信息化对区域经济发展的组织作用

在科学认知信息化多重形态(包括要素形态、技术形态、设施形态、经济形态和运动形态)特征的基础上,分别阐述其对区域经济发展的组织作用。信息资源通过改变原有生产要素的结构对区域经济发生作用;信息技术不仅可推动传统产业的升级换代,还将企业和贸易扩展到网络空间;信息基础设施拓展了信息通达性,促进了主体间的信息交流,并使原有的区域空间结构发生了微调下的整体增强变化;信息产业在直接促进区域经济增长的同时,还通过前后向联系带动其他产业发展;信息流对物流、人流、资金流和技术流具有组织作用,有助于实现流动的组织和组织的流动。     

一种能大量消耗粉煤灰的多孔材料的初步研究

以武汉青山热电厂的粉煤灰为原料制作多孔材料.其中的两种样品的孔隙率分别为45.8%和61%.该材料可作为一种消音和隔热材料用于高速公路和城乡建设, 从而大量消耗粉煤灰以达到保护环境的目的      

青藏高原狮泉河-康西瓦地区 1:100万区域重力调查成果

利用最新取得的区域重力资料,参考航磁、遥感、区域地质资料,对青藏高原狮泉河-康西瓦地区重力场分区、断裂构造体系、构造单元、局部异常、深部构造、成矿远景区(带)等进行了研究.对阿尔金走滑断裂西南端的走向和延伸提出了一些新的看法;讨论了2条重力低值带的成因;推断了班公湖-怒江结合带下部莫霍面隆起的高度,从重力角度提出了对班公湖-怒江结合带的认识;认为青藏块体在拼合后地壳有2个加厚中心;新圈定了一个中、新生代沉积盆地,并进行了初步研究;结合地质、矿产、航磁等资料,初步划分出4个成矿远景区(带).     

新疆拜城新近系含铜岩系沉积体系及沉积环境

新疆拜城地区发育一套新近纪巨厚的陆相碎屑沉积岩系,其中康村组中上部含规模较大的沉积型铜矿,康村组的沉积环境及演化过程对铜矿的形成具有重要意义。基于野外和室内详细的沉积学研究,查明研究区新近系吉迪克组、康村组和库车组总体上为陆相沉积体系,主要包括冲积扇-扇三角洲沉积体系和湖泊沉积体系两大类型,划分为扇三角洲平原、扇三角洲前缘、前扇三角洲、滨浅湖和膏盐湖亚相及若干沉积微相。研究表明研究区康村期主要发育扇三角洲沉积,矿区主要含矿层位于康村组上部红色岩系向灰色岩系转变,沉积环境从扇三角洲前缘亚相到滨浅湖亚相过渡的层位上。     

Geochemistry of overbank and high-order stream sediments in Belgium and Luxembourg: a way to assess environmental pollution

A geochemical survey of Belgium and Luxembourg was carried out as part of an international research project entitled ‘Regional geochemical mapping of Western Europe towards the year 2000'. The aim of this research was to map regional background geochemical patterns based on pristine or at least pre-industrial overbank samples and to deduce regional information on the degree of environmental pollution of floodplain and present-day river sediments. Over the entire study area (about 33,000 km²), 66 overbank sites have been sampled. Catchment areas range between 60 and 600 km². At each site an overbank profile has been dug out in the immediate vicinity of the river and described in detail. A first composite sample was taken 5–25 cm below the surface. This sample is supposed to represent deposition over the last centuries. Human interferences in this interval are often inferable based on changed sedimentary characteristics and the presence of anthropogenic particles such as charcoal, slags and brick fragments. A second composite sample was taken at depth, usually >1.5 m below the surface over an interval of about 20 cm. In most sites, the profile characteristics allowed to assume pre-industrial or even pristine conditions for this lower overbank sample. In some profiles this was confirmed by ¹⁴C-dating and/or by the absence of anthropogenic particles. Finally, a present-day stream sediment was sampled on the site to infer the actual pollution status. After drying at 80°C, disaggregation and sieving, the <125 μm fractions of the three sediment samples were analysed by XRF for major elements and several trace elements. Lower overbank samples generally show a direct link with the geological substrate and allow to assess natural background concentrations. Results from the mapping exercise as well as from the statistical analyses display a clear contrast between the northern part of Belgium where Cenozoic unconsolidated sandy and silty formations dominate which are especially vulnerable for erosion, and the southern part of Belgium and Luxembourg where Paleozoic and Mesozoic sandstones, carbonates, marls and shales are the prevalent lithologies. Here the shales are the most intensively eroded lithologies. This is especially reflected in the element patterns of Al₂O₃, MgO, K₂O, Ga, Ni, Rb, Sc and V which negatively correlate with SiO₂. Despite the human related pollution, the geological contrast between north and south Belgium is still recognisable in the geochemical pattern of the upper overbank and present-day stream sediment samples for the above-mentioned elements. Furthermore there is a clear increase in heavy metal contents (Zn, Cd, Pb, Cu), As and in certain locations in Ba from the lower to the upper overbank sediment, as well as to the present-day stream sediment. The relative increase in element content allows to assess the degree of pollution and helps to define those drainage areas where more detailed research is needed.     

