A multi-scale 3-D crust velocity model in the Hefei-Chao Lake area around the southern segment of Tanlu Fault Zone

Regional high-precision velocity models of the crust are an important foundation for examining seismic activity, seismogenic environments, and disaster distribution characteristics. The Hefei-Chao Lake area contains the main geological units of Hefei Basin, with thick sediments and the Chao Lake depression. Several major concealed faults of the southern NNE-trending Tanlu Fault Zone cross this area. To further explore the underground distribution characteristics of the faults and their tectonic evolutionary relationship with adjacent tectonic units, this study used ambient noise data recorded by a seismic array deployed in Hefei City and Chao Lake, constructing a 3-D velocity model at the depth of 1–8 km. Then a multi-scale high-resolution 3-D velocity model of this area was constructed by this new upper crustal velocity model with the previous middle and lower crustal model. The new model reveals that a high-velocity belt is highly consistent with the strike of the Tanlu Fault Zone, and a low-velocity sedimentary characteristic is consistent with the Hefei Basin and Chao Lake depression. The distribution morphology of high and low velocity bodies shows that the sedimentary pattern of Hefei-Chao Lake area is closely related to the tectonic evolution of the Tanlu Fault Zone since the Mesozoic. This study also identifies multiple low-velocity anomalies in the southeastern Hefei City. We speculate that strong ground motion during the 2009 Feidong earthquake (magnitude of 3.5) was related to amplification by the thick sediments in the Hefei Basin. We also discuss further applications of multi-scale high-resolution models of the shallow layer to strong ground motion simulations in cities and for earthquake disaster assessments.     

海洋船舶业全要素生产率及影响因素分析 ——基于产业环境视角

文章以2004—2015年15个造船省、市、自治区的数据为基础,运用DEA-Malmquist指数法计算了中国海洋船舶业的全要素生产率(TFP)。结果发现,从长远来看,技术进步是海洋船舶业TFP的主要增长动力;而从短期波动看,海洋船舶业TFP的增长易受到技术效率与技术进步的交互作用。同时,不同地域海洋船舶业TFP的增长动力也会有所不同,东部地区海洋船舶业TFP的主要增长动力为技术进步,中西部地区海洋船舶业TFP的主要增长动力为技术进步和技术效率的综合影响。基于以上计算结果,从产业环境的视角分析中国海洋船舶业TFP的影响因素,实证结果表明,宏观的经济形势、国际市场需求、科技发展投入对本国海洋船舶业TFP有积极影响,社会固定投资量的增加对中国海洋船舶业TFP产生负向的影响。并提出适当减少船舱生产的固定设施投入,并将减少的固定资产投入转向研发投入;政府应制定合理的产业政策为海洋船舶业提供良好的宏观经济形势;从税收上给予具备高技术水平的船企以优惠等建议。     

插值条件下格网DEM坡度计算模型的噪声误差分析

针对目前DEM（Digital Elevation Model, DEM）数字地形分析的精度评价多数不考虑DEM误差的空间自相关性或仅仅采用经验的自相关性模型问题,本文从DEM插值入手,从理论上推导了插值条件下格网DEM邻域窗口内坡度噪声误差的空间自相关性模型以及坡度精度模型,并选取典型的插值方法和坡度差分算法,从实验角度分析了在顾及和不顾及空间自相关性两种情况下的格网DEM坡度计算模型的噪声精度,实验结果表明：坡度精度受DEM噪声误差的空间自相关性影响较大,并与DEM插值方法和坡度计算模型中的差分算法有关。     

