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1.
甘肃临夏盆地8~6 MaBP的构造变化   总被引:1,自引:0,他引:1  
甘肃临夏盆地毛沟剖面上半部高精密度古地磁测年结果表明该剖面磁极性年龄为4.34~13.07 MaBP,其中东乡组、柳树组与何王家组的年龄分别为13.07~7.8 Ma,7.8~6.4 Ma和6.40~4.34 MaBP.该测年结果与文献[1]测得的结果基本一致.临夏盆地6.40~6.16 MaBP湖泊沉积环境突变,8 MaBP左右毛沟剖面地层磁偏角发生明显偏转,盆地中王家山剖面银川沟背斜大约在6 MaBP左右发生倾斜与变形,这表明临夏盆地8~6 MaBP经历了一次强烈的构造运动.  相似文献   

2.
    
《科学通报(英文版)》1995,40(11):926-926
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3.
为了克服传统直流电动机因机械换向带来的火花、噪声等缺点,变磁极性直流电动机成为电机无刷化的一个新的发展方向。变磁极性直流电动机采用磁极换向的方式产生旋转磁场,从而带动通以直流电的电枢转动。建立起电压、转矩方程,并推导出电机的机械特性方程,对变磁极性直流电动机的进一步研究有参考价值。  相似文献   

4.
    
Ages of the stratigraphic boundary MIS1/2 and MIS3/4 of the Yuanbu loess section in Linxia are used as the basis of the nodal control age. The age of MIS1/2 and MIS3/4 are obtained from the latest international research result—the climatic events recorded in the stalagmite in the Hulu Cave in Nanjing, that MIS1/2 is 11.5 kaB.P. and MIS3/4 is 59.8 kaB.P.. The ages of the two climatic events contain three nodal age control models (Model 1: 0 kaB.P.—59.8 kaB.P.; Model 2: 0 kaB.P.—11.5 kaB.P. and 11.5 kaB.P.—59.8 kaB.P.; Model 3: 11.5 kaB.P.—59.8 kaB.P.), which are used as the nodal control age separately. The deposition times of various stratigraphic horizons are calculated by using the magnetic susceptibility age model and grain-size age model, and then compared with each other. In addition, the AMS14C age, OSL age and the ages of YD and H events are compared with the ages of the corresponding horizons calculated by the three models of nodal control ages. From the analyses of lithologic characters and climatic stages it has been found that both the magnetic susceptibility age model and the grain-size age model have some defects. Because the accurate control ages are selected as the nodal points of the glacial period or interglacial period, the stratigraphic deposition times determined by the high resolution of magnetic susceptibility age model and grain-size age model approximate to the actual ages. As for the relative accuracy of the two age models, the magnetic susceptibility age model is more accurate than the grain-size age model.  相似文献   

5.
    
Ages of the stratigraphic boundary MIS1/2 and MIS3/4 of the Yuanbu loess section in Linxia are used as the basis of the nodal control age. The age of MIS1/2 and MIS3/4 are obtained from the latest international research result—the climatic events recorded in the stalagmite in the Hulu Cave in Nanjing, that MIS1/2 is 11.5 kaB.P. and MIS3/4 is 59.8 kaB.P.. The ages of the two climatic events contain three nodal age control models (Model 1: 0 kaB.P.—59.8 kaB.P.; Model 2: 0 kaB.P.—11.5 kaB.P. and 11.5 kaB.P.—59.8 kaB.P.; Model 3: 11.5 kaB.P.—59.8 kaB.P.), which are used as the nodal control age separately. The deposition times of various stratigraphic horizons are calculated by using the magnetic susceptibility age model and grain-size age model, and then compared with each other. In addition, the AMS14C age, OSL age and the ages of YD and H events are compared with the ages of the corresponding horizons calculated by the three models of nodal control ages. From the analyses of lithologic characters and climatic stages it has been found that both the magnetic susceptibility age model and the grain-size age model have some defects. Because the accurate control ages are selected as the nodal points of the glacial period or interglacial period, the stratigraphic deposition times determined by the high resolution of magnetic susceptibility age model and grain-size age model approximate to the actual ages. As for the relative accuracy of the two age models, the magnetic susceptibility age model is more accurate than the grain-size age model.  相似文献   

6.
    
In different opinions, the stratigraphic time of the feathered dinosaurs and early birds in Sihetun and its neighboring areas in Beipiao, western Liaoning is appointed to different epoches of eras, such as Late Jurassic, Early Cretaceous and Late Jurassic-Early Cretaceous. Even the recently dating data are still very different. This note first reported the U-Pb age of (125.2±0.9) Ma of zircon separated from tuff of Sihetun vertebrates horizon. The age reveals that Sihetun vertebrate belongs to Early Cretaceous. The method is more objective, because of the strong ability of disturbance resistance and high U-Pb blocking temperature of zircons.  相似文献   

7.
    
《科学通报(英文版)》1991,36(24):2073-2073
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8.
黄金分割法是一种快速搜索函数极值的优化设计方法.研究了它在快速在线极性相关器中的应用,详细讨论了极性相关函数极值搜索的黄金分割设计方法.采用8031单片微机构成极性相关器,黄金分割法的应用,使得完成一次相关分析的时间缩短到1秒以内.  相似文献   

9.
讨论了赣中乐平地区沿沟剖面上二叠统至下三叠统地层的牙形石动物群,列出了牙形石的各个形态属种在地层中的分布及其数量变化.根据特征牙形石分子的地层分布,将该段地层自下而上划分为3个牙形石带,分别是:Clarkina changxingensis-Cl.deflecta-Cl.subcarinata组合带;Hindeodus latidentatus带和Hindeodus parvus带.鉴于在晚二叠世至早三叠世,Hindeodus属种的牙形石分子的Pa分子成为界定种之间的主要标志特征,本文描述了两个重要牙形石种即Hindeodus latidentatus和Hindeodus parvus的Pa分子,并探讨了二者之间所具有的演化关系;此外,还指出这些保存完美的Pa分子具有重要的研究价值.  相似文献   

