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1.
董申保 《地质通报》2007,26(9):1072-1072
值此程裕淇先生文选问世之际,作为他的一个"私塾"弟子,追忆与先生交往50年来,包括陪同他去瑞典访问及多次去云南、华北各地野外考察的情况,摭拾数事,以备参考。  相似文献   

2.
正2009年6月,在成都召开的工程地质年会期间,正逢张咸恭先生90大寿。工程地质专委会为先生组织了祝寿庆贺会,会议安排我们原北京地质学院首届水文地质及工程地质系到会的学生致祝贺词。讲话后,肖树芳,杨华琨,周柔嘉和我起立,向张先生和师母深深行了三鞠躬!表示要在先生一百岁大寿之日,去北京为他祝寿。不曾想到先生竟然提前离我们而去!我想通过祝贺会上我们的一些讲话来寄托我们的哀思与怀  相似文献   

3.
年初先生谢世时,我正在参加全国人大会议,未能在他弥留之际看上最后一眼,心中总有一种隐隐的痛感.在此之前,先生已转辗病榻一年有余,我们这些做弟子的,却很少去看望他,惟恐他老人家化疗后抵抗力不足,我们把外面的病菌带给他.说实话,我们都没有最后的思想准备,先生尽管已九十高龄,但身体底子一直很好,国家在他罹病期间,又提供了最好的医疗条件,我们坚信他会挺过这一关.  相似文献   

4.
后记          下载免费PDF全文
后记裴文中先生说他自己是第四纪地质学家。他所从事的工作无论是古人类、旧石器、古脊椎动物和地层以及史前考古,无一不是从第四纪的角度去研究它的,而且他在这些方面推动了我国第四纪的研究,说他是我国第四纪研究的先驱和奠基人是恰当的。裴先生曾和笔者谈过他去法国...  相似文献   

5.
孟憲民 《地质论评》1936,1(3):339-346
引言箇舊是中國最大的金屬礦廠,平均年産七千噸的錫,價值國幣二千萬元左右。故凡旅行雲南的人無論是去參觀,遊歷,或是考察,調查,總得到箇舊去走一趟,丁文江先生在民國三年往雲南調查滇東礦産的時候也說「到雲南調查地質而不到箇舊,未免  相似文献   

6.
刘国纬 《水科学进展》2013,24(3):457-458
2010年仲夏,我收到陈家琦先生寄给我一本他的新作《云烟札记》。我一口气读完后在给他的回信中写道:"你所‘札记’的不是团团絮絮的云烟,而是一条绚丽的彩带。沿着这条彩带,我看到你气宇轩昂地从北京拐棒胡同走来,看到你风华正茂的少年和意气奋发的青年时代,钦佩你在战火纷飞年代投身革命的胆识,分享了你多彩的留苏生活,也勾起了自20世纪60年代以来我们相处的历历回忆。"2012年1月11日,我去北京宣武医院看望陈家琦先生,那时他已久卧病床,靠鼻饲维持生命,可当他见到我时,目光里依然闪烁着他那固有的乐观和幽默,而那时,他还不知道与他相濡以沫50余载的爱妻已在另一家医院先他而去了。我顿时难忍酸楚,背过脸去,然后才默默地和他对视着,许久,许久。2012年6月22日,陈家琦先生去世的消息传到了南京。痛哉!人生的最后时刻是多么脆弱和无奈啊!然而这都是因为在漫漫一生中,为事业已付出了全部的生命力,乃至弥留之际再也没有一丁点气力了。  相似文献   

7.
黄劭显  杜恒俭  卢振兴 《地质论评》1948,13(Z2):163-184
一、引言宁夏小松山铬铁矿系民国三十三年冬劭显与恒俭应宁夏建设厅之邀,调查贺兰山地质矿产时道经小松山麓所发现,民国三十五年夏劭显振兴得机又莅该地一次,惟两次皆限于时日兴经济,始终未能作详细之探勘。且因僻居西北,设备书籍两缺,携回标本无法整理,直至民三十五年春,劭显去京,始将标本之重要者携去,在程裕淇先生指  相似文献   

8.
我对白云鄂博铁铌稀土矿床的研究过程及往见新识   总被引:1,自引:1,他引:0  
白鸽 《地质学报》2012,86(5):679-682
80年前,丁道衡先生奉命去西北进行古生物考查研究工作,取道乌蒙草原,突然看到荒漠大地上有一座高耸美丽的神山,作了旅游参观之举.走到山脚下,就看到很多黑黑的滚石,到山上,更见有大块致密的磁铁矿石和红绿条带相间的赤铁矿石,就这样偶然发现了白云鄂博大型铁矿床.  相似文献   

9.
忆朱子元兄     
斯行健 《地质论评》1942,7(6):313-316
我和子元相识,是民国十四五年。那时子元和黄汲清李赓阳杨曾威诸兄是北大地质系二年级,我在四年级读书,朱骝先先生适自德国回来,在子元那一班教普通地质学,我也常去旁听,所以和子元汲清都很相熟。我因忝居‘老大哥’的地位,所  相似文献   

10.
热诚祝贺刘东生院士九十华诞——六十年相交与钦敬   总被引:1,自引:0,他引:1  
施雅风 《第四纪研究》2007,27(6):901-904
1从初识到建立中国第四纪研究委员会 欣逢我国第四纪科学成就最大者、楷模、长者和老友刘东生院士九十华诞,敬致最热忱的祝贺.回忆1946年冬在长江三峡东口江边与东生同志初次相识,他正随同侯德封先生勘查三峡大坝工程地质,我是在做大坝水库淹没损失调查,沿江步行去宜昌.  相似文献   

11.
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.  相似文献   

12.
13.
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.  相似文献   

14.
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″.  相似文献   

15.
从榴辉岩与围岩的关系论苏鲁榴辉岩的形成与折返   总被引:4,自引:1,他引:4       下载免费PDF全文
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。  相似文献   

16.
某高速公路下伏煤矿采空区稳定性分析   总被引:10,自引:0,他引:10  
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。   相似文献   

17.
摩擦桩基桩土间极限摩阻力取值问题探讨   总被引:1,自引:0,他引:1  
陈银生 《世界地质》1999,18(1):54-59
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。  相似文献   

18.
19.
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.  相似文献   

20.
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.  相似文献   

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