气象部门出纳日记账系统在国库集中支付中的应用

利用改进后的《出纳日记账处理系统》,按支出科目的类、款、项进行分类,登记零余额账户的银行存款日记账,达到《气象部门财政国库管理制度改革试点资金支付管理办法实施细则》关于登记银行日记账簿的要求。     

Age,growth and natural mortality of blue jack mackerel Trachurus picturatus (Carangidae) from the Canary Islands,Spain (NW Africa)

Status assessment of exploited fish populations is a general requirement to ensure sustainability of fisheries in both global and local contexts. The blue jack mackerel Trachurus picturatus (Bowdich, 1825) remains unassessed in a data-limited fishery in the eastern central Atlantic, within the waters of the Canary Islands (Spain) off the coast of northwest Africa. This is the most southwestern targeted fishery in the species’ distributional range. To obtain basic life-history information, a total of 2 472 specimens were analysed, ranging from 10.2 to 31.9 cm total length, from samples collected monthly between March 2005 and March 2006. Length–weight relationships (a = 0.0023; b = 3.418; R ² = 0.97) showed no significant difference between sexes. Deposition periodicity and coherence of the ageing criteria were verified by analysis of the monthly evolution of the otolith edge. Ages were estimated by counting annual growth rings on whole otoliths, with these fish ranging from age 0 to 6 years. The von Bertalanffy growth model, which was used to estimate growth parameters from both direct readings and back-calculated length-at-age data, gave good statistical fits. The parameters from the direct readings were: L∞ = 34.9 cm; k = 0.214 y^–1; t ₀ = ?2.545 y (R ² = 0.84), and the natural mortality rates estimated from empirical methods varied between 0.20 and 0.55 y^–1.     

新疆东天山地区星星峡群的解体及地质意义

新疆东天山地区星星峡一带的原星星峡群为一套岩性复杂、变质程度差异很大的变质岩系, 在该区进行的1:50000区调工作中, 通过详细的地表调查和地层剖面测量, 并参考了相关变质侵入体的同位素年龄后认为, 根据岩石组合、变质程度、同位素年龄等地质标志, 可将其初步解体为大致形成于晚太古代—古元古代的天湖岩群(Ar₃—Pt₁T.)和长城纪星星峡岩群(ChX.)两套时代不同的岩群。该岩群的解体和区域对比表明, 中天山星星峡一带和塔里木北缘库鲁克塔格一带的前南华系基底应该是一致的, 属于统一的塔里木北缘隆起带。      

赤道印度洋中部断面东西水交换的季节变化及其区域差异

采用海洋再分析资料和实测资料研究了热带印度洋中部东西水交换特征。结果表明存在两个相互独立的过程,即北印度洋过程(4°~6°N)和赤道过程(2°S-2°N)。北印度洋过程受季风影响显著,11月至翌年3月冬季风期间表现出很强的低盐水向西输送,5-9月夏季风期间则为高盐水向东输送;由于冬季风期间的输送较强,年平均表现为低盐水向西输送。赤道过程分为表层过程和次表层过程。表层赤道过程受局地风场驱动,有明显的半年周期;4-5月和10-11月的东向流将赤道西印度洋的高盐水向东输送,其余月份相反;向东的输送较强,年平均表现为净高盐水向东输送。在次表层赤道过程没有明显的季节变化,海流全年一致向东,将海盆西部的高盐水向东输送。     

中国转型期中心城市城乡关系演变

2000 年以来中国开始进入城乡互动与统筹发展的转型期。以中国中心城市为样本, 城乡经济增长与城市化为研究视角, 中心与外围区域为空间范围, 利用时间序列数据, 采用多元变量分析模型方法, 对中国区域中心城市城乡关系要素变化进行了动态分析, 建立了中心城市城乡关系模型, 划分了中国中心城市城乡关系地域类型。研究结果表明:中心城市外围县区的固定资产投资、经济总量、工业生产的增长速度开始超过中心市区, 经济要素过度集聚中心市区的格局发生转变。但中心城市外围县区的公共设施与基础设施供给能力与中心市区仍有较大差距, 公共设施与服务的非均等化是中国城乡统筹发展的关键性障碍因素。依据城乡要素中心市区与外围县区空间变化, 中国中心城市城乡关系可以划分为中心市区集聚型、外围县区快速成长型、中心外围相对均衡型、中心外围整体发展型等4 种类型, 反映出中国各中心城市城乡关系演变阶段、城乡结构特征与空间形态的地域差异变化。     

基于协调与共享发展的中原城市群建设制度创新

协调发展与共享发展是指导中原城市群建设的新理念.运用协调发展、共享发展的理念分析中原城市群建设所面临的问题,结果表明,由于现有制度的缺陷或缺失,导致城市群内部存在人口迁移受阻、经济非理性竞争、公共资源不可共享、空间一体化梗阻、一体化秩序混沌、忽视协调和共享发展等问题.因此,中原城市群需要对现有的制度进行改革和创新,建立保障人口自由迁移制度、合理的利益分配和合作发展制度、有限的公共服务共享制度、发展规划的协调制度、协调与共享发展的组织制度,体现一体化贡献的政府政绩考核制度.     

