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天水黄土沉积特征与环境变化
引用本文:刘小丰,潘保田,高红山,王勇,王均平,张慧,胡春生.天水黄土沉积特征与环境变化[J].中国沙漠,2007,27(3):373-378.
作者姓名:刘小丰  潘保田  高红山  王勇  王均平  张慧  胡春生
作者单位:兰州大学资源环境学院/西部环境教育部重点实验室, 甘肃 兰州 730000
基金项目:国家自然科学基金;NSFC创新群体基金;国家重点基础研究发展计划(973计划)
摘    要:中滩剖面系中滩镇渭河第四级阶地上的黄土堆积,通过黄土剖面的地层结构及粒度分析表明,其形成于0.9 Ma以来,河漫滩堆积年代为0.86—0.94 Ma。在过去1 Ma以来,中滩黄土及河漫滩剖面的地层特征、粒度曲线表明其记录了9个湿热-干冷气候旋回,3次冬季风强化阶段,存在着3次极端干旱事件。中滩黄土粒度特征以粉砂为其众数粒级,其次为粘土颗粒,不同于黄土高原其他地区,可能与秦岭北麓的湿润环境及六盘山对冬季风的阻挡有关。

关 键 词:黄土  粒度曲线  黄土-古土壤序列  气候旋回  1Ma  甘肃天水  
文章编号:1000-694X(2007)03-0373-06
收稿时间:2005-12-12
修稿时间:2006-03-03

Loess Deposit Feature and Environmental Change in Tianshui,Gansu Province
LIU Xiao-feng,PAN Bao-tian,GAO Hong-shan,WANG Yong,WANG Jun-ping,ZHANG Hui,HU Chun-sheng.Loess Deposit Feature and Environmental Change in Tianshui,Gansu Province[J].Journal of Desert Research,2007,27(3):373-378.
Authors:LIU Xiao-feng  PAN Bao-tian  GAO Hong-shan  WANG Yong  WANG Jun-ping  ZHANG Hui  HU Chun-sheng
Institution:School of Resource and Environmental Sciences of Lanzhou University; Key Laboratory of Western China’s Environmental Systems under Ministry of Education, Lanzhou 730000, China
Abstract:Zhongtan section is loess deposits on the fourth terrace of Weihe River in Tianshui city of Gansu province. Based on stratigraphic feature and grain size curve, the loess was formed since 0.9 Ma BP, and the floodplain was deposited during 0.86-0.94 Ma. During the last 1 Ma, Zhongtan underwent nine moist hot-dry cold cycles, three winter monsoon intensifications, and three extremely dry events. Grain size date indicates that Zhongtan loess is different from other sections in the Longxi basin, which was caused by the uplifting of Liupan Mountain and moist environment in the flank of Qinling.
Keywords:1 Ma
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