内蒙古赤峰北部二叠纪基性-中性次火山岩系地球化学特征   总被引：2，自引：0，他引：2  

王友  宫玉亚 《地质通报》2000,19(2):131-136

赤峰北部早二叠世末至晚二叠世初基性—中性次火山岩锆石U Pb和谐线年龄为 (2 76 .3±4 .2 )Ma ,岩石组合为玄武岩、玄武安山岩及安山岩等。岩石化学上属亚碱性系列、钙碱性火山岩系、钠质类型 ;稀土总量中低 ,属轻稀土富集型 ,稀土分布模式为右倾平滑曲线或略有正、负铕异常 ;过渡族元素球粒陨石标准化曲线形态呈“W”型 ,锶初始值为 0 .70 5398,反映物质来源较深。该火山岩系形成于华力西中期强烈造山后均衡调整阶段的引张构造环境。  相似文献   

热带测雨卫星综合探测结果之"云娜"台风降水云与非降水云特征   总被引：18，自引：4，他引：18  

傅云飞刘栋  王雨宇如聪  徐幼平程锐 《气象学报》2007,65(3):316-328

为了解降水云与非降水云相应的微波信号、云水、雨水及潜热特征,文中利用热带测雨卫星搭载的测雨雷达、微波成像仪及红外辐射计探测的匹配融合结果,就2004年8月“云娜”台风进行了个例分析研究。结果表明:“云娜”台风过程中深厚降水云占79%,中云和低云降水仅分别占10.6%和10.4%;非降水低云所占比例最大(45.5%),高云其次(34.1%)。降水云中大粒子居多,非降水云粒子有效半径分布宽。深厚降水云中冰、水含量成正比;中等厚度降水云中的冰含量相对稳定,但液态水含量变化大;深厚和中等厚度非降水云中的冰、水含量皆成反比。对降水率、气柱潜热、气柱云水和云冰沿台风径向分布的分析结果发现,台风生成前的低压中心附近降水率和气柱总潜热比随后时次均大,表明降水释放潜热对“云娜”台风的形成起到了非常重要的作用;在台风形成后,降水率和气柱总潜热自台风云墙向外减小;随着台风的成熟,降水率和气柱总潜热沿台风径向分布趋于稳定。潜热廓线分析表明,深厚降水云潜热释放在对流层中上部(3 km以上),最大潜热高度约4.5 km。对降水云和非降水云的冰、水含量平均垂直廓线分析表明,深厚和中等厚度的降水云中水粒子含量具有相似的平均廓线,最大值(约0.03 g/m3)位于4—5 km高度,降水低云中的水粒子含量最大值(约0.07 g/m3)位于4 km高度;对于非降水云,3种不同高度的潜热廓线、水和冰粒子含量廓线相似,反映了TRMM反演算法对这些参数的反演仍存在缺陷。  相似文献   

黄土滑坡发育特征参数的幂律相依性研究          下载免费PDF全文

田尤  杨为民  李浩 《水文地质工程地质》2018,(3):131-137

以天水市麦积区幅为例,利用最小二乘法的拟合方法,对黄土滑坡发育特征参数的幂律相依性进行了研究。结果表明:(1)滑坡-累积频率的幂律相依性不仅存在于滑坡面积-累积频率、体积-累积频率间,还存在于滑坡后缘距离分水岭高程与其发生的累积频率之间;(2)滑坡规模参数幂指数分布特征为面积与长度＞面积与宽度＞体积与面积;运动特征参数幂指数的分布特征为体积与最大垂直滑动距离＞体积与最大水平滑动距离＞面积与最大垂直滑动距离＞面积与最大水平滑动距离;(3)滑坡的等效摩擦系数与滑坡面积、体积的幂函数相关性差,故而该经验关系式仅能代表趋势特征,不能作为定量分析的依据。  相似文献   

