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81.
以《中国留学人员创业年鉴》为基础数据,采用GIS空间分析技术,运用核密度估计法、L函数和最近邻层次聚类分析等方法,分析2006~2015年中国留学人员创业园空间分布规律以及园区产业集聚特征,结果表明:中国留学人员创业园集聚特征显著,而且随着时间的推移,其多中心趋势明显,集聚规模迅速增大,集聚强度呈“先升后降,但总体增大”趋势;主要集聚于长三角、京津冀和珠三角等地区,尤以前两者最显著,且三大集聚区的集聚强度与集聚规模差异明显,其中长三角留创园的集聚规模最大,京津冀集聚强度最高,而珠三角则比较复杂,其在很小空间尺度范围内服从集聚分布,而在较大空间尺度范围内则服从随机分布;基于不同主导产业的中国留学人员创业园依然集中于长三角、京津冀和珠三角等地区,其主导产业分布格局则差异显著,规律性不强。 相似文献
82.
Bin Chen 《Geochimica et cosmochimica acta》2005,69(22):5387-5388
83.
On the basis of simplification of the Planck function in a low temperature range, this paper revises the practical split-window algorithm and presents a method for retrieving snow surface temperature (Ts) based on MODIS data in the middle-latitude region. The application of this method in Qinghai Lake region reveals that it is feasible for the retrieval of Ts. Results of correlation analysis indicate that there was strong negative relationship between Ts and altitude. By analyzing three typical areas in which land cover was relatively homogenous, this paper discusses the relationship between Ts and normalized difference snow index (NDSI) and then presents a new concept named "NDSI-Ts space". 相似文献
84.
85.
Broadband synthetic aperture borehole radar interferometry 总被引:1,自引:0,他引:1
Trials in mines have established that wideband VHF borehole radars (BHR), working in the 10–100-MHz band, can be used to probe the rockmass between boreholes over ranges from <5 m to as much as 150 m with submeter resolution. There is evidence that ore bodies reflect these radar signals both specularly and diffusely, much as the ground/air interface does when overflown by synthetic aperture radar (SAR). In both SAR and BHR, multiple flight lines, together with diffuse reflections admit the possibility of developing interferometric 3D images of the object. This paper examines the possibility of imaging buried objects in three dimensions by interferometrically combining broadband VHF borehole radar profiles shot in adjacent pairs of boreholes. Broadbanding in BHR has the advantage of releasing the image from 2nπ phase ambiguities, but practically, interferometric borehole radar (InBHR) needs high signal-to-noise ratios (SNR) to avoid noise capture. This means that 3D InBHR is limited to ranges in wavelengths which are less than the rock's attenuation factor Q. Interferometric methods are developed which are capable of mapping ore bodies and other structures in three dimensions. Tangent plane migration methods are developed here in order to reconstruct surfaces that lie in the near-field of sparse interferometric arrays. 相似文献
86.
甘肃拾金坡金矿床是北山造山带南部的一处重要中型金矿床。矿体以石英脉和蚀变岩形式产出,受东西向断裂控制,赋矿围岩为早泥盆世拾金坡二长花岗岩。矿石中主要金属硫化物为黄铁矿及少量方铅矿、闪锌矿和磁黄铁矿。石英脉两侧花岗岩发生强烈的硅化、黄铁绢英岩化和绿泥石化。热液蚀变绢云母40 Ar/39 Ar坪年龄为(364.6±3)Ma,表明成矿作用发生在晚泥盆世。矿石石英中流体包裹体可分为早晚两期:早期流体包裹体群包含不同气液比水溶液包裹体和含CO2包裹体,指示成矿过程存在流体沸腾作用,其均一温度集中在280~325℃,盐度(w(NaCl))为7.86%~9.21%;晚期流体包裹体群只发育水溶液包裹体,均一温度集中于160~230℃,盐度为9.47%~11.10%。成矿流体属中温低盐度、富CO2流体。流体从早阶段演化到晚阶段,温度降低约100℃,压力由约113 MPa骤减到约11 MPa。流体包裹体的δ18 OH2O值为1.39‰~3.39‰,δD值为-71‰~-99‰。氢氧投图中,石英脉和蚀变岩样品构成良好的线性关系,暗示初始成矿流体主要来自变质热液,晚期有强烈大气降水加入。矿石金属硫化物δ34S值变化范围为4.44‰~11.33‰,峰值为8‰~9‰,呈塔式分布。与区域S同位素资料对比分析表明,石英脉型矿石S主要来自前寒武系基底,蚀变岩型矿石S更多地继承了花岗岩围岩S。综合分析认为,拾金坡金矿床属于造山型金矿,形成于造山晚期挤压—伸展转换环境。 相似文献
87.
