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1.
对野外GPS常要设置的参数DX、DY、DZ、DA、DF与大地坐标(一种二维平面坐标)有区别,GPS所用的WGS84坐标系与我们国家常用的北京54和西安80坐标系所使用椭球体参数有差异,正是由于不同椭球的差异才需要求DX、DY、DZ、DA、DF等参数.利用先进的QT编程技术,将其嵌入到Microsoft visual C...  相似文献   

2.
手持GPS是目前地质工作中常用的工具,具有导航方便,高效率等特点。通过Gamin系列手持GPS自带的Map Source软件,可以快速求取空间平移参量DX、DY、DZ,并将物探测点编辑成测线放置在Google Earth软件中查看,提高工作效率。  相似文献   

3.
浅谈手持GPS在地质矿区勘查中的应用   总被引:1,自引:0,他引:1  
宋全福 《吉林地质》2014,(3):126-128
手持GPS未经参数校正时定位精度为80~120 m,利用测量控制点进行参数校正后定位精度可提高至5 m以内,在地质勘查中熟练运用手持GPS将大大提高野外工作效率。  相似文献   

4.
手持式GPS测量在地质勘查中的应用   总被引:14,自引:3,他引:14  
在小比例尺地质测量中,用GPS单点绝对定位技术测定地质点,减少了控制测量环节,降低了成本,因此GPS绝对定位在地质工程测量中仍然有应用的前景,但是,定位时必须做到:(1)合理选取校正的控制点;(2)正确校正参数;(3)定期和不定期检测仪器;(4)保证仪器的高度角和有效工作时间。该方法应用在某地质工程测量中,实测面积60km^3。经传统高精度直测检查验收证明中提出的方法完全可以用于生产实践。  相似文献   

5.
在我国东部平原地区,新近系的厚度变化较大,对下部煤层反射波的准确成像产生巨大影响。致使地震解释出现煤层深度误差大、假向斜、假背斜及断层位置严重偏离等问题。通过模拟新近系起伏变化对深部目的层反射波的正演,发现目的层反射波随上覆低速层的起伏而起伏,其中断点的绕射波特征也随之出现较大变化,对此进行常规叠后偏移易出现成像失真。对此采取分时校正方法,计算出不同赋存深度条件下的煤层反射波校正量曲线.将获得的校正量运用叠后偏移处理,能较好地消除深部同相轴不正常的凹凸现象,实现对目的层构造及其形态的正确成像。济宁二号井八采区的实例证明,分时校正后的叠后偏移方法可有效消除新生界横向起伏变化对深部目的层准确成像的影响。  相似文献   

6.
手持式GPS在化探工作中的应用   总被引:1,自引:0,他引:1  
陈立文  安兴 《西北地质》2012,(2):151-156
主要论述在化探预查和普查阶段使用手持式GPS,实现了单点绝对定位,很大程度上提高了野外定点的精度,降低了工作强度,简化了工作程序,保证了工作质量。GPS在化探工作中的使用必须按照必要程序进行,为保证精度,必须进行GPS试验,主要包括控制点的选择,仪器参数校正,精度试验,多台GPS一致性检查,并明确给出该地区GPS能否使用报告。通过野外实例充分说明了利用手持式GPS的定位方法在地球化学勘查中应用的效果,利用GPS航迹跟踪功能验收当天野外工作,制作航迹监控图、野外实际材料图,利用GPS和MAPGIS制作地质简图及化探测网的布设。重点讨论了GPS有关参数的设定、校正及准确度等细节,从而保证地球化学勘查测点定点的精度和质量。  相似文献   

7.
笔者在黔西南某地金矿的地质调查中通过对手持GPS的运用实践,总结出应用技术路线。认为正确设置和采集原始点坐标,并计算调查区的校正参数是关键,验证误差评价不可少,乃是精度的保证、应用的基础。利用已知点校正时,原始点数据采集要点是正确设置对应坐标系统的目标椭球,投影设为测区对应的中央子午线,其它参数选项卡全关闭,同时,采集原始点数据时,最好为10次及以上平滑方式、差分3D状态下采集。在调查区实践中,坐标转换方法使用经典的"一步法",计算得到四参数及校正参数数据,并应用于项目工程,用其它已知点验证,其平均偏差为±2.9 m,精度较高,完全符合地质勘查规范的要求。经过参数校正后的手持GPS,完全可以取代地形图人工定点。米级带SBAS功能多星机型实际精度接近亚米级的单星机型,支持多星的手持机定位快,精度高,因此,笔者建议今后使用多星和SBAS定位技术的GPS,以期取得事半功倍的效果。  相似文献   