民族文化资源的类型特征及成因分析——以格萨尔（果洛）文化生态保护实验区为例

由人类非物质文化遗产《格萨（斯）尔》史诗派生出的格萨尔文化是青藏高原地区独特的区域文化形态。文化资源是文化的载体和展示形式,具有价值性和不可替代性。研究格萨尔文化资源的分类、空间分布及成因对于探讨青藏高原地区人地关系,保护人类非物质遗产有非常重要的意义。果洛藏族自治州是格萨尔文化资源最为富集的区域,并于2014年被授予格萨尔文化生态保护实验区。本文首先对格萨尔文化资源进行界定和分类,并以果洛为例,探讨格萨尔文化资源的空间分布特征及与自然地理条件（高程、水源、坡度、坡向、可达性）的关系,并分析影响文化资源分布的原因,得出以下结论：① 格萨尔文化资源可以分为4大类,11个亚类和60个子类,果洛的格萨尔文化资源覆盖全部类型,共1189个;② 果洛格萨尔文化资源空间分布具有聚集性,其中A类文化人（团体）类集聚程度最高,并通过最近邻分析和密度分析对各类文化资源的集聚空间进行识别;③ 格萨尔文化资源的空间分布与自然地理条件有关,多位于海拔相对较低、距水源地较近的位置,不同类型的文化资源分布对坡度、坡向和可达性的关系不同。     

中心地理论创新与发展的基本视角和框架

中心地理论是城市地理学揭示规律、解决问题的重要方法之一。面对时代发展、社会转型、技术进步及其带来的城市与区域巨变, 中心地理论需要创新发展。首先, 突破中心地理论的严苛假设、忽视系统动态性和自然-人文要素综合性的固有缺陷, 拓宽其普适性。其次, 以动态的和联系的眼光审视中心地系统外部条件、内部要素和组织形式与机制变化, 从中发现理论创新的视角。包括人口再分布, 城市体系重组, 全球产业网络兴起等宏观背景变化的视角;现代交通条件、信息技术发展、技术革新、体制变革等影响要素和机制变化的视角;全球城市网络形成, 城市带、群、链迅速聚合, 底层中心地重构等中心地系统组织形式新变革的视角;RS、GIS和现代统计手段应用的视角。再次, 中心地理论创新与发展有必要从“肢解”阶段进入到整体完善过程, 构建创新与发展的基本框架:①以指导实际应用, 形成理论和研究范式为创新和发展的目标;②以中心性测度新模型、严苛条件缓和、动态中心地系统、中心地系统畸变模式、中心地扩散域的空间嵌套等为创新和发展的核心内容;③突破自然-人文耦合要素对中心地系统影响机理及模型化表达, 现代中心地系统空间图景, 动态开放的现代中心地系统建设等重点问题。     

食品安全导向下的都市农业发展模式——以北京蔬菜生产为例

随着人们生活水平和认知能力的不断提高,人们对健康的关注和需求也变得更加强烈,因此伴随着近年来食品问题的频繁曝光,食品安全已成为社会各界最关心的议题,其中,蔬菜和牛奶等易腐食品更成为首要关注点。都市农业拥有“近距离短环节”的优势,应当成为城市蔬菜供应的重要渠道和保证城市居民蔬菜安全的主角。本文以北京为研究案例,针对食品安全导向下的城市蔬菜发展模式进行了研究。首先通过解析北京生鲜蔬菜的供应来源,总结了“长距离多环节”农业存在的蔬菜安全问题及都市农业在保证生鲜蔬菜品质安全方面的诸多优势。接着分析归纳了保证蔬菜品质安全下的几种都市农业发展模式,并以典型案例研究的方式分析了各模式的产生背景、运行管理特点。最后提出了促进都市农业发展的保障机制。     