本文通过波浪计算和理论海滩剖面方程的拟合,以Bruun模式为基础,根据Everts剖面积分方法,测算了厦门厦门大学海滨浴场、鼓浪屿港 仔后海滨浴场沙滩未来100a海平面上升引起的海滩后退量值。与此同时,计算了Bruun模式的结果。计算结果表明,两处海滨浴 滩的后退值分别为14.81和13.95m与Bruun模式的结果相当接近。 相似文献
88.
Chen Kaiyun Yuan Honglin Bao Zhian Zong Chunlei Dai Mengning 《Geostandards and Geoanalytical Research》2014,38(1):5-21
Lead isotope ratio data were obtained with good precision and accuracy using a 266 nm femtosecond laser ablation (fLA) system connected to a multi‐collector ICP‐MS (MC‐ICP‐MS) and through careful control of analytical procedures. The mass fractionation coefficient induced by 266 nm femtosecond laser ablation was approximately 28% lower than that by 193 nm excimer laser ablation (eLA) with helium carrier gas. The exponential law correction method for Tl normalisation with optimum adjusted Tl ratio was utilised to obtain Pb isotopic data with good precision and accuracy. The Pb isotopic ratios of the glass reference materials NIST SRM 610, 612, 614; USGS BHVO‐2G, BCR‐2G, GSD‐1G, BIR‐1G; and MPI‐DING GOR132‐G, KL2‐G, T1‐G, StHs60/80‐G, ATHO‐G and ML3B‐G were determined using fLA‐MC‐ICP‐MS. The measured Pb isotopic ratios were in good agreement with the reference or published values within 2s measurement uncertainties. We also present the first high‐precision Pb isotopic data for GSE‐1G, GSC‐1G, GSA‐1G and CGSG‐1, CGSG‐2, CGSG‐4 and CGSG‐5 glass reference materials obtained using the femtosecond laser ablation MC‐ICP‐MS analysis technique. 相似文献
89.
宝兴岩体位于华北板块北缘陆缘活动带东段,岩性为花岗闪长岩,LA-ICP-MS锆石~(206)Pb/~(238)U年龄加权平均值为235.0±1.3Ma,属于中三叠世。岩石的K_2O/Na_2O平均值为1.07,属高钾钙碱性系列;富集大离子亲石元素,亏损高场强元素,具有活动陆缘钙碱性岩系特征;稀土元素总量平均值为147×10~(-6),稀土元素配分曲线右倾,属具中等负Eu异常的轻稀土元素富集、重稀土元素亏损型。通过岩石学、岩石地球化学及年代学研究,结合邻区构造演化研究,认为中三叠世研究区在伸展作用下岩石圈进行拆沉,从而形成大规模的岩浆活动。 相似文献
90.
Input determination has a great influence on the performance of artificial neural network (ANN) rainfall–runoff models. To improve the performance of ANN models, a systematic approach to the input determination for ANN models is proposed. In the proposed approach, the irrelevant inputs are removed. Then an adequate ANN model, which only includes highly relevant inputs, is constructed. Unlike the trial‐and‐error procedure, the proposed approach is more systematic and avoids unnecessary trials. To demonstrate the effectiveness of the proposed approach, an application to actual typhoon events is presented. The results show that the proposed ANN model, which is constructed by the proposed approach, has advantages over those obtained by the trial‐and‐error procedure. The proposed ANN model has a simpler architecture, needs less training time, and performs better. The proposed ANN model is recommended as an alternative to existing rainfall–runoff ANN models. Copyright © 2007 John Wiley & Sons, Ltd. 相似文献