赣南大富足岩体岩石地球化学特征及其构造环境判别

大富足岩体位于武夷山隆起带南段,为一多期复式花岗岩侵入体,岩体由当风凹、泮塘、春坑、荷树岽、土桥凹、水隘背、新村、沙告、先坑、石教坪共10个单元所组成,固结指数、Rb/Sr和K/Rb比值以及稀土配分型式反映侏罗纪的石教坪、先坑、沙告单元和二叠纪的泮塘、当风凹单元均为相对独立的没有分异演化关系的单元,而由新村、水隘背、土桥凹、荷树岽、春坑单元组成的三叠纪富城超单元则为同源岩浆房岩浆过程的产物。根据矿物成分和化学成分和微量元素特征判别,岩体属CCG或同碰撞花岗岩类型,形成于大陆碰撞的构造环境,扬子板块与华夏板块在二叠-侏罗纪的大致沿着杭州-诸广山-花山这条缝合带发生的陆内A型俯冲与这种构造环境相呼应。     

古特提斯东昆仑活动陆缘及其区域成矿

东昆仑地质构造特征、石炭—三叠系火山 -沉积建造及区域岩浆作用研究显示 ,海西 -印支期 ,该区属于古特提斯北侧活动陆缘的组成部分。活动陆缘区特殊的沉积环境、区域岩浆活动及构造变形动力等作用 ,构成了区域矿产形成的主要背景和控制因素 ,从而使不同类型和元素组成的矿床得以形成 ,并表现区域成矿的总体分带规律。     

江苏数字地震台网P波谱震级和地震辐射能的计算

基于江苏数字地震台网的宽频带记录,对38次M≥5.0地震的P波谱震级M_P进行测定,对地震的辐射能量进行了估算。结果表明:本文测定的M_P与中国地震台网中心(CENC)测定的MS、德国地学中心(GFZ)测定的MW具有很好的一致性,与该2种震级之间的平均偏差分别约为0.17和0.10级,基本小于世界主要地震机构之间对同一震级的测定误差(约0.2级);同时,基于M_P估算的地震辐射能与基于修正G-R关系由MS震级换算获得的结果十分接近,两者平均能量之比约为1.1,表明M_P与P波群(P+pP+sP)能量流是基本等效的。因此,基于宽频带数字记录测定中强地震的P波谱震级以及地震辐射能是可行的,且测定过程简便。     

毛乌素沙地西南缘灌丛沙丘沉积物的粒度和元素特征

对毛乌素沙地白刺(Nitraria tangutorum)灌丛沙丘沉积物粒度和元素特征进行了采样分析.结果表明:灌丛沙丘沉积物来源单一,几乎全部由丘间地物质组成,其粒度和元素特征与丘间地物质极其相似;相对而言,灌丛沙丘沉积物比丘间地物质含有更多粗颗粒物,主要因丘间地可做跃移运动的中沙和细沙更易被灌丛阻挡而堆积;灌丛沙丘沉积物中大部分元素含量比丘间地物质低,主要因这些元素易被淋溶迁移到丘间地富集;灌丛沙丘发育以来,虽然其沉积环境存在波动,但相对稳定,未发生过显著变化.     

西藏扎布耶湖ZK91-2钻孔沉积特征与气候环境演化

扎布耶盐湖位于西藏高原腹地,1991年在其南部干盐滩中钻取了20m深湖相沉积,以5～10cm/个的密度进行高分辨率取样,详细探讨了沉积标志、矿物组合（尤其Mg、Ca、Li碳酸盐）、干旱与潮湿两种气候类型的元素组合等气候环境指标,推导了晚更新世以来该湖区湖面涨缩、水质咸谈及气温高低变化。