数码相机标定参数对摄影测量精度的影响分析     

裴智惠  马浩 《全球定位系统》2011,36(2):49-51,64

数码相机的标定参数包括相机的内方位元素和各项镜头畸变差。从摄影测量的理论出发,通过空间前方交会试验,分析并统计了相机标定的各参数对摄影测量精度的影响。  相似文献   

浅谈数字正摄影像的制作技巧与心得     

林跃春  王睿 《测绘与空间地理信息》2011,34(1):109-111

数字正射影像图(DOM)是利用DEM对经过扫描处理的数字化航空像片或遥感数字影像(单色或彩色),经逐像元进行辐射改正、微分纠正和镶嵌,并按规定图幅范围裁剪生成的正射影像数据,并带有公里格网、图廓(内、外)整饰和注记的平面影像地图。DOM同时具有地图几何精度和影像特征的图像。具有信息丰富、形象逼真、获取快捷等优点,可作为地图分析背景控制信息,也可从中提取自然资源和社会经济发展的历史信息或最新信息,为城市规划等应用提供可靠依据。还可从中提取和派生新的信息,实现地图的修测更新。  相似文献   

太原基准地震台数字化形变观测仪器干扰源调查     

张建增  陈常俊  张亮娥  沈晓松  孟彩菊  曹文强  王新胜  何佳  周学文  李荣民  段运洁 《山西地震》2011,(2)

太原基准地震台数字化形变观测仪器伸缩仪和体应变仪记录的分钟值固体潮曲线上叠加有锯齿状的高频干扰,为探寻干扰源,对附近的抽水井、高压输电线、溶洞及煤矿进行调查分析,发现其对观测仪器的影响均不明显,认为与山洞下面可能存在的裂隙带有关。  相似文献   

青海省逐日地面气温数据不同插值方法的对比   总被引：3，自引：0，他引：3  

王思维  刘勇  朱超洪  蒋红 《高原气象》2011,30(6):1640-1646

为了探索适合地形复杂区青海省的逐日地区气温数据空间插值方法,利用2008年7月青海省48个地面气象观测站获取的逐日气温数据进行插值试验,首先通过对逐日气温值与对应的测站高程进行回归分析,将回归分析得到的气温垂直递减率与数字高程模型（Digital Elevation Model,DEM）该站的高度相乘,并与回归直线截距...  相似文献   

桂林布朗李花果期气象条件分析   总被引：2，自引：1，他引：1  

蒋珍姣  龙凤翔  李艳玉  陈桂莲 《气象研究与应用》2011,32(2):47-48,51

通过对桂林市布朗李花果期气象条件分析,得出影响桂林布朗李花果期主要气候特征,并提出相应的种植措施。  相似文献   

四川省广安市土地利用/覆盖遥感动态变化研究   总被引：1，自引：0，他引：1  

陈楠  杨武年  韩丽  李胤 《地理空间信息》2011,(6):96-98

随着社会工业化进程的加快,经济发展同生态环境之间的矛盾越来越突出,因此开展典型地区生态环境遥感动态监测分析是认识全国土地利用变化现状的重要途径。在遥感和GIS技术支持下,通过建立广安市土地利用数据库,对广安市2000-2007年间土地利用/覆盖类型的动态度变化和转移变化进行了分析,确定了土地利用/覆盖类型的初始状态矩阵...  相似文献   

西藏尕尔穷铜金矿金矿物特征研究   总被引：7，自引：0，他引：7  

姚晓峰 《地质与勘探》2011,47(6):1018-1025

尕尔穷铜金矿床是班公湖-怒江成矿带西段第一个达到详查程度的矽卡岩型铜金矿床。通过对矿床中金矿物的电子显微镜观察和扫描电镜能谱分析,查明了金矿物的类型及赋存状态,划分了成矿阶段。研究表明,金矿物有银-金矿物系列、铜-金矿物系列和少量碲化物类,主要有自然金、银金矿、金银矿、铜质金银矿、铜金矿、铜质银金矿和碲金银矿。金矿物主...  相似文献   

Estuarine deposition of a mid-Viséan tetrapod unit,Ducabrook Formation,central Queensland: implications for tetrapod dispersal     

