中老泰铁路建设对云南省及沿线国家空间联系格局的影响

中老泰铁路作为泛亚铁路东、中、西三线的中线,对中国与老挝、泰国的跨境合作以及助推“一带一路”倡议的“中国-中南半岛”经济走廊的建设起着重要作用。选取中国云南省和老挝、泰国作为研究区域,以非障区的区域开发为基础,并选取铁路沿线15个主要城市,基于城市流网络视角对比铁路建设前后区域可达性与城市流网络的变化,结果显示：铁路建成将提升障区可进入性与非障区可开发性,提高区域互联开发潜力,提升研究区内可达性。可达性呈现以铁路线路为轴向周围辐射递减的格局,但泰国西部及老挝东部自然障区可达性提升效果甚微;铁路将增强城市间联系强度,实现“树状-网状”的城市流网络形态高效重构,网络发育更加成熟稳固;铁路也使得网络结构扁平化、分散化,流网络重构过程中资源的分散与耗散并存,城市间联系效率下降。     

离体海带柄部“色环区”的再生实验

海带是一种大型的经济海藻,其孢子体由三种“器官”组成——叶片、柄和假根。海带是间生长。一般认为生长部在叶片的基部。生长部的细胞具有很强的分生能力,在海带生长过程中,不断地从叶片基部分生出新组织推动老组织向前延伸。在适宜环境条件下,新组织增长速度超过叶尖部老组织的脱落速度,结果就形成了海带叶片的增长。受精卵分裂后,一直到约100个细胞左右的小海带,藻体所有的细胞都有分裂能力。     

A study of internal solitary waves observed on the continental shelf in the northwestern South China Sea

Based on in-situ time series data from the acoustic Doppler current profiler (ADCP) and thermistor chain in Wenchang area, a sequence of internal solitary wave (ISW) packets was observed in September 2005, propagating northwest on the continental shelf of the northwestern South China Sea (SCS). Corresponding to different stratification of the water column and tidal condition, both elevation and depression ISWs were observed at the same mooring location with amplitude of 35 m and 25 m respectively in different days. Regular arrival of the remarkable ISW packets at approximately the diurnal tidal period and the dominance of diurnal internal waves in the study area, strongly suggest that the main energy source of the waves is the diurnal tide. Notice that the wave packets were all riding on the troughs and shoulders of the internal tides, they were probably generated locally from the shelf break by the evolution of the internal tides due to nonlinear and dispersive effects.     

挪威近海Storegga滑坡侧翼麻点的成因及烟囱构造

1 Storegga滑坡崖地质背景 挪威的陆缘形态以Storegga滑坡崖为标志,该滑坡崖是由一系列巨大的全新世陡坡崩塌形成的.14C测年证实,最近一次崩塌出现在约7.2 ka以前.     

Geochemistry and Petrogenesis of Late Ediacaran Rare-metalAlbite Granites of the Arabian-Nubian Shield

The Abu Dabbab albite granite(ADAG), in the central Eastern Desert of Egypt, hosts the most significant rare metal ore deposit in the northern part of the Neoproterozoic Arabian-Nubian Shield. Here, we report detailed field,petrographic, mineralogical and geochemical investigation of the ADAG, an isolated stock-like granitic body with sharp intrusive contacts against metamorphic country rocks, probably emplaced at about 600 Ma. The fine-grained porphyritic upper unit is a preserved remnant of the shallowly-emplaced apex of the magma chamber, whereas the medium-grained lower unit crystallized at deeper levels under subvolcanic conditions. The peraluminous leucocratic ADAG shares common geochemical characteristics with post-collisional intraplate A-type magmas. In addition to the conspicuous enrichment in Na2 O, the ADAG is remarkable for its anomalous concentrations of Ta, Nb, Li, Hf, Ga, Sn, Zn and heavy rare-earth elements. Nb-Ta minerals in the ADAG are mixed with Fe-Mn oxides, forming black patches that increase in abundance toward of the base of the intrusion. Columbite-tantalite, cassiterite and wolframite are the most important ore minerals.Pronounced negative Eu anomalies(Eu/Eu* = 0.10–0.24) reflect extreme magmatic fractionation and perhaps the effects of late fluid-rock interaction. The ADAG was most likely generated by partial melting of the juvenile middle crust of the ANS as the geotherm was elevated by erosional uplift following lithospheric delamination and it was emplaced at the intersection of lineations of structural weakness. Although formation of the ADAG and its primary enrichment in rare metals are essentially due to magmatic processes, late-stage metasomatism caused limited redistribution of rare metals. Fluid-driven subsolidus modification was limited to the apex of the magma chamber and drove development of greisen, amazonite, and quartz veins along fracture systems.     

加里福尼亚Fremont谷一井可反映断层的最新活动

自1978年3月,在Fresmout谷(F谷)一口井中连续记录到水位资料.其靠近Garlock断裂带(G带)上的数条断层显示出有左旋位移和倾滑位移.水位差表明有断层从观测井和灌溉井间通过.4年间,记录到6次急剧的水位变化(脉冲),这些发生在2—4天以上的水位变化,幅度为15—30厘米,似断层蠕动的结果.在观测井南300米处的G带上可能有两种蠕动:(1)阶梯状的倾滑位移;(2)左旋位移.利用指数函数、反正切函数和斜余弦函数变化的位错模型分析了水位变化、压力分布和断层位移.结果表明,该断层上的单个蠕动事件的位移量在1厘米以内.1978—1982年期间,累计蠕变值为20-50毫米,这取决于使用模型的特殊性.     

热带气旋运动和环境地转气流之间的关系

一、引言 50年代以来,对引导概念及其在预报的应用已作了许多重要的研究。多数研究表明,对流层中层的基本气流或深厚层的气压加权平均气流可以作为热带气旋运动的引导气流。许多作者讨论了涡旋运动对基本气流的偏差,但研究结果互相矛盾。这就导致了本文的研究。