湖南益阳奥陶系五峰组—志留系周家溪群笔石     

黄莫  李明  杨振京  邓丽婷 《现代地质》2021,35(5):1343-1353

为响应国际地层委员会奥陶系分会的要求,实现扬子区与江南区奥陶纪晚期—志留纪早期生物地层精时对比,选取位于江南斜坡带的湖南益阳南坝剖面作为研究对象,对志留系底部Parakidograptus acuminatus带笔石进行了系统的研究。剖面内五峰组岩性为黑色页岩,与上覆周家溪群下组整合接触,地层连续无沉积间断。通过连续不间断采集笔石标本,在研究剖面共识别出笔石6属8种,包括:Parakidograptus acuminatus,Normalograptus elegantulus,Nor. mirnyensis,Metabolograptus persculptus,Neodiplograptus parajanus,Neo. guantangyuanensis,Petalithus hamus,Streptograptus cyclodontus。依据获取的笔石标本,初步识别出Metabolograptus persculptus带和Parakidograptus acuminatus带,确定研究剖面时代为晚奥陶世赫南特期—早志留世鲁丹期。  相似文献   

基于地球化学背景的多图幅系统误差校正——以区域地球化学调查数据Au元素为例   总被引：1，自引：0，他引：1  

戴慧敏  赵君  杨忠芳  宫传东  郑春颖  孙中任 《地球学报》2014,35(5):648-654

针对区域地球化学图件中出现的含量等值线环绕子区边界现象,以Au的多个图幅拼接为例,使用了分幅标准化法、衬度返回法及定和化法3种方法对地质大调查以来新方法获得的某成矿带区域地球化学数据进行系统误差校正,校正后编制地球化学等量线图显示,所采用的3种校正方法对于研究区数据存在的系统误差都不能达到较好的调平效果。针对研究区数据特点,尝试在分幅标准化法和衬度返回法基础上提出基于地球化学背景的误差校正方法,进一步对4种方法校正后数据参数特征及编制地球化学等量线图进行对比。基于地球化学背景的误差校正方法对研究区达到了较好的数据校正效果,并对校正前后数据进行相关对比和检验,满足化探数据中存在的系统误差属于线性误差这一基本假设,在实际应用中,可供地球化学数据系统误差校正灵活地使用,以取得更好的应用效果。  相似文献   

概率密度匹配法对中国区域卫星降水资料的改进   总被引：8，自引：2，他引：6       下载免费PDF全文

宇婧婧  沈艳  潘旸  赵平  周自江 《应用气象学报》2013,24(5):544-553

为考察概率密度匹配法 (PDF方法) 对中国区域卫星反演降水产品系统误差订正的适用性,基于逐日和逐时我国地面观测降水量资料,引入PDF方法,分别对逐日0.25°×0.25°水平分辨率和逐时0.1°×0.1°水平分辨率的CMORPH (Climate Prediction Center Morphing Technique) 卫星降水产品的系统误差进行订正。在分析CMORPH卫星降水产品误差特征的基础上,根据两种资料不同的时空分辨率和误差特点,调整概率密度匹配时选取样本的时间和空间范围,设计相应的订正方案。评估结果表明: PDF方法订正后, 两种分辨率卫星降水资料在中国区域系统误差均显著减小,达到了理想的订正效果。在我国站点稀疏的西部地区,订正后的CMORPH卫星降水产品仍保持卫星观测的降水空间分布,降水量也明显接近于地面观测降水量。可见,PDF方法是中国区域卫星反演降水产品系统误差订正的一种有效方法。  相似文献   

Land use structure optimization under systematic framework     

Liu Yanfang  Huang Liang 《地球空间信息科学学报》2013,16(3):46-52

This paper puts forward the concept of land use structure optimization under space-time coupling through analyzing the systematic characteristic of land use structure optimization. It mainly expounds the construction of land use structure optimization model at different levels. Lastly, this paper explains the practicableness of land use structure optimization under systematic framework through the example of Qionghai city.  相似文献   