K. E. Parker  J. A. Webb 《Australian Journal of Earth Sciences》2013,60(4):509-530

At Ducabrook property, central Queensland, the mid-Viséan Ducabrook Formation has yielded a diverse vertebrate fauna (fish and one tetrapod taxon) from a thin unit among siltstone interbedded with sandstone, minor oolitic limestone and conglomerate. Five lithofacies can be distinguished: the Oolitic Facies, distinguished by oolitic limestone and straight parallel ripple crests; the Sandy Facies, composed of plane-laminated and current-rippled sandstones; the Conglomeratic Facies, represented by pebble conglomerate displaying planar cross-bedded megaripples; the Silty Facies of siltstone with abundant calcrete nodules or sand/silt/clay interlaminations; and the Lime-Flake Facies, characterised by abundant locally derived lime flakes. The last includes the fossiliferous tetrapod unit. The Oolitic Facies was deposited in the inner (proximal) and outer (distal) zones of an estuary, based on identification of tidal sedimentary structures (e.g. mud drapes) and estuarine oolitic fabrics; the Lime-Flake Facies and Silty Facies were deposited in the estuary and lower reaches of a river and its surrounds; and the Sandy and Conglomeratic Facies represent braid-river deposits. Overall, the sequence represents intermittent deposition throughout an estuary, both within the tidal channel and the surrounding tidal flats, with additional deposition from the feeder river. The tetrapod unit, from the Lime-Flake Facies, represents a twin-peaked storm-induced flood event onto the tidal channel floor. The vertebrate bones have a shared taphonomic history and have undergone only local transport. The tetrapod and fish were spatially and temporally concurrent, probably in a shallow tidally influenced proximal estuarine habitat experiencing monsoonal conditions. Estuarine adaptations of these vertebrate taxa can explain migration along shallow-water continental shelves between the supercontinents during the Late Devonian and Early Carboniferous.  相似文献   

Digital Geological Mapping of Sinus Iridum Area of the Moon Based on the Chang’E-I Data     

DING Xiaozhong  HAN Kunying  PANG Jianfeng  WANG Liang  HAN Tonglin  JU Yuanjing  DING Weicui 《《地质学报》英文版》2013,87(6):1643-1657

Based on the CCD images,IIM data and DEM data of China＇s lunar exploration project （Chang＇E-Ⅰ） and related processed and analytic results,an integrated study of regional geology of Sinus Iridum and its adjacent area was conducted,and a series of relevant researches and analyses were carried out,including analysis of impact craters and their extrusive and accumulative materials,division of stratigraphic and tectonic units and classification of rock types,integrated analysis of chronology and lunar evolution history.In consideration of crater＇s shape features,quantity and preserving status of filling materials,the lunar impact craters can be divided into 7 types and 11 subtypes,and the accumulative materials of craters are divided into 6 types and 9 accumulative groups.According to the content and distribution of TiO2 and image characteristics,the basalts are divided into high-TiO2,medium-TiO2 and low-TiO2 basalts.Discussion was made on division of tectonic units and evolution features in the study area.The geological map of the Sinus Iridum Quadrangle （LQ-4） at a scale of 1∶2.5 M was preliminarily compiled with the ArcGIS system,and the spatial database of the map was established.Related technical specification,procedure and method for lunar geological mapping have been worked out,so as to lay a foundation for the forthcoming geological mapping of the global Moon in China by using the data of Chang＇E-Ⅱ and also for comprehensive study and geological mapping of other celestial bodies in the future.  相似文献   

福建“华安玉”岩石地球化学特征及成因研究     

李玉娟 《地质科学译丛》2013,(4):19-28

“华安玉”是福建省特有的玉石矿种,产于早三叠世溪口组新祠角岩段中,主要矿物为铁次透辉石,次要矿物为钾长石、石英和方解石等。地球化学分析表明,w（SiO2）变化范围为57．55％～66．46％,平均为60．69％,w（CaO）变化范围为9．88％～15．95％,平均为12．54%,相对低Si,Al而富Ca,Mg等;大离子亲石元素Sr,Ba及高场强元素Ti,Nb强烈亏损而具有明显的负异常,而Th、U、Nd、Hf表现为弱正异常,Pb正异常明显;∑REE变化范围较小,一般196．19×10^-6～241．77×10^-6,平均222．57×10^-6,轻重稀土比值（∑LREE／∑HREE）为3．60～4．59,平均为4．32,δEu=0．63～1．00,平均为0．81。微量元素和稀土元素特征曲线显示与大陆上地壳组成一致。新祠角岩形成于被动大陆边缘的潮坪泻湖环境,原岩主要是钙质粉砂岩、泥岩等,物源主要来自于闽北山地丘陵区的陆源改造型花岗质岩石。燕山期强烈的构造岩浆活动对其进行了多期热接触变质或交代作用,钙质粉砂岩、泥岩等经变质为透辉石角岩,形成优质的“华安玉”矿体。  相似文献