8.
在矿区初步勘查阶段,由于缺乏大比例尺地形图来设计勘探线时,会经常利用罗盘和GPS进行勘探线剖面实测,但这种测量往往造成与设计有所偏离,针对勘探线剖面测量数据偏离,拟建立一种平面几何方法进行校正.通过分段偏离角(α),利用三角正弦函数、余弦函数对矿区勘探线剖面简易测量数据进行校正,实践证明,该偏离校正是一种行之有效的方法.  相似文献   

9.
精密单点定位技术具有无需控制点、单台GPS接收机静态测量可获得高精度的坐标成果等优点,在青藏高原等困难地区的物探测量实践中具有广阔的应用前景。本文以利用精密单点定位技术处理青藏高原西部和东部的两个1∶25万区域重力调查项目形成的控制点观测数据为基础,经过计算对比这些点的精密单点定位成果和传统测量平差方法所得的CGCS2000坐标成果之间的差值,分析误差来源,得出误差的主要来源是两者坐标值在历元和框架差异引起,进而通过历元和框架校正得出控制点的CGCS2000坐标,重新对比发现校正后的坐标值具有与传统测量平差坐标值相一致的精度,在此基础上提出了在实际物探测量中利用精密单点定位技术得到CGCS2000坐标成果的思路和注意事项,同时讨论了该方法的应用范围。  相似文献   

10.
潜在蒸散发量估算方法在河南省的适用性分析   总被引:2,自引:0,他引:2       下载免费PDF全文
邹磊  夏军  马细霞  曾思栋 《水文》2014,34(3):17-23
利用FAO56-PM法计算潜在蒸散发时气象资料往往不易满足。针对该问题,本文研究了辐射法、温度法和基于温度及辐射资料的RBF神经网络预测模型。以FAO56-PM法计算值为标准,比较分析了Priestley-Taylor法、Hargreaves法、Mc Cloud法以及Makkink法在河南省五个典型地区(安阳、新乡、郑州、驻马店、信阳)的适用效果。并以新乡地区为例评价了校正参数后各估算方法和基于温度及辐射资料的RBF神经网络预测模型的适用性。结果表明,Makkink法在五个典型地区估算的潜在蒸散发量误差较小,其余方法误差较大。校正参数后,各估算方法在新乡地区的估算结果均得到明显改进,具有较好的地区适用性。基于温度及辐射资料的RBF神经网络预测模型具有较高的预测精度,可应用于潜在蒸散发量的估算和预测。  相似文献   

11.
Pant-y-ffynnon Quarry in South Wales yielded a rich cache of fossils in the early 1950s, including articulated specimens of new species (the small sauropodomorph dinosaur Pantydraco caducus and the crocodylomorph Terrestrisuchus gracilis), but no substantial study of the wider fauna of the Pant-y-ffynnon fissure systems has been published. Here, our overview of existing specimens, a few described but mostly undescribed, as well as freshly processed material, provides a comprehensive picture of the Pant-y-ffynnon palaeo-island of the Late Triassic. This was an island with a relatively impoverished fauna dominated by small clevosaurs (rhynchocephalians), including a new species, Clevosaurus cambrica, described here from a partially articulated specimen and isolated bones. The new species has a dental morphology that is intermediate between the Late Triassic Clevosaurus hudsoni, from Cromhall Quarry to the east, and the younger C. convallis from Pant Quarry to the west, suggesting adaptive radiation of clevosaurs in the palaeo-archipelago. The larger reptiles on the palaeo-island do not exceed 1.5?m in length, including a small carnivorous crocodylomorph, Terrestrisuchus, and a possible example of insular dwarfism in the basal dinosaur Pantydraco.  相似文献   

