青藏高原的剧烈隆起对中华文明产生的影响

自1百万年前以来,青藏高原的迅速隆起确定了长江、黄河的形成。在青藏高原周围的两个构造结附近,已发现有元谋人和兰田猿人等。从而提出：这些中国古人类起源的环境因素与青藏高原的剧烈隆起有关。由青藏高原隆起形成的特殊地质、地理、气象条件,对近万年来中华文明的形成过程也产生了重要影响,从而形成独特的中华文明思想体系。因此,中华文明的形成不仅与长江、黄河等流域有关,而且与青藏高原的剧烈隆起有密切关系。     

100多年来中国城市空间分布格局的时空演变研究

文章剖析100多年来中国城市空间分布格局的演变特点、成因,并展望演变趋势。对城市人口密度、非农人口规模、CD值和城市规模结构的综合分析表明,中国城市空间格局具有东密西疏、呈三级阶梯状分布、省际差异大、交通指向明显的特点。这种地带性差异由来已久,是自然环境、政治、经济、社会和外部环境等因素长期综合作用的结果。这些要素在空间上存在很大差异,且要素协同作用时,具有惯性和马太效应,中国未来城市空间格局的差异仍将持续存在,并有可能扩大,东部沿海新城市空间将成为未来城市格局的主体。     

Geochemistry of Quaternary sediments of the Jeongokri archaeological site,Korea: implications for provenance and palaeoenvironments during the Late Pleistocene

The geochemical characteristics of an approximately 6‐m‐long sediment core collected from the Jeongokri archaeological site (Hantan River, Korea) were examined to determine the provenance of the sediments and to reconstruct the palaeoenvironment of the study area during the Late Pleistocene (200–127 ka). The core sediments were subdivided into two parts based on grain size: an upper (0–380 cm depth) and lower part (>380 cm depth). The lower part was deposited primarily by fluvial processes during an interglacial period [marine isotope stage (MIS) 7] with warm and humid conditions. Conversely, the upper part was mainly deposited by aeolian processes during a cold and dry glacial period (MIS 6). Geochemical characteristics, represented by major, trace and rare earth element (REE) compositions, and textures of the Jeongokri core sediments show distinct differences between the upper and lower parts. The mineralogy and major, trace and REE compositions indicate that the influence of felsic source rocks (e.g. granite) was dominant in the lower sediments, which were derived from the Hantan River. In contrast, increased quartz content and the very fine and homogeneous grain size in the upper sediments indicate an aeolian origin. REE ratios and distribution patterns, and geochemical signatures indicate that these sediments were derived predominantly from Chinese loess deposits and partially from local sediments from the Korean Peninsula; the possible source area of the upper sediments is the northern part of the Yellow Sea basin. The Yellow Sea basin, having mixed geochemical signatures between Chinese loess and Korean‐derived sediments, was exposed because of low sea levels during MIS 6. The exposed Yellow Sea basin was located in the path of winter‐monsoon winds, which may have carried a great deal of airborne sediments from the basin to the Jeongokri area. Copyright © 2011 John Wiley & Sons, Ltd.     

基于井下摆天然地震数据测量首都圈近地表波速结构

收集了首都圈数字化地震遥测台网58个井下摆2003-2008年记录的102次M≥3.0地震的数据.通过鉴别直达波及对应地表反射波的波形,发现两者到时差与震中矩和方位角无关.基于斯涅尔定律,分析获得了这些台站上方厚约300 m浅地表土层P波和S波平均速度结构以及波速比.结果表明,首都圈区域近地表P波和S波平均速度分别约为...     

Study on characteristics of 3-D translating-pulsating source green function of deep-water havelock form and its fast integration method

The singularities, oscillatory performances and the contributing factors to the 3-D translating-pulsating source Green function of deep-water Havelock form which consists of a local disturbance part and a far-field wave-like part, are analyzed systematically. Relative numerical integral methods about the two parts are presented in this paper. An improved method based on LOBATTO rule is used to eliminate singularities caused respectively by infinite discontinuity and jump discontinuous node from the local disturbance part function, which makes the improvement of calculation efficiency and accuracy possible. And variable substitution is applied to remove the singularity existing at the end of the integral interval of the far-field wave-like part function. Two auxiliary techniques such as valid interval calculation and local refinement of integral steps technique in narrow zones near false singularities are applied so as to avoid unnecessary integration of invalid interval and improve integral accordance. Numerical test results have proved the efficiency and accuracy in these integral methods that thus can be applied to calculate hydrodynamic performance of floating structures moving in waves.     

