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.     

The Statistical Analysis of Migration of Strong Earthquakes-Taking the North China Region asan Example

The migration of strong earthquakes is an important research topic because the migration phenomena reflect partly the seismic mechanism and involve the prediction of tendency of seismic activity. Research on migration of strong earthquakes has mostly focused on finding the phenomena. Some attempts on getting regularity were comparatively subjective. This paper suggests that there should be indices of migration in earthquake dataset and the indexes should have statistical meaning if there is regularity in the migration of strong earthquakes. In this study, three derivative attributes of migration, i.e., migration orientation, migration distance and migration time interval, were statistically analyzed. Results in the North China region show that the migration of strong earthquakes has statistical meaning. There is a dominant migration orientation (W by S to E by N), a dominant distance ( ≤ 100kin and on the confines of 300 ～ 700km), and a dominant time interval ( ≤ la and on the confines of 3 - 4a). The results also show that the migration will differ slightly with different magnitude range or earthquake activity phase.     

塔上无人提引器的应用

塔上无人提引器,在60年代已被广泛使用,但由于经常发生“跑管”事故,故许多地质队没有继续使用。1987年,我队在绳索取心钻进工作中,使用塔上无人爬杆斜脱式提引器,5年中完成钻探工作量12363.63m,基本上消除了因提引器而造成的事故。所用钻机为THJ-500型或XU-1000型;钻塔为14.5m角铁斜塔;钻具为φ75或φ59绳     

微型核反应堆特性与应用

我国的微型核反应堆由中国原子能科学院研制，命名为MNSR-C(Miniature Neutron Source Reaetor)，已有三座MNSR—C型堆在国内外投入运营。地矿部山东省中心实验室的MNSR—C堆为我国地矿系统第一座原子核反应堆。该堆于1990年通过国家计量认证。微堆中子活化分析应用研究，中子辐照及中子应用研究已开始为国内、外提供服务。     

诗意的海洋学——记现代海洋科学创始人马修·莫里

马修·莫里(MatthewF.Maury,1806-1873),美国海军军官,海洋学创始人之一。他的《海洋自然地理》出版于1855年,至今已有150年的历史,是现代海洋科学最早的教科书,并成为世界科学出版物的一个里程碑。莫里从一名普通的海员成为一名海洋科学家,曾写下许多有关海洋科学的著作,《海洋自然地理》是他一生的巅峰之作。     

中国海洋学会理事会换届，国家海洋局局长王曙光当选为理事长

9月16日,中国海洋学会第六次全国会员代表大会暨2005年学术年会在宁夏回族自治区银川市隆重开幕。会议为期两天,国家海洋局局长王曙光、国家海洋局副局长陈连增、宁夏回族自治区党委书记陈建国、中国海洋学会第     

国家自然科学基金海洋科学项目基础资料数据库管理系统的设计

介绍了以ＦｏｘＰｒｏ为软件开发平台的国家自然科学基金海洋科学项目基础资料数据库管理系统的设计。该系统包括国家自然科学基金支持的海洋各分支学科项目的基础信息，如资料、人员、获奖情况等。并提供了查询和统计分析等功能，为管理部门管理和有效地利用海洋科学基金项目的基础资料提供了科学手段。     

东营城区高精度三维地震采集方法研究

根据东营城区内建筑物较多，环境干扰较大，地下构造复杂，断裂非常发育，目的层埋藏深，资料信噪比较低的特点，以地震老资料和钻井资料为基础，建立地震地质模型，利用射线追踪技术选取合适的观测系统参数。充分利用卫星数字地图，没计了灵活多变的观测系统，采用可控震源与炸药震源配合使用方法，及时对城区内地下面元的覆盖次数、方位角和炮检距的分布进行质量监控，利用现场处理系统对资料进行及时分析，提高了地震资料品质。所获得的东营城区高精度三维地震采集资料显示，其浅中层分辨率和中深层信噪比都有了明显改善，取得了良好的地质效果。     

海洋走航式单边连续观测地震折射波Δt解释方法--1种新的浅层折射单支时距曲线解释方法

在浅层工程折射地震测量中 ,通常采用相遇观测系统采集数据和相应的解释方法进行解释 ;对于单边观测采集方法由于与其相应的解释方法较少而少被采用。本文提出 1种方法简单、精度可靠、可直接利用同一点相邻 2排列 2次观测的初至折射时间并适合于海洋走航式单边连续观测系统的折射初至资料解释方法。其精度基本与同观测段的采用相遇观测的差异时距方法解释的精度十分接近。该方法即适合于人工解释又适合于计算机自动解释。     

中国港口在对外开放中的地位和作用

中国港口在对外开放中的地位和作用·吴志平陈泽卿（执笔中国的对外开放是从沿海地区开始的，在建立经济特区之后，相继推出１４个港口开放城市，并先后批准了５０多个沿海开放港口。此外，中国一手抓对原有港口和港区进行大规模的改建和扩建，另一手抓新建大中型港口，使...