中国东海济舟岛南部春季水华的影响要素研究     

FU Dongyang  HUANG Zhaojun  ZHANG Yuanzhi  PAN Delu  DING Youzhu  LIU Dazhao  ZHANG Ying  MAO Zhihu  CHEN Jianfang 《海洋学报(英文版)》2015,34(3):51-58

A soil circulation occurs in the south of Cheju Island in the spring. Nutrients and its influence on chlorophyll a(Chl a) around the circulations were studied from April 9 to May 6, 2007. Spring bloom with elevated concentrations of Chl a was observed during the investigation. High concentrations of phosphate, nitrate and silicate at 0.6, 12, and 8 mmol/m3, respectively, were detected. A low water temperature prevented the growth of phytoplankton. Chl a concentrations in the study area might be strongly associated with the high silicate concentration.  相似文献   

RTK终端实时动态检测技术研究     

毛琪  潘树国  高旺  程良涛  张浩 《测绘工程》2015,(3):47-52

传统的RTK(实时动态定位)终端检测采用静态基线数据解算的方法,该检测方法与RTK终端实际动态应用场景不符,无法满足动态检测需要。通过研制高精度的车载导航基准设备和开发车载动态检测软件,同时解决车载设备数据的同步问题,提出基于车载移动平台的实时动态RTK终端检测技术。车载基准设备和待检测设备可以动态解算同源数据并实时上发结果,软件处理中心通过比对处理解算结果,对待检测设备进行检测评价。实验结果表明,设计所得的车载系统可稳定运行,并实现动态检测过程。同时,在良好的观测条件下,检测精度平面方向达到1cm,高程方向达到2cm,实现高精度实时动态检测的目的。  相似文献   

一种新的非差FCBs估计方法     

易文婷  陈亮  郭海林  毛勇 《测绘信息与工程》2015,40(3)

提出了一种新的非差FCBs估计方法,利用三角函数周期特性消除整周模糊度,避免了模糊度固定的难题.基于该方法,实现了PPP模糊度固定.实验结果表明,模糊度固定后,北、东、高程3个方向上的RMS分别从1.44 cm、3.37 cm、2.88 cm减小到0.75 cm、0.78 cm和2.06 cm,分别提高约47.8％、76.8％和28.5％.  相似文献   

一种基于横向或纵向扫描线处理的填洼算法     

刘永和  冯锦明  邵月红  徐精文 《测绘科学》2015,40(2):145-149

针对传统PlanchouDarbous算法采用递归执行方式导致处理效率低下等问题,该文提出了一种适合基于CUDA的GPU并行执行的DEM洼地填充算法。此算法采用淹没-排水思路,多次推进式扫描完成排水;在串行执行和并行执行两种方式下,算法处理有所差异,其中串行算法代码更短;串行算法的时间复杂度为O(n),测试结果表明串行执行时快于PlanchonDarboux算法,且在CUDA环境下的并行执行用时不到串行执行用时的一半。算法思路简单,易于编程实现。  相似文献   

核密度估计的道路匹配方法探讨     

邹丹  毛政元  李继红  刘小伶 《测绘科学》2015,40(7):104-108

针对目前地图合并技术的同名实体匹配中线实体(以道路为例)研究的不足,文章基于密度插值和DEM分析,提出一种针对线实体进行全局匹配的方法:采用积分的思想将核密度估计方法扩展应用于线实体密度计算,通过提取其密度谷脊线,将其应用于地图合并技术领域中的线实体匹配研究主题,指导相似度指标阈值的选取,并取得了较好的效果,为实现同一地区不同来源或不同比例尺(主要是相近比例尺)地图数据合并及数据库集成提供了参考。  相似文献   

一种基于主题爬行模式的地理信息分布式检索方法     

王小康  邓硕  吴博  李景文 《测绘与空间地理信息》2015,(4):96-97,101

当前网络中地理信息以几何形式递增,为了高效地从海量网络信息中检索出高质量的地理信息,本文提出了一种基于主题爬行的地理信息分布式检索方法。本文采用面向对象的方法将网络地理数据按照四元组的要求进行分解和组织,对地物实体的主题文本特征、地理空间特征、时间维特征等相关信息进行封装,建立四元组实体对象,实现了地理信息数据的相互集成与组织。引入MapReduce模式的并行处理机制完成对网页中地理信息数据的优化存储与索引,并且通过分别计算网页文本、地理文本与查询关键词的主题相关性对爬取的网页进行有序的排列,从而提供快捷、高效的地理信息主题查询。  相似文献   

