GPS事后相位差分坐标解算模型及其相关问题的研究     

高成发 《测绘学报》2006,35(2):148-148

在GPS事后相位差分定位模式中,基线处理的数学模型和整周模糊度的正确解算直接影响了坐标成果所能达到的精度指标。以土地资源调查和交通工程测量为工程实际应用背景,重点对GPS事后RTK坐标解算模型、GPS外业观测时间的合理确定和GPS工程控制网投影变形的处理三个方面进行了较为深入的研究。观测值权的确定是基线坐标解算过程所遇到的主要技术难点之一,在分析常规定权方法的基础上提出了“高度角定权法”,并以某大型水电站的实测数据分析了三种定权方法对基线坐标解算结果精度的影响,数据结果清楚地表明本文提出的“高度角定权”能有…  相似文献   

The accumulation of radiocesium in coarse marine sediment: effects of mineralogy and organic matter   总被引：1，自引：0，他引：1  

Kim Y  Kim K  Kang HD  Kim W  Doh SH  Kim DS  Kim BK 《Marine pollution bulletin》2007,54(9):1341-1350

The controlling factors affecting the accumulation of (137)Cs in marine sediment have not been investigated in detail, especially in coarse grained sediment. Eighty eight coarse marine sediment samples near Wuljin, Korea, were characterized by quantitative X-ray-diffraction (XRD), gamma-ray, and total organic carbon (TOC) analysis. Those factors were then compared. The grain size was in the range of -0.48 to 3.6Mdphi corresponding to sand grains. TOC content was in the range of 0.06-1.75%, and the concentration of (137)Cs was 相似文献   

The Ashele VMS-type Cu-Zn Deposit in Xinjiang,NW China Formed in a Rifted Arc Setting     

Bo Wan  Lianchang Zhang  Peng Xiang 《Resource Geology》2010,60(2):150-164

The Ashele Cu-Zn deposit is a typical VMS deposit in Chinese Altay located in the southern margin of the Altaid orogen. The deposit occurred in the polyphase fold system, and the main orebody is located at the hinge of the syncline. All orebodies show lenticular form, and are stratabound by a suite of early to middle Devonian bimodal volcanic rocks. The hosting basalt is low K tholeiite and characterized with high Mg, Fe, Ca and low K, Ti. These basalts show flat REE pattern with Ce negative anomaly (Ce/Ce* 0.73–0.76). Niobium, Ta, Zr, Hf are depleted and Rb, Ba, Th, U, Sr, Pb are enriched with respect to the N-MORB. Both the Sr and Nd isotopes show depleted properties, while the (⁸⁷Sr/⁸⁶Sr)_i and the ε_Nd(t) range from 0.70469 to 0.70488 and 4.6 to 5.3, respectively. All geochemical and isotopic data from the hosting basalt show that it originates from an island arc source. We also report the S isotope data from the massive orebody, and δ³⁴S‰ change from 1.8‰ to 5.6‰. The S isotope data provide evidence that the sulfur originates from a mixing source between magma and seawater sulfate. We propose that the mafic magma provides the ore-forming metal and some percentage of sulfur, while it also acts as a heat engine which makes the fluids leach the metal from the underlying volcanic rocks. Combining the geological characteristics of the Ashele and geochemical data, and comparing with other Cu-Zn VMS deposits in the world, we propose that Ashele formed in a rifted arc setting.  相似文献   

Identification of Mineral Intensity along Drifts in the Dayingezhuang Deposit, Jiaodong Gold Province, China   总被引：2，自引：0，他引：2  

Li Wan  Qingfei Wang  Jun Deng  Qingjie Gong  Liqiang Yang    Huan Liu 《Resource Geology》2010,60(1):98-108

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Penglai Zircon Megacrysts: A Potential New Working Reference Material for Microbeam Determination of Hf–O Isotopes and U–Pb Age     

Xian-Hua Li  Weng-Guo Long  Qiu-Li Li  Yu Liu  Yong-Fei Zheng  Yue-Heng Yang  Kevin R. Chamberlain  De-Fang Wan  Cun-Hua Guo  Xuan-Ce Wang  Hua Tao 《Geostandards and Geoanalytical Research》2010,34(2):117-134

We introduce a potential new working reference material – natural zircon megacrysts from an Early Pliocene alkaline basalt (from Penglai, northern Hainan Island, southern China) – for the microbeam determination of O and Hf isotopes, and U–Pb age dating. The Penglai zircon megacrysts were found to be fairly homogeneous in Hf and O isotopes based on large numbers of measurements by LA-multiple collector (MC)-ICP-MS and SIMS, respectively. Precise determinations of O isotopes by isotope ratio mass spectrometry (IRMS) and Hf isotopes by solution MC-ICP-MS were in good agreement with the statistical mean of microbeam measurements. The mean δ¹⁸O value of 5.31 ± 0.10‰ (2s) by IRMS and the mean ¹⁷⁶Hf/¹⁷⁷Hf value of 0.282906 ± 0.0000010 (2s) by solution MC-ICP-MS are the best reference values for the Penglai zircons. SIMS and isotope dilution-TIMS measurements yielded consistent ²⁰⁶Pb/²³⁸U ages within analytical uncertainties, and the preferred ²⁰⁶Pb/²³⁸U age was found to be 4.4 ± 0.1 Ma (95% confidence interval). The young age and variably high common Pb content make the Penglai zircons unsuitable as a primary U–Pb age reference material for calibration of unknown samples by microbeam analysis; however, they can be used as a secondary working reference material for quality control of U–Pb age determination for young (particularly < 10 Ma) zircon samples.  相似文献   

Young (late Amazonian), near-surface, ground ice features near the equator, Athabasca Valles, Mars     

