孤峰青青不纪年

早就听说仙都山有龙须草,黄帝炼丹得仙乘龙飞升,群臣攀龙须,须附而生草.这产仙草的仙山不由得令人神往.这次由楠溪江返程回杭,途中真的到了仙都山.仙都山,古称缙云山,那是因传说轩辕皇帝在鼎湖峰上置炉炼丹时,山的上空有绯红绯紫的五色云缭绕而得名.它属括苍山脉的北支,瓯江支流好溪从山间流过,呈九曲练溪,十里画廊.有奇峰一百六,异洞二十七,人们赞誉它集桂林之秀、黄山之奇、华山之险于一身.面对山门,这"九曲溪"、"十里廊"的长卷山水又如何着手游呢?幸亏有老朋友的领引,解决了这个难题,只花了半天时间,便游历了仙都山的精粹.     

信息荟萃

2005年度全省矿产资源补偿费征收入库首次突破2亿元本刊讯2005年全省各级国土资源管理部门抓住经济快速发展、矿产资源需求旺盛、矿产品价格上涨等有利时机,采取得力措施,进一步加大了对重点矿种和矿山企业缴费大户的矿产资源补偿费征收力度,征收率、入库率再创新高。截至2005年12月31日,全省矿产资源补偿费入库22016.41万元,为国土资源部下达我省任务的275.21%,首次突破2亿元大关,创历史最好水平。(开发处)商丘局多项举措落实徐书记批示精神本刊讯商丘市国土资源局结合年终工作总结,采取多种形式,认真传达学习贯彻省委徐光春书记批示精神。…     

The Lagoon of Venice： geological setting,evolution and land subsidence

The paper deals with the geological setting, history and subsidence of the Venetian Plain. Major attention is paid to the Pleistocene-Holocene stratigraphic sequence in the Lagoon of Venice, in relation to its origin that datesback to 6-7 kyr BP. Geological land subsidence, which played an important role in the origin and the evolution of the lagoon, and anthropogenic subsidence, that has recently assumed a major importance for the Venetian environment, are discussed. Considering also the sealevel rise, 23 cm loss in land elevation has occurred in the last century, leading to increased flooding events and environmental problems that require protective works.     

致密碎屑岩储层裂缝和产能预测的单井建模——以新场气田沙溪庙组为例

近年来，利用三维地震资料进行致密碎屑岩储层裂缝和产能的识别预测取得了一些进展，而这之中最重要也最基础的是单井裂缝和产能的建模工作。本以新场气田沙溪庙组致密储层为例，详细介绍了综合运用岩芯资料、测井资料和录井资料进行裂缝和产能单井建模的方法，为利用三维地震资料建立裂缝和产能的灰色遗传过程识别模式打下了良好的基础。     

广西环江县北山铅锌黄铁矿矿床发现史

广西环江北山铅锌矿床是由古人发现的，始于何时尚难断定。其采矿历史较悠久，据文献记载与考证，采铅锌矿炼银始于宋王朝，距今约８００年左右；炼锌始于明王朝，距今约３８０余年，１９７１年广西冶金地质勘探公司二一五队曾在北山一带普查评价褐铁矿，首先提出了该区褐铁矿＂属小型热液多金属铅锌硫化物矿床铁帽＂的概念。经广西地质局第九地质队（现广西第七地质队）１０年（１９７５－１９８６）的勘查，证实为一个以锌为主的大型多金属黄铁矿矿床，探明储量，其中锌、锗、黄铁矿为大型矿床规模，银、镉为中型矿床规模，铅、铁为小型矿床。为此该队荣获地矿部１９８９年度找矿成果二等笑。现今由中国有色金属工业总公司与广西壮族自治区人民政府合资兴建的北山铅锌硫铁矿已初具规模，一座新兴的矿山城镇已耸立在桂北群山之中，它将成为广西有色金属工业重要原料基地之一。     

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.     

印支运动的沉积学响应——以湖北秭归盆地中、上三叠统为例

通过对秭归盆地南缘中、上三叠统巴东组和沙镇溪组地层剖面的实测及1∶10万秭归幅地质填图发现,中三叠统巴东组在秭归盆地东南缘存在不同程度的缺失,秭归郭家坝一带,只沉积巴东组一段、二段地层。秭归楠家湾一带,整个巴东组全部缺失,上三叠统沙镇溪组直接覆盖于早三叠世嘉陵江组之上。而秭归盆地西缘沙镇溪、巴东麂子岩一带,巴东组发育齐全。上述现象表明,在早三叠世末期,由于印支运动的影响,巴东组地层出现了较大差异。沙镇溪组在沉积上继承了巴东组高低不平的古地貌特征,沉积厚度变化较大。上三叠统沙镇溪组与中统巴东组之间,在盆地不同的部位可呈现出整合或平行不整合的接触关系,而不存在断层接触关系。     

鲁苏榴辉岩的地球化学

以微量元素、稀土元素、Ｓｒ和Ｎｄ同位素变异特征为依据，确定鲁苏榴辉岩为多成因、多来源和多阶段，指出主要是在印支期扬子陆块与华北陆块碰撞造山作用过程中，挤入的上地幔碎片以及不同原岩类型的壳内高压变质岩碎块。燕山晚期的区域构造热事件使得某些榴辉岩的同位素体系再平衡。     

海河口演变特性分析

总结了海河口的历史变化过程，通过实测资料分析了海河口建闸后的淤只情况、目前的淤积形态及其主要原因，认为河口建闸３０ａ来，在径流量逐渐减小的条件下，潮汐水流是塑造闸下淤积形态的主要动力。