原特提斯洋的俯冲、增生及闭合:阿尔金-祁连-柴北缘造山系早古生代增生/碰撞造山作用   总被引：20，自引：18，他引：2  

张建新  于胜尧  李云帅  喻星星  林宜慧  毛小红 《岩石学报》2015,31(12):3531-3554

分布在青藏高原北缘的阿尔金-祁连-柴北缘早古生代造山系被认为是原特提斯构造域最北部的构造拼合体。与其北侧具有长期增生历史的中亚造山系相比,特提斯造山拼合体被认为是各种来自冈瓦纳大陆北部大陆块体相互碰撞的产物。然而,与典型的阿尔卑斯和喜马拉雅碰撞造山带相比,阿尔金-祁连-柴北缘早古生代造山系包括有大量蛇绿岩、弧岩浆杂岩、俯冲-增生杂岩等,因此一些学者认为青藏高原北部的早古生代造山系为沿塔里木和华北克拉通边界向南逐渐增生的增生型造山带。但是,增生造山模式又很难解释南阿尔金-柴北缘地区普遍存在的与大陆俯冲有关的UHP变质岩、广泛分布的巴罗式变质作用和相关的岩浆作用,以及与碰撞造山有关的变形构造等。在本文中,通过对已有研究资料的综合总结,结合一些新的研究资料,我们提出在青藏高原东北缘的阿尔金-祁连-柴北缘造山系中,早古生代时期存在两种不同类型的造山作用,即增生和碰撞造山作用,其主要标志是北祁连-北阿尔金的HP/LT变质带、蛇绿混杂岩及与洋壳俯冲有关的构造岩浆作用,以及分布在柴北缘-南阿尔金与大陆俯冲和陆陆碰撞有关的UHP变质带、区域巴罗式变质作用、深熔作用、相关的岩浆活动及伸展垮塌作用等,并建立了一个反映原特提斯洋俯冲、增生、闭合及碰撞造山作用的构造模式。  相似文献   

西藏扎布耶盐湖铀源初探     

黄大友  王四利  毛建勋  徐伟  陈玉梁  刘志鹏 《铀矿地质》2015,(3):389-394

扎布耶盐湖蕴藏着丰富的矿产资源,具有超百万吨的锂矿资源。盐湖卤水中铀浓度亦很高,达到1818~3273μg·L-1,文章对该盐湖的地质背景及水中铀浓度概况进行了阐述,初步分析了其铀的来源。  相似文献   

