致力产业结构调整促进建筑业健康快速发展

通过近两年的建筑业行业组织结构优化调整，目前，青岛市共有建筑业企业1277家，其中总承包企业328家、占企业总量的25％，专业承包企业534家、占企业总量的42％，劳务分包企业415家、占企业总量的33％，建筑业行业组织结构初步趋于合理。1277家建筑业企业中，国有企业36家、集体企业63家，企业改制面达92％；     

增强企业活力措施的研究

企业是一个有机生命体，企业活力是企业生命力的重要体现。企业的生存力、成长力、再生力是企业活力的重要组成部分，企业活力是三者的合力。三者都相互依赖，综合体现了企业活力；凡是影响三者的因素，皆可影响企业活力。本文正是通过对影响企业生存力、成长力、再生力的因素进行分析，从而提出一些增强企业活力的措施。     

对长沙本土房地产品牌建设的探讨

近年来，长沙房地产企业之间竞争激烈，一方面是外来品牌的入侵给本土企业带来了压力，另一方面是许多本土企业自身实力、规模较小。本土房地产企业要在激烈的竞争中有效地应对外来品牌，必须加强自身的品牌建设，提高品牌的个性、内涵、知名度、美誉度。从国内房地产发展整体情况着眼，着重分析本土房地产企业的现状以及在品牌建设中存在的问题，然后从品牌定位、品牌个性塑造等方面，为本土房产企业发展提供有益的建议。     

勘察设计企业知识管理模式探讨

本文遵循理论与实际相合的指导思想，从知识管理的理论出发，围绕勘察设计企业的生产经营特点，综合运用管理学、战略管理、生产营运管理、人力资源管理、技术创新、组织行为学等学科知识，分别从组织结构、激励机制、企业文化、信息平台四个方面对勘察设计企业知识管理模式进行系统论述，促进企业核心竞争力的建立，推进企业创新和发展。     

以先进性教育为契机 狠抓落实 确保完成全年工作任务——赵传宝在局2005年经济工作会上的报告摘要之二

1、继续推进产权多元化改革。体制创新是增强企业活力和加快企业发展的动力。产权多元化改革是企业改革的核心。地勘单位要选择有条件的企业，进行产权多元化改革。二六三大队要以筹建新加坡（吉安）食品医药科技有限责任公司为契机，与外商合资合作，打造混合所有制经济，建立现代企业制度。其他单位也要根据所属企业情况，积极、稳妥推进企业改制工作。局工贸总公司要完成核工大厦股份制改造的前期工作。     

浅谈吉林省企业水平衡测试

本文简述了企业取、用、耗、排各种水量的平衡关系，通过水平衡测试，分析企业用水工艺、用水水平、用水效率以及节水潜力等，对吉林市某企业进行了实例分析，进而提出企业节水措施有关建议。     

对创建学习型企业的几点思考

在世界经济环境和企业环境发生翻天覆地变化的今天，企业之间的竞争已发展为全方位、多元化的竞争。善于学习，善于思考，迅速把新知识应用于企业发展，已成为企业成功的关键。“比别人学习得更快、更好、是未来唯一持久的优势”。因此，创建学习型企业，是现代企业参与知识经济时代竞争的必然选择，也是今后摆在每一个企业面前的重要课题。     

浅谈广西建筑业的改革与发展

通过2001年下半年的建筑施上企业资质重新就位，我区建筑施工企业在体制、资产、人员方面发生了很大变化，施工企业由过去占绝大多数的国营、集体两种性质的企业，通过体制改革、资产重组、分立，变为现在占绝大多数的股份制企业和民营企业。企业资产增强，技术水平和管理水平上了一个新台阶，企业的经营更加灵活，     

论煤炭地质企业党政工三者关系

转换经营机制，建立现代企业制度，已成为煤炭地质企业改革的迫切任务。在现代企业制度下，如何理顺党政工三者的关系则成为企业建设中的重要课题。笔者认为，企业改革，领导体制更新，党组织、行政、工会和职工群众在企业活动中的各自职责将更加明确，党政工相互关系会更加协调。１党的领导与行政负责的关系在煤炭地质企业领导体制中，党的领导是指基层党组织在企业中处于政治核心地位，在思想形态上把握企业的政治方向，坚持党的路线方针。其主要任务是搞好党的思想、组织和作风建设，领导企业的思想政治工作和精神文明建设，保证党和国家…     

