盛冰期南京石笋δ18O与年纹层厚度的对比

根据南京葫芦洞一支石笋高精度^230Th年龄及纹层计数，建立年际精度时标．在21800～21180aBP时段内，石笋纹层厚度与δ^18O的良好相关性，支持纹层厚度反映夏季风降水效应的观点．两种代用指标提供了末次盛冰期持续620年的十年际分辨率季风降水信息．年纹层及δ^18O序列的功率谱分析结果表明全球冰量最大背景下十年-百年尺度的季风气候变化与太阳活动周期基本一致．     

STRATIGRAPHIC AND GEOCHRONOLOGIC ANALYSES OF THE QUATERNARY DEPOSITS IN THE THREE-LAKE REGION OF QAIDAM BASIN

The Qaidam Basin is a larger sedimentary basin in western China where the thickness of the Quaternary deposits is in the range of 2000-3000 m at its subsiding center. This paper first dates palaeomagnetically the cores obtained from the five continuously sampled intervals and those from a typical profile, determineds the age of the index fossil zones, and calculates the deposition rates for the varve deposits based on the sedimentological analysis. As a result, we can calculate the ages of the various characteristic beds (including fossil zones, seismic reflection beds, and marker layers of electrical properties) for any given borehole-section when it was divided into facies, and check the validity of the chronology. According to all those studies, the stratigraphic and geochronologic analysis program of the Quaternary deposits in the Qaidam Basin has permitted a detailed discussion to be made in this paper.     

末次盛冰期南京降水记录中ENSO的演化

基于南京葫芦洞一支石笋TIMS-U系测年和纹层计数的交叉定年。获得丁末次盛冰期在24170～21222aBP时段石笋年纹层厚度的时间序列,主要反映了夏季风降水变率．小波分析揭示末次盛冰期连续3ka夏季风降水记录中厄尔尼诺一南方涛动（ENSO）周期和强度随时间的演化特征,该记录表明ENSO在末次盛冰期并非一直存在,有着高发期和平缓期。其爆发的频率和强度逐渐减弱。支持ENSO演化的“冰期阻尼效应”假说．     

人类活动与黄河三角洲发育的关系

从历史地理学和沉积学角度探讨了晚全新世以来人类活动对黄河三角洲发育过程的影响。一方面，黄河流域高原产沙区土地利用方式的改变影响着入黄泥沙数量和河口地区堆积方式；另一方面，河口三角洲地区的人工改造、引水引沙等一系列工程措施控制着黄河三角洲的发育模式和空间展布规律。