Devon M. Burr  Richard J. Soare  Jean-Michel Wan Bun Tseung 《Icarus》2005,178(1):56-73

A suite of four feature types in a ∼20 km² area near 10° N, 204° W in Athabasca Valles is interpreted to have resulted from near-surface ground ice. These features include mounds, conical forms with rimmed summit depressions, flatter irregularly-shaped forms with raised rims, and polygonal terrain. Based on morphology, size, and analogy to terrestrial ground ice forms, these Athabascan features are interpreted as pingos, collapsing pingos, pingo scars, and thermal contraction polygons, respectively. Thermal Infrared Mapping Spectrometer (THEMIS) data and geological features in the area are consistent with a sedimentary substrate underlying these features. These observations lead us to favor a ground ice interpretation, although we do not rule out volcanic and especially glaciofluvial hypotheses. The hypothesized ground ice that formed the mounds and rimmed features may have been emplaced via the deposition of saturated sediment during flooding; an alternative scenario invokes magmatically cycled groundwater. The ground ice implicit in the hypothesized thermal contraction polygons may have derived either from this flooding/ground water, or from atmospheric water vapor. The lack of obvious flood modification of the mounds and rimmed features indicates that they formed after the most recent flood inundated the area. Analogy with terrestrial pingos suggests that ground ice may be still extant within the positive relief mounds. As the water that flooded down Athabasca Valles emerged via a volcanotectonic fissure from a deep aquifer, any extant pingo ice may contain evidence of a deep subsurface biosphere.  相似文献   

A novel CFAR tonal detector using phase compensation     

Qing Wang Chun Ru Wan 《Oceanic Engineering, IEEE Journal of》2005,30(4):900-911

A novel tonal detector is presented in this paper. The detector uses phase compensation for detecting sinusoidal signal with unknown amplitude, frequency, and phase in complex Gaussian noise with unknown variance. We analyze the statistical properties of the discrete Fourier transform (DFT) of the observations and consider the leakage effect. Then we develop the detector by using generalized likelihood ratio test (GLRT). The new detector fully utilizes the phase information of the signal and achieves constant false alarm rate (CFAR) property. Theoretical analysis and simulation results show its improvement in detection performance.  相似文献   

Oil and Gas Distribution in Hailar Basin,Northeast China     

Yanbin Xu  Zishun Li  Ping Gao  Meng Tian  Xiuyun Qiao  Chuanbiao Wan 《世界地质(英文版)》2003,6(1)

Through petroleum exploration of 20 years, a new petroleum production area has been constructed in Hailar Basin. Their petroleum geological characteristics and hydrocarbon distribution has been known in detail. The Hailar Basin is a basin group consisted of many scattered sub-basins with similar structural developed history. Each sub-basin has unique hydrocarbon distributing rules, including (1) oil/gas reservoir distribution is controlled by the oil/gas sag, and the oil/gas bearing in big sag is rich; (2) underwater fan and turbidity fan are the most favorable reservoirs; structure zone controlled by main fault is favorable zone of forming composite oil/gas accumulation; (3) lower fault-block in higher rise and higher fault-block in lower rise are favorable to oil/gas accumulation; (4) deep fault and granite body are closely related to oil/gas reservoir, its distributing area is favorable area of oil and mantle source non-hydrocarbon gas formation;(5) higher geothermal area is favorable oil/gas bearing area.  相似文献   

Late Cenozoic deformation subsequence in northeastern margin of Tibet —Detrital AFT records from Linxia Basin     

Zheng  Dewen  Zhang  Peizhen  Wan  Jinglin  Li  Chuanyou  Cao  Jixiu 《中国科学:地球科学(英文版)》2003,46(2):266-275

Two events of Tibet uplifting are revealed by detrital apatite fission track (AFT) age data from Linxia Basin. They occurred at about 14 and 5.4-8.0 MaBP respectively. We interpret the first one to be related to the uplifting of the northern Tibet, which might have resulted from convectively removing the thickened lower lithosphere. The second one is a result of Laji Mountain uplifting. Numerous studies of the Tibetan Plateau suggest that the onset time of the deformation in the northeastern margin of Tibetan Plateau and the time of Tibet attaining to its present elevation is about 8 MaBP. They are approximately coincident with the uplift of Lajishan Mountain. It suggests that the northeastern margin of Tibet propagated northeastwardly to its present site in about 8 MaBP for accommodating the sustained convergence between India-Eurasia plate and for keeping its high elevation. The active block pattern dominating the strong earthquake distribution of Chinese continent probably formed at about 8.0-5.4 MaBP.

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长江中游临近预报业务系统 (MYNOS) 及其应用   总被引：1，自引：1，他引：0       下载免费PDF全文

万玉发  王志斌  张家国  吴翠红  吴涛  王珏 《应用气象学报》2013,24(4):504-512

针对长江中游强风暴天气特点和现代预报业务需求,在借鉴世界临近预报系统, 特别是美国的Auto-Nowcaster和WDSS-II以及英国的GANDOLF等先进经验的基础上,以我国多普勒天气雷达网为重要技术手段,结合数值预报等信息资源,于2007年研究建成长江中游临近预报业务系统 (MYNOS)。MYNOS主要技术方法包括:雷达与雨量计实时同步积分结合的降水估算方法 (RASIM),雷达反演参量与中尺度模式输出物理量相结合的强风暴性质自动识别和追踪技术,基于暴雨回波生命史特性约束下的多尺度合成降水量临近预报,基于数值预报模式和模糊逻辑学的强对流天气分类落区潜势预报,集GIS功能并整合各种定量监测与预警产品于一体的短时预报工作站。MYNOS已成为短时临近预报业务的支撑平台,其中实时生成的流域定量降水估算与临近预报、强对流天气分类潜势诊断与识别预警产品等成为日常预报业务的重要参考依据。  相似文献