勘察设计企业财务管理之我见

本文论述企业管理具有计划、控制、监督和资本运营作用；要不断完善成本预测、成本核算、成本分析等管理理念；合理调控筹集资金的配置和使用，提高资金效益和盈利水平，进一步提高勘察设计企业的综合实力。     

关于勘察设计企业资产经营和资本结构的思考

勘察设计院过去作为事业单位,主要是完成国家指令性任务,其资本结构一般不影响勘察设计单位的经营和运行。但在勘察设计单位改为企业并进一步按照《公司法》的要求改为有限责任公司或股份有限公司时,必然要考虑勘察设计企业在市场经济条件下的资本结构问题,这不仅仅是企业经营能力的体现,同时也关系到勘察设计院改为有限责任公司或股份有限公司后的股东结构问题,并对改制后的勘察设计单位股东收益分配产生根本性的影响。我们在这里仅对勘察设计企业资本构成的相关问题进行讨论,供大家参考。 一、经营定位与资产结构 对一个企业资本结构进行研究,我们首先应该     

上市勘察设计企业发展盘点

正"十三五"已到中期,深化改革正在进入深水区,未来环境发展的不确定性会越来越大,勘察设计行业面临的内外部挑战也越来越多。近年来,诸多勘察设计企业纷纷投身资本市场,希望通过资本和技术的紧密结合寻找新的成长路径,实现自身的跨越式发展。总体来看,登陆资本市场对勘察设计企业而言,机遇和挑战并存。一方面,上市为勘察设计企业带来了可观的资金支持,勘察设计企业可以迅速提升实力、做大做强,同时,上市也是对勘察设计企业管理水平、发展前景、盈     

勘察设计企业并购模式的选择

随着我国社会主义市场经济体制改革的不断深化,加入WTO后与国际市场融入度的不断加强,企业生存与发展的环境日益呈现出市场一体化、需求多元化、竞争激烈化的特征,为了拓展企业的业务范围、扩大企业规模以及提高市场的竞争实力以应对日益激烈的市场竞争,勘察设计企业面对严峻的市场和竞争环境,结合企业自身的资源、环境和并购目的选择合适的并购模式,通过借助并购等资本运营手段,将企业做大做强,增强其综合实力,有效参与全球竞争。     

勘察设计企业建设企业文化思路探讨

无论是我国加入WTO，还是勘察设计体制改革，都必将使勘察设计企业面临更加激烈的竞争、在市场竞争越来越激烈的信天，最持久的竞争力就是企业文化。本文通过分析环境的变化和勘察设计企业的特点，得出提炼勘察设计企业核心价值观的依据，并提出勘察设计企业的4个核心价值观：贴近顾客，以人为本、团队精神、创新精神。     

关于在电信勘察设计企业推行信息化的探讨

电信勘察设计企业的运营和管理注重业务、流程、管理、数据和系统的有机结合,注重全方位提高企业核心竞争力,实现企业的有序、高效、健康发展,信息化建设在其中起着不可替代的重要作用。本文详细阐述了电信勘察设计企业推行信息化的重要性、信息化建设的现状及实施要点,并以实际案例介绍了勘察设计企业信息化建设的模式及推广的意义。     

用设计引领产业化发展——国有勘察设计企业业务发展新思路浅析

正国有勘察设计企业发展现状近年来,由于国内外基础设施建设市场较好,大多数大型国有勘察设计企业的勘察设计业务基本处于饱和状态,而且受制于体制机制等原因,其劳动用工与做大勘察设计业务规模之间的矛盾日益突出,且已经成为束缚企业做大的瓶颈。与此同时,随着市场化的推进、投资模式的调整,特别是EPC、PPP等模式的兴起,提供涵盖勘察设计、施工、设备提供、运营维护等工程建设全过程的"一揽子"服务受到市场热捧,勘察设计企业若只承接仅占工程建设极小份额的勘     

运用信息技术 提高管理水平

本文针对目前我国勘察设计企业管理现状，指出信息技术的应用在勘察设计企业管理中的促进作用；它可使管理者树立规范化、制度化的工作方法，并在许多方面为勘察设计企业创造价值和效益。     

园林设计单位企业制度改革的探析

在国有企业的改革改制大潮中,勘察设计单位的企业制度创新也迫在眉睫。与一般国有企业不同的是,勘察设计单位是技术服务型企业,怎样优化和整合技术、人才、无形资本,是其在探索现代企业制度时必须思考的问题。上海市园林设计院的改革实践和今后的改革思路都是围绕这一课题展开的。     

改制上市必须基于企业发展长远目标

对工程勘察设计企业而言,需要从必要性和可行性两方面来考虑上市的问题。工程勘察设计单位作为知识密集型、智力密集型的企业,推动企业发展的首要因素是人力资本而非财务资本,本身并没有迫切的上市融资需求。而对于已经转型为工程公司,需要融资发展工程总承包业务的企业,以及转型为科技产业集团,     

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。     

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.     

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.