排序方式: 共有65条查询结果,搜索用时 421 毫秒
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腾格里沙漠晚更新世以来湖相沉积年代学及高湖面期的初步确定 总被引:20,自引:1,他引:20
张虎才 《兰州大学学报(自然科学版)》1997,(2)
对腾格里沙漠古湖泊沉积和地貌的考察及对典型代表剖面初步研究结果表明,一个连续而巨大的淡水湖泊高水位形成于距今3.9~3.6万年前.在距今3.3~2.3万年期间,腾格里沙漠西北部曾存在一面积至少达16200km2、水深25m(白碱湖,最大水深超过60m,分布于大海子一带)的淡水湖泊.大量的瓣鳃类、腹足类化石及介形类化石组合的存在表明该时期湖泊水温不低于10℃,由此把该时期的湖泊暂且称“腾格里大湖”(MegalakeTengger) 相似文献
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广东南雄断裂带Ar-Ar年龄及其地质意义 总被引:3,自引:0,他引:3
南雄断裂带是一条大型的拉伸剥离断层。在详细的野外调查和岩石样品镜下观察的基础上,对南雄断裂带糜棱岩中的同构造变形-变质矿物白云母进行了Ar-Ar法同位素年龄测定。年代学研究结果表明,南雄断裂带作为拉伸剥离正断层活动开始于早白垩世(117.3±2.7 Ma),而其强烈的伸展变形韧性剪切发生在早白垩世末~晚白垩世初(Ar-Ar坪年龄为94.6±0.4 Ma),随后在88.9±1.0 Ma和81.1±2.0 Ma还可能发生过2次较明显的热扰动事件。南雄断裂带Ar-Ar年龄数据为进一步判断华南白垩纪岩石圈伸展作用发生的时间提供了新的热年代学制约,即是说,早白垩世末~晚白垩世初是区域岩石圈伸展的重要时期。 相似文献
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汪前进 《广西民族大学学报》2006,12(2):13-27
从文献的角度按时间序列尽量弄清黄河及其支流究竟在何时、何地出现河清,持续多久、发生的范围及其程度,以及朝野做出的反映与采取的行动. 相似文献
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宝天曼自然保护区油松生长释放研究 总被引:2,自引:2,他引:0
利用采自宝天曼自然保护区的一组油松(Pinus tabulaeformis Carr.)树轮样芯,根据树木年轮学的基本方法测量油松样芯的年轮宽度并交叉定年,通过生长变化率的大小对生长释放事件进行了判定.结果显示77.78%的油松有过一次以上的生长释放事件,平均每棵油松的释放次数为4.6次;随着油松年龄的增长,林窗逐渐开放,油松生长释放次数逐渐增多,不同年龄段31~40 a、41~50 a、51~60 a、>60 a的油松,平均每株释放次数分别为1.6、3.6、4.6、11.3次;不同年龄的油松在1969和1999年左右出现了较大的生长释放事件. 相似文献
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三百山盆地的粗面岩主要出现在盆地东部仰天湖破火山口构造中,粗面岩锆石SHRIMP测年的年龄为141.56±0.96 Ma,应归属于早白垩世.盆地粗面岩具有钾含量高,全碱含量高,稀土元素配分曲线图表现为右倾的轻稀土富集型,Eu负异常不明显或表现为正异常的特征,表明三百山盆地的粗面岩属橄榄玄粗岩系列,具有高压型粗面岩的特征,标志着一个加厚的陆壳存在;岩浆物质来源于由上地壳物质俯冲到深部与地幔的混合而形成的再循环富集地幔,岩石形成的构造环境为“同碰撞”环境,代表挤压至拉张过渡构造环境. 相似文献
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A preliminary study of chronology for a newly-discovered ancient city and five archaeological sites in Lop Nor,China 总被引:1,自引:0,他引:1
YIDILISI Abuduresule 《科学通报(英文版)》2010,55(1):63-71
In the past century, it has long been debated in the archeological, historical, geographical, and many other related communities where the capital of the Luolan and Shanshan states was in the Lop Nor region. This paper presents three AMS radiocarbon ages from a newly-discovered ancient city at about 6.3 km to the northwest of the Xiaohe Graveyard, and fifteen new radiocarbon ages from the Loulan (LA), LE, Qieerqiduke, Milan, and Tuyin sites in Lop Nor. The new investigation shows that the age of newly-disco... 相似文献
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Two tree-ring MXD (maximum latewood density) chronologies of Abies fabri were developed from the eastern slopes of Gongga Mountain, and a regional chronology (RC) was established based on the two MXD chronologies. There were significant positive correlations between the three MXD chronologies and August–September temperature, and the RC had the highest correlation (r=0.733, n=48, P<0.001) with mean August–September temperature. Based on growth-climate analyses, we reconstructed mean August–September temperature during the past 171 years for the study area. The reconstruction explained 53.5% of the instrumental temperature variance during the period 1960–2007 (F=52.8, R2adj =52.4%). In the past 171 years, there were 22 very warm years and 23 very cold years, four cold periods (1837–1842, 1884–1891, 1899–1905 and 1984–1989) and three warm periods (1966–1973, 1916–1924 and 1876–1881). Our reconstruction was validated by other tree ring-based temperature reconstructions from the surrounding area and documented climate disaster events. 相似文献