中部地区主要城市工业用地的地价杠杆作用

1经济发展和工业用地价格状况 我国经济政策上的中部地区就主要包括山西、河南、湖北、湖南、江西、安徽等6省。中部6省土地面积为102．7万km^2，人口3．63亿，分别占全国的10．7％和28．1％。近年来，在国家政策的大力支持和自身努力下，中部地区城市经济都取得了长足的发展，经济发展同时也带动了土地价格的上涨，但工业用地的价格并没有相应上涨。     

β-环糊精-1，2，5，8-四羟基蒽醌包结物荧光法测定铍

本文对1，2，5，8-四羟基蒽醌(THA)与镀形成配合物和THA进入β-环期精(β-CD)的内空腔与镀形成包结物这两种测定镀的荧光分析方法进行了比较，试验表明，后者的灵敏度和重现性有显着提高．选择性明显改善。详细研究了方法的测定条件．并应用于矿样中痕量镀的测定，结果符合质量要求。     

新型抗旱保水剂问世

一种能够提高干旱、半干旱地区植物栽培成活率，集促进植物生根、持水保肥、营养缓释等功效于一身的抗旱保水剂日前研制成功。据专家介绍。这一抗旱保水剂是中国地质科学院矿产资源研究所与中国农业科学院土壤肥料研究所合作，利用内蒙古鄂尔多斯市杭锦旗黏土资源（杭锦2号土），经过4年多的潜心研究和反复实验开发研制而成的。以小麦为例。是对照组的1.5-1.8倍。可使玉米果穗秃顶率下降1-2.8个百分点，穗粒数增加25-60粒，且长势明显优于施用其他复合肥。     

长乐-南澳剪切带晋江段构造岩特征及其构造变形机制

长乐-南澳左行韧性剪切带位于东南沿海，是酉太平洋大陆边缘构造带的一个组成部分。本文基于野外观察及室内分析，并借助透射电镜对变形石英的内部结构进行了观察，利用变形石英显微构造参数估算剪切带中的应力差值，由此探讨了形成构造岩的机制。     

试论经济欠发达地区如何做到经济发展与资源保护并举

百色市地处广西西部,是全国有名的连片贫困地区,集老、少、边、山、穷为一体,发展经济、提高人民生活水平尤其紧迫。随着西部大开发战略的实施和工业化、城镇化的快速推进,百色市相继上马一批水利、交通、能源和扶贫等重大基础设施项目,对资源需求迅速增长。资源是经济发展的基础,影响和制约着经济的发展,而经济形     

Mantle processes during ocean formation：Petrologic records in peridotites from the Alpine－Apennine ophiolites

Mantle peridotites were early exposed at the sea-floor of the Jurassic Tethys derived from the subcontinental mantle of the Europe-Adria system. During continental rifting and oceanic spreading, these lithospheric peri-dotites were percolated via diffuse reactive porous flowby melt fractions produced by near-fractional melting of the upwelling asthenosphere. Ascending melts inter-acted with the lower lithosphere, dissolving pyroxenes and precipitating olivine, and crystallized at shallower levels in the mantle column causing melt impregnation.Subsequent focused porous flow formed replacive dunitechannels, cutting the impregnated oeridotites, which were conduits for upward migration of MORB-type liq-uids. Melt migration produced depletionlrefertilization and significant heating of the percolatedlimpregnated mantle, i.e the thermochemical erosion of the litho-sphere. Impregnated and thermally modified lithos-pheric mantle was cooled by conductive heat loss dur-ing progressive lithosphere thinning and was intrudeaby MORB magmas, which formed Mg-rich and Fe-richgabbroic dykes and bodies. Alpine-Apennine ophiolitic peridotites record the deep-seated migration of melts which changed their compositions and dynamics during the rift evolution. The thermochemical erosion of the lithospheric mantle by the ascending asthenospheric melts, which induces significant compositional and rhe-ological changes in the lower lithosphere, is a major process in the evolution of the continent-ocean transi-tion towards a slow spreading oceanic system.