10.
百花山兽类区系特征及生态分布   总被引:4,自引:0,他引:4  
1989~1991年对百花山自然保护区的兽类区系进行了比较系统的调查,共记录到6目13科25种.整个区系以古北界成分为主,占68.0%,同时也呈现出比较明显的南、北两方动物分布的过渡特征.本文从地理分布特征出发,对本区兽类区系的组成进行了比较详细的分析,并讨论了这些兽类的生态分布和垂直分布状况以及鼠形动物的季节变化.  相似文献   

11.
A new species of Gobiconodon is found from the Yixian Formation of western Liaonlng, China. The new taxa,G zofiae sp. nov., has a confluent opening for branches Ⅱand Ⅲ of the trigeminal nerve on the anterior lamina of the petrosal. G zofiae sp. nov. is similar to Repenomamus in having an ossified Meckel‘s cartilage connecting the lower jaws and ear region. The new species, with enlarged I^1/I1, posteriorly located infraorbital foramen and four mental foramina,distinctly differs from the other species of Gobiconodon. The new material indicates that Gobiconodon has four, not five,upper molariforms. The presence of Gobiconodon in Jchol Biota makes it possible to correlate Jehol Biota with faunas in eastern Asia and North America, and suggests the age of the Yixian Formation to be Early Cretaceous.  相似文献   

12.
对江西省信丰县铁石口剖面晚二叠世长兴阶至铁石口阶下部的牙形石动物群有了新的认识。基于牙形石的研究,将该地区晚二叠世的地层划分为3个牙形石生物带,自上而下分别是:Clarkina changxingensis yini带;Clarkina postwangi带;Clarkina changxingensis带。探讨了浙江长兴煤山标准剖面晚二叠世长兴组至殷坑组下部的牙形石生物带的划分,将这段地层划分为4个牙形石带,自上而下分别是:Clarkina meishanensis meishanensis带; Clarkina changxingensis yini-Clarkina meishanensis zhangi带;Clarkina postwangiClarkina subcarinata-Clarkina changxingensis组合带,而最下部的一个带又分为2个亚带,即上部的Clarkina changxingensis亚带和下部的Clarkina subcarinata-Clarkina wangi亚带。最后将铁石口剖面与煤山剖面进行了牙形石生物地层对比,认为铁石口剖面除了长兴组下部被第四纪河床覆盖之外,晚二叠世上部的地层可以完全与煤山剖面进行对比。  相似文献   

13.
Analysis of the International Geomagnetic Reference Field (IGRF) 1900-2000 shows that the Earth's main magnetic field has changed dramatically during the 20th century: its dipole moment has decreased by 6.5% since 1900, the strengths of its quadrupole and octupole have increased by 95% and 74%, respectively, four major planetary-scale magnetic anomalies on the Earth's surface have enhanced by 21%-56%, and the magnetic center has shifted 200 km towards the Pacific Ocean. These time-variation features are similar to the behavior before a geomagnetic polarity reversal.  相似文献   

14.
    
《科学通报(英文版)》1992,37(16):1376-1376
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15.
作者于1991~1995年对温州地区的淡水蛭类进行了调查研究,所得标本经鉴定共计淡水蛭类21种,隶属于13属、7科;经分析其区系属于中国-日本区,其中3种为我国特有种  相似文献   

16.
作者于1991~1995年对温州地区的淡水蛭类进行了调查研究,所得标本经鉴定共计淡水蛭类21种,隶属于13属、7科;经分析其区系属于中国-日本区,其中3种为我国特有种.  相似文献   

17.
    
Despite of the recent influx of reports describing important fossil specimens from the Mesozoic Jehol Biota, detailed information on the mechanism of fossilization and paleoenvironment in which these fossils were deposited is scanty. We present an analysis of microenvironment based upon scanning electron microscope observations of in situ pyrite framboids and microcrystallines of plant and vertebrate feather fossils in the Jehol Biota. Pyrite microcrystallines and framboids occur extensively inside and on surface of plant fossils.Framboids found on feathers and in sedimentary matrix were in a lower abundance. These framboids have diameters ranging from 6 μm to 31 μm with an average of 20 μm, indicating a dysoxic aqueous condition with free oxygen level less than 30 μmol/L for the microenvironment where these framboids were formed. The outgrowth of framboids inside plant tissues suggests the presence of water molecules and free oxygen at the cellular level during pyritization; the relative timing between tissue decay and framboid formation implies a rapid tissue degradation occurred during the very early stage of fossilization. This line of reasoning is consistent with the observation that cell level structure of plant fossils from these deposits is rarely preserved. We propose a \"fossil envelop\" model to accommodate the different geochemical conditions between the microenvironment surrounding the fossil material and the macroenvironment of background lake bottom water.  相似文献   

18.
    
《科学通报(英文版)》1991,36(2):135-135
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19.
本文研讨了岷江上游彻底关至映秀湾河段的水生无脊椎动物区系与生物量,分析了该河段中受引水式工程影响而出现的水库化与脱水河段,及与之相关的环境、水生无脊椎动物区系与生物量动态。  相似文献   

20.
通过求解多排分离式热管内部气-液两相流的动量微分方程,得出了内部压力分布规律,对沸腾段和凝结段内的传热机理进行了理论研究,给出了定量的结果,在实验基础上提出了一个预测多排分离式热管传热性能的数学模型,与实验结果比较表明,在预测传热性能是切实可行的。  相似文献   

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