吉林地震台网与中国地震台网测定东北地区深源地震震级偏差研究

选用吉林地震台网正式运行以来记录的18次东北地区mb (mB)≥4.0深源地震资料,以中国地震台网地震目录给出的震级为标准震级,进行震级偏差统计分析,得出震级校正值.分析震级差异形成的原因,为吉林地震台网测定东北深源地震震级偏差校正提供参考.     

吉林四方甸子钼矿床成岩成矿时代及岩石地球化学特征

吉林四方甸子钼矿床是一新发现的石英脉型钼矿床,矿床产于二长花岗岩中。矿床成矿包括无矿石英脉阶段、石英-辉钼矿-黄铁矿阶段和石英-碳酸盐化阶段。通过对矿区内花岗质岩石进行LA-ICP-MS同位素测年,获得花岗闪长岩成岩年龄为（170.0±1.0） Ma,二长花岗岩成岩年龄为（179.0±1.0） Ma。对含矿石英脉中辉钼矿Re-Os同位素测年分析,获得辉钼矿模式年龄值为（175.0 ± 2.6）～（176.5 ± 2.6）  Ma,加权平均值为（176.1 ± 1.1） Ma,等时线年龄为（176.6 ± 4.2）  Ma,表明四方甸子钼矿床形成于早侏罗世晚期。岩体w(SiO₂)为66.17%～76.60%,w(Na₂O)和w(K₂O)分别为3.15%～5.40%和2.42%～5.42%,里特曼指数σ为2.17～2.93。稀土元素分布形式呈右倾型,轻、重稀土元素分馏明显。微量元素总体显示相对富集Rb、Ba、Th、U等大离子亲石元素（LILE）,亏损Nb、Ta、Ti、P等高场强元素（HFSE）。综合分析表明,岩石为弱过铝质I型花岗岩。成岩成矿动力学背景为燕山早期古太平洋板块向欧亚大陆俯冲作用的大陆边缘环境。     

Economic development and energy efficiency in Jilin Province,China

The relationship between economic development and energy consumption is revealed by employing cointegration theory, the index decomposition method, and a log-linear regression approach based on a case study of Jilin Province, China. The results suggest： 1） the economic development and energy consumption are interdetermined, whose relationship is positive and long-term. The economic development is highly depending on the energy in Jilin Province. 2） Under the condition of other unchanged factors, the change of industrial energy efficiency contributes to the energy saving, while that of industrial structure increases the energy consumption. 3） The industrial structure change enhances the energy intensity, but the energy utility efficiency change lowers it. From the view of contribution to the energy consumption, the contribution of industrial structure was more than that of the energy utility efficiency in 2000-2011. 4） In 2000-2011, the comprehensive energy intensity change and hydroelectricity energy intensity change were related to all industrial structures＇ change, and the influencing factors about structure of oil energy intensity change were more than those of coal energy intensity change; from the impact degree, agricultural proportion decreased exerted an positive and greater effect on lowering the energy intensity of comprehensive energy and hydroelectricity, and industrial one did on coal and natural gas. Some conclusions can be drawn as follows： the major way to promote the coordinated development of the industrial economy and energy consumption is to optimize the industrial structure by increasing the proportion of the tertiary industry and low energy consumption industrial sectors and to enhance the energy utility efficiency.     

基于通信流的吉林省流空间网络格局

基于实际发生的信息流研究流空间网络格局是一种新的尝试。以吉林省县级以上地方为研究单元,以各地间固定电话通话时长为原始数据,采用主成分分析法、C-Value 和D-Value层级分析法、优势流分析法、最小生成树法对吉林省流空间格局进行了分析。研究表明：吉林省流空间是以长春市为中心,长春市、延吉市、通化市、公主岭市为主导型城市,吉林市、白城市、白山市、辽源市、松原市、四平市为次级主导型城市,其他城市为从属型城市的层级化网络结构;行政区划在流空间格局中发挥基本的影响作用;以长春市为“单中心”的流空间特征明显,吉林省并无明显的次中心作用,长春市与吉林市流空间联系并不紧密,与传统认识和意愿有所不同;公主岭市和敦化市在吉林省流空间格局中占有重要地位,公主岭市倾向于融入长春城市圈,敦化市在吉林省东部空间网络格局中发挥了重要作用,两市的区域联通功能亟待挖掘;四平市和梨树县流空间联系紧密,适宜同城化发展。     

吉林省域城镇体系规划综合调控作用研究

基于省域城镇体系规划的本质认识及吉林省城镇体系发展背景、现状及趋势的研究基础上,借鉴发达省区的经验教训,实施适应吉林省发展的"保护两厢,聚集中央"新型城市化发展战略,采取战略取舍、结构分异、整合发展、空间管制等战略举措充分发挥省域城镇体系的综合调控作用,促进吉林省经济、社会、生态环境的可持续发展.     