面向协同式森林灭火决策的领域本体构建及其解析

森林灭火决策的参与人员可能来自不同的组织、不同领域,他们有不同知识结构、专业背景、学识和各自的经验、偏好,这往往不利于决策过程中的交流、协同进行。本文把本体引入协同式森林灭火决策中,解决决策成员在协作中对他人所述的内容理解一致问题。分析了现有建立领域本体的主要方法,并借鉴软件开发的生命周期理论,提出建立面向森林火灾的领域本体的具体实现方法。以森林灭火决策为应用导向,通过对森林灭火决策的内容分析及与领域专家相互交流,根据领域中概念分类体系和概念的组合结构,从相关领域(林业、气象学、消防工程、地理学)抽象出概念术语集、关系集、函数集、规则集等,建立可共享、理解、重用、互操作的概念模型;利用本体建模工具,建立森林灭火本体库;设计与实现了本体的解析与可视化工具,用户可以交互式的查询术语的概念内涵,利用可视化工具,显示概念之间的关系。研究成果将为学科或领域间的高效协作打下通信与交流的基础,为林业、消防的信息化研究、林火本体服务提供可借鉴的框架和成果,为林火管理和应急指挥决策提供一个语义层级次上的重要途径。     

Lateral variation in Moho depth around the southern Tanlu fault zone and its adjacent area

We estimated Moho depth beneath the southern Tanlu fault zone and its adjacent area using common-conversion-point(CCP)stacking of receiver fun-ctions,which were computed from teleseismic records of the CEArray.Our estimated Moho depth matches well with 2-D profiles derived from active-source deep seismic reflection surveys,suggesting that the calculated the Moho depth map is likely accurate beyond the 2-D profiles.Overall,the estimated Moho depth map showed a high spatial correlation with tectonic provinces,i.e.,Moho topographic boundaries are in good agreement with geological boundaries.Beneath the Dabie orogenic belt and the mountainous areas in southern Anhui Province,the Moho lies relatively deep,and there is an obvious difference in Moho depth between the two sides of this segment of the Tanlu fault.We further selected four depth profiles with dense instrumentation to show Moho depth changes across different tectonic blocks in the study area.We saw two step-like changes in Moho depth beneath the Xiangfan-Guangji and Gushi-Feizhong,which run parallel along the WNW-ESE direction and delineate the southern and northern bounds of the northern Dabie orogenic belt,which is likely the suture zone between the North China Block and South China Block.Crust beneath the northeast corner of the study area is significantly thinner than other areas,which is consistent with the crustal detachment model proposed for suturing between the North and South China blocks in the region east to the Tanlu fault.     

Analysis of influencing factors on fine sediment flocculation in the Changjiang Estuary

Based on the test data in dynamic water and static water, the main factors, which influence the fine sediment flocculation, are analyzed with a gray model method of correlation theory. It is shown that the main influencing factors are water temperature, settling time, salinity, grain size, sediment concentration and current velocity according to the correlation coefficients. Among them, the salinity and the sediment grain size are critical type influencing factors (CrTIF); the settling time, the sediment concentration and the velocity are continuous type influencing factors (CoTIF); and the water temperature has the characteristics of both. When the critical values of CrTIF are reached or exceeded, the fine sediments will be flocculated, but values of CrTIF will not influence the settlement strength of floes. The influence of CoTIF is continuous. The values of the CoTIF will not only influence the occurrence of flocculation but also the settlement strength of the floes.     

Miocene emplacement and deformation of the Konga Shan granite (Xianshui He fault zone, west Sichuan, China): Geodynamic implications

The presently active sinistral Xianshui He strike-slip fault (XSH) is a lithospheric scale strike-slip fault in the eastern Himalaya. In the study area this fault affects the eastern edge of the Konga Shan granitic massif, where it has caused both brittle and ductile deformation. A RbSr isochron and Nd and Pb isotope study of three samples, and a UPb zircon study of a single sample, were completed on the granite.

UPb data indicate a granite emplacement age of 12.8 ± 1.4 Ma. The RbSr isochrons show that the granite emplacement and the deformational event were synchronous, at around 12-10 Ma (minimum age for deformation). The Nd and Pb isotope compositions of whole rocks and K-feldspars indicate the involvement of Proterozoic continental crust, which is confirmed by UPb systematics indicating inherited zircons.

Sinistral faulting along the XSH began at the latest at 12 Ma and marks the extrusion toward the east of the West Sichuan and South China blocks, following their extrusion along the Red River fault zone between 50 and 21 Ma.