坚持科学发展观促进企业健康、持续发展

从四个方面论述了企业开展诚信示范创建工作的经验和体会，阐明了信用、诚实对于设计人员个人、设计企业乃至整个行业的重要作用，强调了只有坚持科学发展观，构筑全新、完整的企业诚信体系，才能促使企业健康、持续地发展。     

Unity of the national and the international in the socio-cultural development of the peoples of the USSR

International unity is becoming ever stronger in this country owing to an increasing similarity in the development of the cultural environment. This comprises the provision of all the country's republics with a sufficient number of schools, theatres, and other institutions and cultural information media in accordance with the needs of the population. An important part is played by the rise in ‘the general educational level, as well as the level of professional qualifications and skills. Among all the Soviet nations and nationalities, this rise being more rapid among formerly backward peoples. Prominent among the factors of internationalization is the progressive development of the nationalities’ cultural resources, while professional culture is being increasingly brought within the reach of the masses.The implementation of the nationalities policy promotes the all-round development of all Soviet nations and nationalities, their drawing together, the upsurge of the individual capabilities of every Soviet citizen.     

Global repeating events in the history of the Earth and the motion of the Sun in the Galaxy

Chronological analyses of correlations between certain global repeating events (mass extinctions of marine organisms, meteorite impacts, and flashes in the frequency of geomagnetic reversals) during the Phanerozoic Eon and the motion of the solar system in the Galaxy are presented for five rotationally symmetrical models for the regular Galactic gravitational field. Thirteen of sixteen mass-extinction events can be described by a repetition interval of 183±3 million years. This is in agreement with the anomalistic period (interval between two subsequent passages of the Sun through the apocenter of its Galactic orbit) in the model of Allen and Martos. The positions of the minima and maxima in Gaussian functions approximating the frequency distribution for geomagnetic reversals also agree with the times of passage of the Sun through the apocenter and pericenter, respectively, of its Galactic orbit in this model. The maximum in the distribution of the deviations of the dates of mass extinctions from the nearest dates of impacts of large, crater-forming bodies is close to zero, providing evidence that many such events are correlated. As a rule, extinctions follow impact events. The impacts of large bodies have occurred most often when the solar system passes through the Galactic plane, while mass extinctions occur more often at some distance from the Galactic plane (about 40 pc). As a rule, intervals of increases in the frequency of geomagnetic reversals coincide with dates of impacts of large bodies. At the same time, these intervals do not show a clear correlation with the dates of mass extinctions. The intensity of mass extinctions, like the energy released by impacts, is consistently higher in periods when the Sun is moving from the apocenter toward the pericenter of its orbit, than when it is moving from the pericenter toward the apocenter. Thus, there is evidence for a variety of relationships between repeating global events in the Phanerozoic and the motion of the Sun in the Galaxy. Long-period variations in the frequency of geomagnetic reversals are correlated with the orbital motion of the Sun, and increases in the frequency of geomagnetic reversals are correlated with impacts. Mass extinctions are correlated with the impacts of large bodies, whose motions may have been perturbed by clouds of interstellar material concentrated toward the Galactic plane and by the shock front associated with the Perseus spiral arm, through which the solar system passes. The velocity of the Sun relative to the spiral pattern is estimated.     

Deviation of the major axis of the inertia ellipsoid of the Moon from the direction toward the Earth

It is known from observations that the center of mass of the Moon does not coincide with the geometric center of its figure, and the line connecting these two centers is not aligned with the direction toward the center of the Earth, instead deviating toward the Southeast. This stationary deviation of the axis of the inertia ellipsoid of the Moon to the South of the direction toward the Earth is analyzed. A system of five linear differential equations describing the physical libration of the Moon in latitude is considered, and these equations are derived using a new vector method taking into account perturbations from the Earth and partly from the Sun. The characteristic equation of this system is obtained, and all five oscillation frequencies are found. Special attention is paid to the fifth (zero) frequency, for which the solution of the latitude libration equations are stationary and represents a previously unknown additional motion of the rotational axis of theMoon in a cone with a small opening angle. In contrast to the astronomical precession of the Earth, the rotation of the angular-velocity vector is in the positive direction (counter-clockwise), with the period T ₃ = 27.32 days. On this basis, this phenomenon has been named “quasi-precession.” This quasi-precession leads to a stationary inclination of the major axis of the inertia ellipsoid of theMoon to the South (for an observer on Earth), making it possible to explain one component of the observed deviation of the center of mass of the Moon from the direction toward the Earth. The opening angle of the quasiprecession cone is approximately 0.834″.     