强震区软弱破碎千枚岩隧道系统锚杆支护作用效果分析     

邹育麟  何川  周艺  汪波  许金华 《岩土力学》2013,34(7):2000-2008

以在建的穿越5•12强震区发震断裂带的广甘高速公路杜家山隧道为工程依托,选取20 m典型围岩区段为试验段,对有、无系统锚杆时的洞周位移、锚杆轴力、钢拱架内力、围岩与初支接触压力、及其二衬内力进行实测对比分析,探讨锚杆支护作用效果不明显的成因,提出了在强震区软弱破碎千枚岩隧道围岩中采用“钢喷”初期支护的支护方案。研究结果表明：设置锚杆的断面,其锚杆轴力值较小,最终洞周变形值及围岩与初支的接触压力值相对偏大,钢拱架和二衬的安全储备相对不足;锚杆的施工不仅在某种程度上加剧了对深部围岩的扰动,而且还延误了喷射混凝土和钢支撑支护对暴露围岩及时封闭的最佳时机;震后深部围岩的震裂损伤和震裂岩体地下水的渗透性增强,致使围岩松弛区域超过了锚杆设置范围,且锚杆与围岩间的黏结力被削弱。  相似文献   

New Schizolepis Fossils from the Early Cretaceous in Inner Mongolia, China and its Phylogenetic Position     

XU Xiaohui  LI Ruiyun  DONG Chong  WANG Qiujun  JIN Peihong  SUN Bainian 《《地质学报》英文版》2013,87(5):1250-1263

Three Schizolepis species collected from the Lower Cretaceous layer of the Huolinhe Basin,Inner Mongolia,China are described.These fossils are Schizolepis longipetiolus Xu XH et Sun BN sp.nov.,which is a new species,Schizolepis cf.heilongjiangensis Zheng et Zhang,and Schizolepis neimengensis Deng.The new species is a well-preserved female cone,slender and cylindrical in shape.The seed–scale complexes have long petioles and are arranged on the cone axis loosely and helically.The seed scales are divided into two lobes from the base.Each lobe is semicircular or elongate ligulate in shape,widest at the middle or the lower middle part,with an obtuse or bluntly pointed apex.The inner margin is almost straight and the outer margin is strongly arched.On the surface of the lobe,there are longitudinal and somewhat radial striations from the base to the margin.The seed is borne on the adaxial surface at the base or middle of each lobe.Schizolepis was established in 1847,and,although more than twenty species have been discovered and reported,its phylogenetic position is controversial because of the imperfection of fossils.Most authors have considered there to be a close evolutionary relationship between Schizolepis and extant Pinaceae.Here,we analyze characteristics and compare Schizolepis with Picea crassifolia Kom,which is morphologically most similar to Schizolepis.The results indicate that the genus probably has a distant evolutionary relationship with extant Pinaceae.A detailed statistical analysis of the global paleogeographic distribution of Schizolepis showed that all the fossils of this genus appeared in strata ranging from the Upper Triassic to the Lower Cretaceous in the North Hemisphere,being rare in the Upper Triassic and Lower Jurassic,but being very common from the Middle Jurassic to the Lower Cretaceous,and particularly abundant in the Lower Cretaceous.According to the statistical results,we speculate that the genus originated in Europe in the Late Triassic then spread from Europe to Asia between the Late Triassic and the Late Jurassic.In the Early Cretaceous most species existed in China’s three northeastern Provinces and the Inner Mongolia Autonomous Region and adjacent areas.Combining the paleogeographic distribution of the genus with ancient climatic factors,we deduced that Schizolepis began to decline and became extinct in the Early Cretaceous,and the reason for its extinction is closely related to the icehouse climate during the Early Cretaceous.  相似文献   

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田亮  段金梅  王强  赵亚平  乔亚明 《大地测量与地球动力学》2013,33(1):78-80

??????????GPS??SLR??VLBI?????????в????н??в???????????????????????????????似??????????????????????????????????????????????SLR??VLBI??????????????????????????????GPS?????????????7 mm ???????????GPS????????????????й??  相似文献   