东疆二叠纪镁铁-超镁铁岩体中辉石的成分特征及其对成岩和Ni-Cu成矿的指示   总被引：2，自引：2，他引：0  

薛胜超  秦克章  唐冬梅  毛亚晶  姚卓森 《岩石学报》2015,31(8):2175-2192

新疆东部早二叠世镁铁-超镁铁岩体主要分布在天山东段觉罗塔格构造带、中天山地块和北山地区,与这类岩体相关的Ni-Cu矿床主要产出在觉罗塔格带和中天山地区,北山目前并未发现典型Ni-Cu矿床。这些岩体中的斜方辉石主要为古铜辉石,少量为紫苏辉石;单斜辉石属透辉石、次透辉石或普通辉石。矿物成分系统变化显示橄榄石Fo值北山最高、觉罗塔格带到中天山逐次降低的特点,橄榄石Fo值在78~86和Ni含量低于1800×10-6范围内更有利于Cu-Ni成矿;斜方辉石En端元和单斜辉石Wo端元极差值也显示北山最高、觉罗塔格带和中天山较低的规律,且相对小的极差值更有利于成矿。单斜辉石AlⅣ/AlⅥ比值结果显示北山岩体在矿物结晶过程中压力较低,硫溶解度较大,可能是其矿化程度弱于觉罗塔格带和中天山的一个重要因素。觉罗塔格带、中天山和北山镁铁-超镁铁质岩体的母岩浆为非碱性系列、大陆拉斑玄武质岩浆。根据北山和觉罗塔格带岩体单斜辉石微量元素成分估算的母岩浆具有LREE富集以及Nb、Ta、Zr、Hf负异常的特征,指示出两者源区为受俯冲板片交代的地幔,且坡北源区俯冲交代程度更低。觉罗塔格带和中天山单斜辉石Alz vs.Ti显示裂谷堆晶趋势向弧堆晶趋势演化,而北山单斜辉石Alz vs.Ti则显示明显的裂谷堆晶趋势,这说明俯冲交代作用在觉罗塔格带和中天山地区表现的更为强烈。北山镁铁-超镁铁岩体中发现单斜辉石Ti的高异常及矿物温压计算结果显示,表明北山地区具有比觉罗塔格带和中天山更高的岩浆温度,这可能与塔里木二叠纪地幔柱的活动有关。  相似文献   

Ore-forming Fluid Characteristics of the Saishitang Cu-polymetallic Deposit in Qinghai Province, China     

LAI Jianqing  JU Peijiao  MAO Yin  AN Jianghu  WANG Xiongjun 《《地质学报》英文版》2015,89(2):485-504

Saishitang Cu-polymetallic deposit is located in the southeast section of Late Paleozoic arcfold in the southeastern margin of Qaidam platform. Accoring to the geological process of the deposit,four mineralization episodes were identified: melt/fluid coexisting period(O),skarn period(A),first sulfide period(B) and second sulfide period(C),and 10 stages were finally subdivided. Three types of inclusions were classified in seven stages,namely crystal bearing inclusions(type I),aqueous inclusions(type II) and pure liquid inclusions(type III). Type I and II inclusions were observed in stage O1,having homogenization temperature from 252 to 431°C,and salinities ranging from 24.3% to 48.0%. Type I inclusion was present in stage A1,having homogenization temperature from 506 to 548°C,and salinities ranging from 39.4% to 44.6%. In stage B1,type II and III inclusions were observed,with homogenization temperature concentrating between 300–400°C,and salinities from 0.4% to 4.3%. Type II inclusions were present in stage B2,with homogenization temperature varying from 403 to 550°C. In stage C1,type I and II inclusion commonly coexisted,and constituted a boiling inclusion group,having homogenization temperatures at 187–463°C,and salinities in a range of 29.4%–46.8% and 2.2%–11.0%. Type II and III inclusions were developed in stage C2,having homogenization temperature at 124–350°C,and salinities ranging between 1.6% and 15.4%. In stage C3,type II and III inclusions were presented,with a homogenization temperature range of 164–360°C,and salinities varying from 4.0% to 11.0%. The results of micro-thermal analysis show that fluids are characterized by high temperature and high salinity in stage O1 and A1,and experienced slight decrease in temperature and dramatic decrease in salinity in stage B1 and B2. In stage C1,the salinity of fluid increased greatly and a further decrease of temperature and salinity occurred in stage C2 and C3. Fluids boiled in stage C1. With calculated pressure of 22 MPa from the trapping temperature of 284–289°C,a mineralization depth of 2.2 km was inferred. Results of Laser Raman Spectroscopy show high density of H2 O,CH4 and CO2 were found as gas composition. H-O isotope study indicates the oreforming fluids were the mixture of magmatic water and meteoric water. Physicochemical parameters of fluids show oxygen and sulfur fugacity experienced a decrease,and redox state is weakly reducing. Along with fluid evolution,oxidation has increased slightly. Comprehensive analysis shows that melt exsolution occurred during the formation of quartz diorite and that metal elements existed and migrated in the form of chlorine complex. Immiscible fluid separation and boiling widely occurred after addition of new fluids,bringing about dissociation of chlorine-complex,resulting in a great deal of copper precipitation. In conclusion,Saishitang deposit,controlled by regional tectonics,is formed by metasomatism between highly fractionated mineralization rock body and wall rock,and belongs to banded skarn Cu-polymetallic deposit.  相似文献