《地球科学与环境学报》2004—2010年载文信息及被引频次统计分析

运用文献计量学方法,对《地球科学与环境学报》(以下简称《学报》)2004—2010年载文的第一作者学历、职称和服务单位、论文资助项目来源、研究领域、出版时滞、被引频次、下载次数、影响因子等论文信息指标进行了统计分析。结果表明《学报》呈现以下特征:高学历作者比例稳步提升;副高职称和中级职称作者是《学报》作者的骨干力量;作者来源呈多元化发展,主办单位论文呈下降趋势;大多数论文有各类基金项目资助;基础地质及矿产地质是《学报》载文的主要内容;出版时滞需要进一步优化;被引频次计量指标反映《学报》呈现良好的发展态势。     

多策略中文地址匹配方法

地址匹配是地理编码过程中一个关键环节,是实现数据空间化的关键技术之一。针对当前中文地址匹配方法的精确率、匹配率和时间开销不能兼顾的问题,本文提出了一种多策略中文地址匹配方法。通过建立轻量级的词典进行中文地址分词,同时构建多叉树存储分词后的地址数据,匹配过程中结合模糊匹配和层级回溯匹配共同完成地址匹配工作,最终基于真实数据进行了试验。试验结果表明,该方法在匹配率、精确率和时间开销3个指标上较当前其他匹配方法表现得更加均衡。     

Petrogenesis of Kejie Granite in the Northern Changning-Menglian Zone, Western Yunnan: Constraints from Zircon U-Pb Geochronology, Geochemistry and Hf Isotope

The Kejie pluton is located in the north of the Changning-Menglian suture zone. The rock types are mainly biotite-granite. Zircon LA-ICP-MS U-Pb dating indicates that the Kejie pluton emplaced at about 80–77 Ma, Late Cretaceous. The Kejie pluton samples are characterized by high SiO2(71.68%–72.47%), K2O(4.73%–5.54%), total alkali(K2O + Na2O = 8.21%–8.53%), K2O/Na2O ratios(1.36–1.94) and low P2O5(0.13%–0.17%), with A/CNK of 1.025–1.055; enriched in U, Th, and K, depleted in Ba, Nb, Sr, Ti, P and Eu. They are highly fractionated, slightly peraluminous I-type granite. The two samples of the Kejie pluton give a large variation of εHf(t) values(-5.04 to 1.96) and Hf isotope crustal model ages of 1.16–1.5 Ga. Zircon Hf isotopes and zircon saturation temperatures of whole-rock(801°C–823°C) show that the mantle-derived materials maybe have played a vital role in the generation of the Kejie pluton. The Kejie pluton was most likely generated in a setting associated with the eastward subduction of the neo-Tethys ocean, where intrusion of mantle wedge basaltic magmas in the crust caused the anatexis of the latter, forming hybrid melts, which subsequently experienced high-degree fractional crystallization.     

中国城市公共健康水平的时空演化及其影响因素

采用定基极差熵权法与定基等权赋值法相结合的综合评价方法、核密度估计、探索性空间数据分析等方法,分析2003—2018年中国284个地级以上城市公共健康水平的时空演化特征,并运用广义空间两阶段最小二乘法考察其影响因素。结果发现：① 研究期内中国城市公共健康水平整体呈上升趋势,但各城市间公共健康水平差异有所扩大,且始终存在多级分化现象;② 四大板块核密度曲线在重心位置、主峰高度、波峰数量、拖尾长度、拖尾厚度上均有各自演化形态,是一种时段特征与地区特色相互耦合叠加的结果;③ 中国城市公共健康水平存在正向空间溢出效应和空间“同群效应”,空间集聚类型实现了由LL型为主体向HH型为主体的转化;④ 收入水平、人口密度、科技进步、工业化程度、卫生体制改革对城市公共健康具有影响,但各因素对不同区域的影响存在异质性。