区域政策、产业特性与中央企业空间布局演变

通过建立企业区位选择的“推力-拉力”模型, 本文考察了具有不同产业特性的央企在不同区域政策阶段的空间布局演化, 分析了区域政策、产业特性对央企空间布局的影响机制和影响过程。主要结论为:企业空间布局的动力来自内部推力与外部拉力, 前者由企业特征和产业特性组成, 后者由区域政策制度和区域条件组成。区域政策制度和产业特性是影响央企空间布局的主要因素。央企空间布局总体变化与区域政策的演变趋同, 但产业间存在差异。资本、资源密集型产业央企布局受区域政策和区域条件影响较强;劳动密集型产业央企布局偏好政策优惠及交通便利区域;高新技术、现代服务业央企对创新网络和社会资本等因素依赖较大, 布局受区域政策影响较弱;组织结构为区域部型、公共服务业、特殊行业的央企布局受外部拉力影响较弱。     

特提斯喜马拉雅带东段列麦白云母花岗岩年代学及成因

列麦白云母花岗岩位于特提斯喜马拉雅东段,侵位于雅拉香波穹窿边部早古生代浅变质岩中。为揭示其形成时代及成因,本文对其开展LA-ICP-MS锆石U-Pb年代学、Hf同位素及岩石地球化学研究。结果表明列麦白云母花岗岩具有高SiO_2(71.08%～71.49%)、Al_2O_3(15.55%～15.72%)和K_2O(4.32%～4.57%),高的A/CNK比值(1.17～1.21),低的CaO/Na_2O比值(0.22～0.28),属于高钾钙碱性过铝质花岗岩;富集Rb、Th和Hf,亏损Ba、Nb、Sr和Ti,稀土元素呈轻稀土(LREE)富集,重稀土(HREE)相对亏损的向右倾斜的配分模式(LREE/HREE=16.57～17.91),具有弱负Eu异常(δEu=0.78～0.79)。与二云母花岗岩比较,列麦白云母花岗岩具有较高的Rb含量(204.1×10~(-6)～293.8×10~(-6))、较低的Sr(134.6×10~(-6))及显著的重稀土分馏效应。锆石新生边年龄为48.5±1.1 Ma(MSWD=2.1),代表其结晶年龄,该年龄为目前报道的最早年龄,其初始Hf同位素组成ε_(Hf)(t)=-6.4～-2.3,显示物源为壳源性质,二阶段模式年龄介于731～839 Ma之间,表明成岩物质形成于新元古代;核部继承锆石年龄变化在135.7～3339.2 Ma之间,表明其源岩为早白垩世沉积岩,是在印度与欧亚大陆主碰撞阶段,陆-陆碰撞导致地壳缩短加压升温,引起早白垩世沉积岩部分熔融而形成的。     

Protracted thrusting followed by late rapid cooling of the Greater Himalayan Sequence,Annapurna Himalaya,Central Nepal: Insights from titanite petrochronology

The Greater Himalayan Sequence (GHS) has commonly been treated as a large coherently deforming high‐grade tectonic package, exhumed primarily by simultaneous thrust‐ and normal‐sense shearing on its bounding structures and erosion along its frontal exposure. A new paradigm, developed over the past decade, suggests that the GHS is not a single high‐grade lithotectonic unit, but consists of in‐sequence thrust sheets. In this study, we examine this concept in central Nepal by integrating temperature–time (T–t) paths, based on coupled Zr‐in‐titanite thermometry and U–Pb geochronology for upper GHS calcsilicates, with traditional thermobarometry, textural relationships and field mapping. Peak Zr‐in‐titanite temperatures are 760–850°C at 10–13 kbar, and U–Pb ages of titanite range from c. 30 to c. 15 Ma. Sector zoning of Zr and distribution of U–Pb ages within titanite suggest that diffusion rates of Zr and Pb are slower than experimentally determined rates, and these systems remain unaffected into the lower granulite facies. Two types of T–t paths occur across the Chame Shear Zone (CSZ). Between c. 25 and 17–16 Ma, hangingwall rocks cool at rates of 1–10°C/Ma, while footwall rocks heat at rates of 1–10°C/Ma. Over the same interval, temperatures increase structurally upwards through the hangingwall, but by 17–16 Ma temperatures converge. In contrast, temperatures decrease upwards in footwall rocks at all times. While the footwall is interpreted as an intact, structurally upright section, the thermometric inversion within the hangingwall suggests thrusting of hotter rocks over colder from c. 25 to c. 17–16 Ma. Retrograde hydration that is restricted to the hangingwall, and a lithological repetition of orthogneiss are consistent with thrust‐sense shear on the CSZ. The CSZ is structurally higher than previously identified intra‐GHS thrusts in central Nepal, and thrusting duration was 3–6 Ma longer than proposed for other intra‐GHS thrusts in this region. Cooling rates for both the hangingwall and footwall of the CSZ are comparable to or faster than rates for other intra‐GHS thrust sheets in Nepal. The overlap in high‐T titanite U–Pb ages and previously published muscovite ⁴⁰Ar/³⁹Ar cooling ages imply cooling rates for the hangingwall of ≥200°C/Ma after thrusting. Causes of rapid cooling include passive exhumation driven by a combination of duplexing in the Lesser Himalayan Sequence, and juxtaposition of cooler rocks on top of the GHS by the STDS. Normal‐sense displacement does not appear to affect T–t paths for rocks immediately below the STDS prior to 17–16 Ma.