滇中川街盆地中侏罗世弓鲛(软骨鱼类)化石新材料     

孙柏东  王伟  刘军平  宋冬虎  吕勃烨  徐云飞  王璐 《地质通报》2018,37(11):1991-1996

云南禄丰县川街盆地中侏罗统产出弓鲛鱼类化石后甸弓鲛(Hybodus houtienensis Young)、新庄弓鲛(新种)(Hybodus xinzhuangensis Sun)、川街弓鲛(新种)(Hybodus chuanjieensis Sun)。后甸弓鲛(Hybodus houtienensis Young)是中国发现最早的弓鲛鱼类之一,正型标本为破碎的鳍棘,副型标本为一枚牙齿齿冠。依据在川街盆地相同层位发现的新化石材料,对后甸弓鲛副型标本进行了增补,补充了描述,建立了2个弓鲛新种:新庄弓鲛与川街弓鲛,丰富了"后甸弓鲛带"弓鲛类群,并讨论了弓鲛属的生物地层、生活的古环境和地理分布特征。  相似文献   

Bayesian Markov Chain Random Field Cosimulation for Improving Land Cover Classification Accuracy   总被引：2，自引：0，他引：2  

Weidong Li  Chuanrong Zhang  Michael R. Willig  Dipak K. Dey  Guiling Wang  Liangzhi You 《Mathematical Geosciences》2015,47(2):123-148

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建筑物群集对象的改进型棱柱模型表达     

霍志敏  史云飞  张玲玲  聂庆微  吕春光  孙华生 《测绘科学》2021,46(10):137-144

针对B-Rep模型表达建筑物群集对象存在数据量大、更新和维护困难等问题,该文提出了一种专用于建筑物群集对象表达的改进型棱柱模型.该模型对原始棱柱模型进行改进,改进后的模型由棱柱和基底组成,且棱柱的上、下边界由一到多个表面构成.进一步提出了基于改进型棱柱模型的群集对象构建方法,该方法通过接合图生成、内部点提取和点投影生成建筑物群集对象的三维模型.试验结果表明,在不需要侧面信息情况下,改进型棱柱模型可以代替B-Rep表达群集对象,并且随着群集对象房间数的增大,比B-Rep更加节约存储空间.  相似文献   

Effects of UV-B radiation on tetraspores of Chondrus ocellatus Holm (Rhodophyta), and effects of red and blue light on repair of UV-B-induced damage     

鞠青  肖慧  王悠  唐学玺 《中国海洋湖沼学报》2015,33(3):650-663

We evaluated the effects of red and blue light on the repair of UV-B radiation-induced damage in tetraspores of Chondrus ocellatus Holm. Tetraspores of C. ocellatus were treated with different UV-B radiation levels(0,36,72,108,144 and 180 J/m2),and thereafter subjected to PAR,darkness,or red or blue light during a 2-h repair stage,each day for 48 days. The diameters and cellular contents of cyclobutane pyrimidine dimmers(CPDs),chlorophyll a(Chl a),phycoerythrin,and UV-B-absorbing mycosporinelike amino acids(MAAs) contents of the tetraspores were determined. Our results show that low doses of UV-B radiation(36 and 72 J/m 2) promoted the growth of C. ocellatus; however,increased UV-B radiation gradually reduced the C. ocellatus growth(greater than 72 J/m2). The MAAs(palythine and asterina-330) in C. ocellatus were detected and analyzed by LC/MS. Our results suggest that moderate red light could induce the growth of this alga in aquaculture. In addition,photorepair was inhibited by red light,so there may be some other DNA repair mechanism activated by red light. Blue light promoted the activity of DNA photolyase,greatly improving remediation efficiency. Red and blue lights were found to reduce the capacity of C. ocellatus to form MAAs. Therefore,PAR,red light,and blue light play different roles during the repair processes for damage induced by UV-B radiation.  相似文献   

NIST RM 8301 Boron Isotopes in Marine Carbonate (Simulated Coral and Foraminifera Solutions): Inter‐laboratory δ11B and Trace Element Ratio Value Assignment     

Joseph A. Stewart  Steven J. Christopher  John R. Kucklick  Louise Bordier  Thomas B. Chalk  Arnaud Dapoigny  Eric Douville  Gavin L. Foster  William R. Gray  Rosanna Greenop  Marcus Gutjahr  Freya Hemsing  Michael J. Henehan  Philip Holdship  Yu‐Te Hsieh  Ana Kolevica  Yen‐Po Lin  Elaine M. Mawbey  James W. B. Rae  Laura F. Robinson  Rachael Shuttleworth  Chen‐Feng You  Shuang Zhang  Russell D. Day 《Geostandards and Geoanalytical Research》2021,45(1):77-96