从榴辉岩与围岩的关系论苏鲁榴辉岩的形成与折返

位于华北和扬子两板块碰撞带中的苏鲁榴辉岩形成的温压条件不但是超高压，而且是高温。榴辉岩的PTt轨迹表明其为陆-陆磁撞俯冲带的产物。榴辉岩的区域性围岩花岗质片麻岩为新元古代同碰撞期花岗岩，榴辉岩及其他直接围岩皆呈包体存在于其中，并见新元古代花岗岩呈脉状侵入榴辉岩包体中。区域性围岩新元古代花岗岩的锆石中发现有柯石英、绿辉石等包裹体，表明新元古代花岗岩的组成物质也经受过超高压变质作用，且榴辉岩与围岩新元古代花岗岩的锆石U-Pb体系同位素年龄基本相同。但新元古代花岗岩所记录的变质作用和变形作用期次（或阶段）却少于榴辉岩。椐上述可得如下推断：超高压榴辉岩与新元古代花岗岩岩浆是同时在碰撞带底部（俯冲板块前部）形成的；榴辉岩的第一折返阶段是由新元古代花岗岩岩浆携带上升的，其第二折返阶段是和新元古代花岗岩一起由逆冲及区域性隆起而上升，遭受剥蚀。     

某高速公路下伏煤矿采空区稳定性分析

在论述某高速公路下伏砦脖煤矿采空区地质、采矿和工程地质特征的基础上, 进行了稳定性数值模拟分析, 定性与定量地分析与评价了该煤矿采空区的地表变形特征及稳定性。研究结果表明: 该煤矿采空区的变形尚未完成, 对拟建的高速公路将产生很大的危害, 必须采取相应的工程治理措施。     

摩擦桩基桩土间极限摩阻力取值问题探讨

通过对广珠东线高速公路横沥大桥的试桩及土体的工程地质条件分析,总结出影响摩擦桩基桩土间极限摩阻力取值的一般问题以及解决问题的方法和措施。     

Paleomagnetic implications on the evolution of the tethys belt from the atlantic ocean to the pamirs since the triassic

We first re-examined the apparent polar wander curves for stable Eurasia and Africa since the Triassic. These curves were then combined together with curves of North and South America according to the kinematics of the Atlantic ocean and a synthetic polar wander curve was given. Then, most of the paleomagnetic results from the Tethys mobile belt, from the Atlantic to the Pamirs, were analysed.Several groups of plates, microplates and blocks can be seen. First, relatively stable regions like Maghreb and Sicily, which have not moved much. Then we have a group formed by Iberia, Sardinia, Italy and, to a lesser extent, Corsica and the Western and Central Alps. For these blocks, movements are anticlockwise rotations chiefly driven by the anticlockwise rotation of Africa, but they are sometimes stronger.To the east, a major change takes place. The north of the Aegean Sea and the Ionian zone are clockwise rotated and these rotations are recent: Oligocene-Miocene for the first part, Pliocene to the present for the second part.A major problem arises in Turkey, Caucasus and Iran. Paleomagnetic results indicate a position far to the south of Eurasia, and, at the same time, geological evidence is in favour of a position close to Eurasia. We discuss these discrepancies.     

On the consistency of proposed models for the Pyrenees with the structure of the eastern parts of the belt

The structure of the eastern Pyrenees consists mainly of south-directed thrusts involving basement and cover rocks. An antiformal stack developed by the piling up of basement thrust sheets which outcrop in the Axial zone. These structures account for a thin-skinned thrust model rather than a vertical fault model in which the Axial zone would be essentially autochthonous, and the North-Pyrenean fault the axial plane of a fan thrust system. New data from the Eastern Pyrenees and the thin-skinned model suggest that(1) the structure east of the Pedraforca nappe is similar to that of the Central Pyrenees; (2) the cover rocks of the South-Pyrenean units and of the Axial zone-after restoration—built up a northwards-thickening prism consistent with the existence of a unique Pyrenean sedimentary basin during Mesozoic time; (3) the Axial zone is only a complex antiformal stack developed as a part of South-Pyrenean system related to the Paleogene thrusting-tectonics. The Axial zone palaeogeographic area had no special meaning during Mesozoic time.