A, Donahue D, Head M. Reappraisal of Chinese Loess Plateau stratigraphical sequences over the last 30,000 years: precursors of an important Holocene monsoon climatic event. Radiocarbon, 1998, 40(2), 905～913.
[5] Huang Chunchang, Zhou Jie, Pang Jiangli, et al. A regional aridity phase and its possible culture impact during the Holocene Megathermal in the Guanzhong basin, China. The Holocene, 2000, 10(1): 135～143.
[6] 施雅风,孔昭宸,王苏民,等. 中国全新世大暖期的气候波动与主要事件. 中国科学(B辑), 1992, (12): 1300～1308[Shi Yafeng, Kong Zhaochen, Wang Sumin, et al. Climatic Fluctuation And Important Events During Holocene Magathermal In China. Science in China(B), 1992, (12):1300～1308]
[7] 孙英民,李有谋. 考古学导论. 河南开封: 河南大学出版社, 2002. 80～81[Sun Yingmin, Li Youmou. Introduction to Archaeology. Kaifeng Henan: Press of Henna University, 2002. 80～81]
[8] 黄春长,庞奖励,张战平. 黄土高原环境恶化的自然背景研究. 陕西师范大学学报(自然科学版), 2000, 28(3): 110～114[Huang Chunchang, Pang Jiangli, Zhang Zhanping. Background of Environmental Deteriortion in Loess Plateau. Journal of Shaanxi Normal University (Natural Science), 2000, 28(3): 110～114 ]
[9] 赵景波. 风化淋滤带地质新理论-CaCO3淀积深度理论. 沉积学报, 2000,18(1): 29～35[Zhao Jingbo. A new geological theory about eluvial zone-theory illuvial on depth of CaCO3. Acta Sedimentologica Sinica 2000,18(1): 29～35]
[10] 郭正堂, 魏兰英, 吕厚远,等. 晚第四纪风尘物质成分的变化及其环境意义. 第四纪地质,1999, (1): 41～48[Guo Zhengtang, Wei Lanying, Lv Houyuan, et al. Changes in the composition of Late Pleistocene aeolian dust and the environmental significance. Quaternary Sciences 1999 (1): 41～48]
[11] 赵景波. 西北黄土区第四纪土壤与环境. 西安: 陕西科学技术出版社, 1994. 28～69[Zhao Jingbo. Quaternary soils and environment in loess area of Northwestern China. Xi'an: Shannxi Science and Technological Press, 1994. 28～69]
[12] 朱显谟,祝一志. 试论中国黄土高原土壤与环境. 土壤学报,1992, (4): 351～357[Zhu Xianmo, Zhu Yizhi. A preliminary study on soil on Loess Plateau and environmental. Acta Pedologica Sinica, 1992, 29(4): 351～357]
[13] 刘东生,等. 黄土与环境. 北京:科学出版社, 1985. 232～235[Liu Tungsheng, et al. Loess and Environmental. Beijing: Science Press, 1985. 232～235]
[14] 师育新,戴雪荣,李节通,等. 末次间冰期兰州黄土记录中的粘土矿物及其环境意义探讨. 海洋地质与第四纪地质, 1997, 17(1): 87～93[Shi Yuxin, Dai Xuerong ,Li Jietong, et al. Origin and significance of clay minerals in the Last Interglacial Loess in Lanzhou Area, North-Central China. Marine Geology & Quaternary Geology, 1997,17(1): 87～93]
[15] 中国科学院<中国自然地理>编辑委员会. 中国自然地理.土壤地理. 北京:科学出版社, 1981.60～62[Chinese Academy of Science. Chinese Physical Geography.Soil Geography. Beijing: Science Press,1981. 60～62]
[16] 黄春长. 渭河流域3100年前资源退化与人地关系演变. 地理科学, 2001, 21(1): 30～35[Huang Chunchang. The Deterioration of Land Resources and the Change in Human-Earth Relationships in the Weihe River Basin at 3100aB.P. Scientia Geographical Sinica , 2001, 21(1):30～35]