High Precision Geoid Models HKGEOID-2000 for Hong Kong and SZGEOID-2000 for Shenzhen,China     

Zhicai Luo  Jinsheng Ning  Yongqi Chen  Zhanji Yang 《Marine Geodesy》2013,36(2):191-200

High precision geoid models HKGEOID-2000 for Hong Kong and SZGEOID-2000 for Shenzhen, China, have been developed with a hybrid approach of so-called sequential processing, using high precision GPS/leveling data, land and sea gravity anomalies, and digital terrain models. These two local geoid models have the same 1-km resolution. The estimated accuracy (external accuracy) is better than 1.7 cm for HKGEOID-2000 and 1.4 cm for SZGEOID-2000. Some common areas are covered by HKGEOID-2000 and SZGEOID-2000. So these two geoid models, along with high quality GPS/leveling data collected on the overlapping areas, can be used to detect the systematic bias between HKGEOID-2000 and SZGEOID-2000, as well as the difference between Hong Kong Principal Datum and 1956 yellow sea height datum of China, yielding RMS errors of 1.011 m and 1,003 m, respectively. Moreover, HKGEOID-2000, along with GPS ellipsoidal heights, is employed to determine the errors of the “orthometric heights” from purely trigonometric heighting, yielding an RMS error of 0.102 m. The combination of SZGEOID-2000 and GPS ellipsoidal heights has been used to replace the traditional spirit leveling and mapping, called GPS mapping.  相似文献   

Qualitative and Quantitative Description of Multibeam Echosounder Systematic Errors on Rocky Areas     

Nathalie Debese  Nicolas Seube  Laurent Heydel 《Marine Geodesy》2013,36(3):306-321

This paper deals with the problem of systematic depth errors made in surveying dumped rocks with multibeam echosounder. These errors may induce dangers for navigation in very shallow water areas or huge costs for coastal engineering contractors who perform rock dumping operation and surveying. We analyze results from four different multibeam echosounder systems and compare those data to a reference digital terrain model of a dumped rocks area obtained from a 3D terrestrial laser scanner. The systematic depth errors are statistically described and analysed on local areas. Finally, we propose a look-up table linking the error amplitude with the rock size, resulting from our error analysis.  相似文献   

青藏高原探空大气水汽偏差及订正方法研究   总被引：4，自引：1，他引：3  

梁宏  张人禾  刘晶淼  孙治安  李世奎 《大气科学》2012,36(4):795-810

水汽是大气的主要成分和降水的主要物质来源.青藏高原大气水汽分布对区域天气和气候有很大影响,为了探讨探空观测的大气水汽总量（R）资料的可靠性,本文以地基GPS遥感的大气水汽总量（G）为参照标准,对拉萨（1999~2010年）和那曲（2003年）的R进行对比分析和偏差（R-G）订正.结果表明:近10多年拉萨站R比G明显偏小,偏小程度随使用不同的探空仪而异.GZZ-2型机械探空仪和GTS-1型电子探空仪多年平均的PW偏差分别为-8.8%和-3.9%,随机误差分别为17.6%和13.6%.近10多年PW偏差变化呈减少趋势,这与探空仪性能改进有关.分析发现,青藏高原PW偏差具有明显季节变化和日变化特征,夏季比冬季明显,1200 UTC比0000 UTC明显.拉萨站GZZ-2型和GTS-1型探空仪在1200 UTC多年平均的PW偏差分别为-15.8%和-7.3%,在0000 UTC分别为-1.6%和-0.4%.那曲站GZZ-2型探空仪在1200 UTC和0000 UTC的PW偏差分别为-12.4%和-0.3%.分析还表明,太阳辐射加热与气温的日变化和季节变化是造成高原PW偏差日变化和季节变化的重要原因.据此,提出了高原PW偏差的订正方法,并以拉萨和那曲站为例进行PW偏差订正,订正后的PW系统偏差显著减少,随机误差也相应得到了改善.  相似文献