The boron isotopic ratio of ¹¹B/¹⁰B (δ¹¹B_SRM951) and trace element composition of marine carbonates are key proxies for understanding carbon cycling (pH) and palaeoceanographic change. However, method validation and comparability of results between laboratories requires carbonate reference materials. Here, we report results of an inter‐laboratory comparison study to both assign δ¹¹B_SRM951 and trace element compositions to new synthetic marine carbonate reference materials (RMs), NIST RM 8301 (Coral) and NIST RM 8301 (Foram) and to assess the variance of data among laboratories. Non‐certified reference values and expanded 95% uncertainties for δ¹¹B_SRM951 in NIST RM 8301 (Coral) (+24.17‰ ± 0.18‰) and NIST RM 8301 (Foram) (+14.51‰ ± 0.17‰) solutions were assigned by consensus approach using inter‐laboratory data. Differences reported among laboratories were considerably smaller than some previous inter‐laboratory comparisons, yet discrepancies could still lead to large differences in calculated seawater pH. Similarly, variability in reported trace element information among laboratories (e.g., Mg/Ca ± 5% RSD) was often greater than within a single laboratory (e.g., Mg/Ca < 2%). Such differences potentially alter proxy‐reconstructed seawater temperature by more than 2 °C. These now well‐characterised solutions are useful reference materials to help the palaeoceanographic community build a comprehensive view of past ocean changes.  相似文献   

Fast estimation method of volumes of landslide deposit by the 3D reconstruction of smartphone images     

Fu  Lin  Zhu  Jun  Li  Wei-lian  You  Ji-gang  Hua  Zhang-yu 《Landslides》2021,18(9):3269-3278

The fast estimation of volumes of landslide deposit has great significance for emergency rescue decision-making, such as deposit filling and excavation and road dredging. The existing methods for the volumes of landslide deposit estimation have the disadvantages of a long data acquisition cycle, poor timeliness and high cost. Therefore, this paper researches a fast estimation method of volumes of landslide deposit based on the 3D reconstruction of smartphone images. First, the improved algorithms of speeded up robust features (SURF) and oriented fast and rotated brief (ORB) algorithms are combined to realize the fast matching of landslide feature points. Second, the 3D scene sparse reconstruction of landslide deposit is realized through boundary constraints. Third, taking the steepest gradient into account, the interpolation of the bottom of the landslide deposit and the fast estimation of the volumes are carried out. Finally, a prototype system is developed, and a case study is performed. The experimental results show that the estimation results of the proposed method are between those of the commercial software ContextCapture, Metashape and Pix4Dmapper, which are commonly used in the field of 3D reconstruction, but the estimation speed is 1–2 times faster than that of the commercial software mentioned above. The proposed method can realize the low-cost and fast estimation of landslide deposit volumes and provide technical support for landslide emergency rescue.

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湖北宜昌第四纪沉积物中铁质重矿物特征对三峡贯通的指示^*     

由文智  向芳  杨坤美  姜月华  喻显涛  李磊 《古地理学报》2021,23(4):855-870

长江三峡的演化问题一直是地学界争论的焦点和热点。近年来,不少学者通过锆石、石榴子石、角闪石等重矿物的同位素和微量元素组成来判断长江物源,取得了较好的成果,但将单颗粒铁质重矿物作为物源指示矿物并应用于三峡贯通方面研究较少。因此作者运用电子探针、扫描电镜和能谱仪对湖北宜昌地区第四纪沉积物中的铁质重矿物进行化学特征和形貌分析,并与可能的物源区样品进行对比,来分析物源演化过程及判定三峡贯通时间。研究结果显示,宜昌地区第四纪沉积铁质重矿物的主要源岩为位于三峡以西的攀枝花钒钛磁铁矿、峨眉山玄武岩和位于三峡以东的黄陵花岗岩,在善溪窑组沉积结束以后,宜昌地区第四纪沉积物的物源发生了明显改变,出现来自三峡以西的物质,表明长江三峡此时发生了贯通。结合ESR测年数据和前人研究结果可知,长江三峡的贯通发生在0.75—0.73Ma B.P.。  相似文献