近20年吉林西部水旱灾害变化特征及机理研究

吉林西部水旱灾害频繁发生。特别是自1980年以来,水旱灾害造成的成灾面积及其损失呈快速增长的趋势,这与我国和世界其它地区水旱灾害增多的趋势相一致。以往大多认为这一趋势是全球变化和自然因素引起的。文章通过对吉林西部人类活动与生态环境的互动关系研究,发现造成这一趋势的原因是人类对自然不合理活动所引起的生态环境退化如土地的沙漠化、盐碱化,草地的严重退化和社会其它因素。     

吉林省西部湿地土地利用格局变化的多情景模拟

吉林省西部属于生态脆弱区,湿地作为重要的生态单元,其发展变化对区域生态环境产生重要影响。近年来,由于受到较多的人为干扰,该区域湿地变化极为显著。为了充分发挥湿地生态环境功能,促进区域生态环境改善,以吉林省西部2000-2010年湿地变化数据为基础,基于情景分析法设置了自然变化（情景1）、规划优先（情景2）和生态优先（情景3）三种情景,利用CLUE-S模型对2020年湿地空间格局进行模拟,并从湿地空间分布变化特征和景观抗干扰能力两个方面对不同情景下的湿地格局进行分析评价,旨在了解不同情景下湿地格局的差异性,寻求合理的湿地空间分布格局。结果表明：CLUE-S模型的土地利用预测正确率为84.54%,κ指数为0.83,能够较好地模拟2020年湿地格局变化,特别是对沼泽湿地、水域和建设用地模拟效果较好;不同情景下湿地空间格局特征具有明显的差异性,三种情景下的沼泽湿地的质心均偏向西南,水域的质心均偏向东南,而水田的质心在情景1中偏向东北,在情景2和情景3中偏南,沼泽湿地和水田在情景3比情景1中具有更强的聚集性,而水域恰相反,情景1比情景3中具有更强的聚集性;不同情景下的湿地景观抗干扰能力不同,2010-2020年,情景1中的所有湿地类型的景观干扰指数都逐渐增加,而情景2和情景3中沼泽湿地和水域的景观干扰指数逐渐降低,尤以生态优先情景的下降幅度最大。表明在实施科学的生态建设时,湿地景观具有较强的抗干扰能力。     

吉林省红旗岭矿区铜镍硫化物矿床成矿规律、矿床成因、找矿标志

红旗岭镍矿区是我国岩浆岩型铜镍硫化矿床的主要矿化集中区之一,在本区内出露的镁铁-超镁铁质岩所划分的3个岩带中,有的岩体含铜镍矿,有的不含矿.通过近期在区内开展的全国危机矿山找矿中所形成的资料及从构造控岩控矿、岩性控矿、成矿与岩石类型的关系进行对比,对区内镁铁-超镁铁质岩体的综合找矿标志进行总结,为今后在区内寻找隐伏岩体及其含矿性的评价提供一定的理论依据.     

Changing rural development inequality in Jilin Province, Northeast China

Rural development inequality is an important practical issue during the course of full establishment of a ′moderately well-off society′ in modern China,and the objective understanding and evaluation of the status and regional inequality of rural development can provide scientific basis for ′building a new countryside′ and coordination development of rural-urban regions.Based on the county-level data of 2000,2005 and 2009,this paper examines the rural development inequality of Jilin Province in Northeast China by establishing a rural development index.The spatio-temporal dynamic patterns and domain factors are discussed by using the method of exploratory spatial data analysis and multi-regression model.The results are shown as follows.Firstly,most of the counties were in lower development level,which accounted for 58.3%,62.5% and 66.7% of the total counties in 2000,2005 and 2009,respectively.The characteristics of spatial inequality were very obvious at county level.For example,rural development level of Changchun Proper and the proper of seven prefecture-level cities were much higher than that of the surrounding regions.The counties in the eastern and northern Jilin Province were the lowest regions of rural development level,while the middle counties were the rapid growth areas in rural economy.Secondly,Moran′s I of rural development index(RDI) was 0.01,–0.16 and –0.06 in 2000,2005 and 2009,respectively,which indicated that spatial agglomeration of RDI was not obvious in Jilin Province,and took on the characteristic of random distribution.The counties of both the units and its adjacent units have higher development level(HH) were transferred from the western areas to the eastern areas,while the countries of both the units and its adjacent units have lower development level(LL) were diffused from the eastern to middle and western Jilin Province.Finally,the result of multi-regression analysis showed that the improvement of agricultural production condition,development of agricultural economics and the adjustment of industrial structure were the domain factors affecting rural development inequality of Jilin Province in the later ten years.     

吉林省雨凇气候特征及其天气分型

利用1980-2007年吉林省11个气象观测站常规观测资料,采用统计分析的方法,对共计100次雨凇天气的时空分布特征进行了分析。结果表明：吉林省雨凇天气南多北少,丘陵地带及长白山脉的迎风坡一带为雨凇的频发区。雨凇多发于冬初和初春,并且雨凇出现几率在减少。吉林省的雨凇天气的温度层结结构与中国南方省市雨凇的情况存在较大差异：吉林省雨凇天气并不存在融化层和逆温层等结构。通过对地面形势的分析,将雨凇天气分为低压后部型、高压前部型、低压南部型和低压型。它们的共同点是高空均有较深厚的后倾槽移过吉林省,温度槽落后于高度槽;近地面层先升温后降温,850 hPa相对湿度为70 %左右,而地面相对湿度均可达到80 %或以上。强雨凇天气主要发生在东南部地区,强雨凇天气出现时的地面及高空形势与一般的雨凇天气发生时的形势基本相似,但850 hPa和地面的相对湿度比一般情况偏大10 %左右。