12.
Robert L. Linnen   《Lithos》2005,80(1-4):267-280
The solubilities of columbite, tantalite, wolframite, rutile, zircon and hafnon were determined as a function of the water contents in peralkaline and subaluminous granite melts. All experiments were conducted at 1035 °C and 2 kbar and the water contents of the melts ranged from nominally dry to approximately 6 wt.% H2O. Accessory phase solubilities are not affected by the water content of the peralkaline melt. By contrast, solubilities are affected by the water content of the subaluminous melt, where the solubilities of all the accessory phases examined increase with the water content of the melt, up to 2 wt.% H2O. At higher water contents, solubilities are nearly constant. It can be concluded that water is not an important control of accessory phase solubility, although the water content will affect diffusivities of components in the melt, thus whether or not accessory phases will be present as restite material. The solubility behaviour in the subaluminous and peralkaline melts supports previous spectroscopic studies, which have observed differences in the coordination of high field strength elements in dry vs. wet subaluminous granitic glasses, but not for peralkaline granitic glasses. Lastly, the fact that wolframite solubility increases with increasing water content in the subaluminous melt suggests that tungsten dissolved as a hexavalent species.  相似文献   

13.
Calcite samples were extracted both from the rock matrix and the superficial coating of a karstified fault plane of an underground quarry, located in the eastern border of the Paris basin. The karstification is dated as Quaternary. Analysis of mechanical calcite twinning reveals that only the calcite matrix has also undergone a compression trending WNW that can be attributed to the Mio-Pliocene alpine collision. Both coating and matrix have undergone a strike-slip regime with σ1 roughly trending north–south, that could correspond to the regional present-day state of stress, a strike-slip compression rather trending NNW, modified by local phenomena. To cite this article: M. Rocher et al., C. R. Geoscience 335 (2003).  相似文献   

14.
HYDROGEOLOGY     
正20141756 Chen Ruige(Mathematical College,China University of Geosciences,Beijing100083,China);Zhou Xun Numerical Simulation of Groundwater Level Fluctuation in a Coastal Confined Aquifer with Sloping Initial Groundwater Level Induced by the Tide(Geological Bulletin of China,ISSN1671-2552,CN11-4648/P,32(7),2013,p.1099-1104,6 illus.,16 refs.) Key words:confined water,groundwater level  相似文献   

15.
正20141408 Cai Jia(Institute of Geology,Chinese Academy of Geological Sciences,Beijing100037,China);Liu Fulai Petrogenesis and Metamorphic P-T Conditions of Garnet-Spinel-Biotitebearing Paragneiss in Danangou Area,Daqingshan-Wulashan Metamorphic Complex Belt(Acta Petrologica Sinica,ISSN1000-0569,CN11-1922/P,29(7),  相似文献   

16.
17.
正20142386An Guoying(China Aero Geophysical Survey and Remote Sensing Center for Land and Resources,Beijing 100083,China)Application of Satellite Remote Sensing in Regional Hydrogeological Investigation:Taking Cenozoic Strata in Wenquan Sheet(1∶250 000)of Karakoram Range as an Example(Geosci-  相似文献   

18.
正20141016An Chengbang(Key Laboratory of Western China’s Environmental Systems,Ministry of Education,Lanzhou University,Lanzhou 730000,China);Zhao Yongtao Lake Records during the Last Glacial Maximum from Xinjiang,NW China and Their Climatic Impli-  相似文献   

19.
正20141538 Cao Qing(School of Earth Sciences and Engineering,Xi’an Petroleum University,Xi’an 710065,China);Zhao Jingzhou Characteristics and Significance of Fluid Inclusions from Majiagou Formation,Yichuan Huangling Area,Ordos Basin(Advances in Earth Science,ISSN1001-8166,CN62-1091/P,28(7),2013,p.819-828,7 illus.,3 tables,43 refs.)  相似文献   

20.
GEOCHEMISTRY     
正20142002 Wei Hualing(Institute of Geophysical and Geochemical Exploration,Chinese Academy of Geological Sciences,Langfang065000,China);Zhou Guohua Element Content and Mineral Compositions in Different Sizes of Soil in Tongling Area,Anhui Province(Geological Bulletin of China,ISSN1671-2552,CN11-4648/P,32(11),2013,p.1861  相似文献   

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