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201.
根据钻石的光学性质、导热性、亲油疏水性、硬度与工艺钻点,以及钻石的某些表面与内部特征,利用10倍放大镜肉眼可以比较有效地鉴别钻石及其模仿品。  相似文献   
202.
福建省构造运动,构造层划分及其主要特征   总被引:10,自引:0,他引:10  
李兼海 《福建地质》1998,17(3):115-130
研究构造运动及构造层特征是查明地壳构造演化历史的重要证据,从福建省目前建立的地层序列分析,自古元古代以来,省内初步可划分出15次构造运动,并分别归属迪口,晋宁,加里东,印支,燕山,喜马拉雅6个构造旋回,文中对地震旦纪地层次建立构造地层单位,并阐述了各构造运动,构造旋回,构造阶段和构造层,亚构造层的基本特征,较系统地反映了福建省地壳构造演化历史。  相似文献   
203.
大地测量在研究青藏地壳运动及其机制中的作用   总被引:2,自引:0,他引:2  
基于对GPS和重力测量数据的分析,扼要地介绍了重力与内部构造关系,大地水准面的场源与其动力效应等方面的研究内容和方法。总结了利用重力与形变资料研究青藏地区的现代地壳运动及其动力机制的研究结果。  相似文献   
204.
When estimated from measurements of introduced tracer particles, the rate of surface soil movement tends to be greater than the natural rate for equivalent particles on the same site. This consistent overestimation is greatest in the period following tracer introduction and leads to a measurement bias that may be as high as 300 per cent. The magnitude of the bias decreases with time, as the tracer is incorporated into the surface material, but remains detectable statistically for more than a year on some low-angle sites.  相似文献   
205.
���������ֽ�ؿ��α������о�   总被引:1,自引:1,他引:0  
?????????????????????У???????????????????????????????о????????????α????????????????????????????????λ???????????С?????????????????????????????????????????У??????????λ??????????????????????????????????????????????????????????????????????????????????????????????????????????????Ч??????????????????????????????????????????????????????е????????С??????????????????????????α????????????????????????????????????????????Ш????????????  相似文献   
206.
山东地壳运动GPS观测网的建设与初步结果分析   总被引:2,自引:2,他引:0  
简述山东地壳运动GPS观测网的建设和数据处理的基本方法,并对系统所得的初步结果进行分析,分析表明,该系统可产出连续、高精度的GPS基准站三维坐标及基线数据,可为地震监测和地壳运动的科学研究提供良好的GPS数据素材。  相似文献   
207.
人口移动与区域经济格局变动   总被引:2,自引:2,他引:0  
陆玉麒 《地理研究》1990,9(1):41-46
人口移动是我国近几年发生的重要社会经济现象之一,其机制是东部地区人多地少的推力与西部地区产业结构性空缺的吸力,以及国家对后者特定的工资与粮食政策。它对地域分工格局的变动产生着重大影响。  相似文献   
208.
???????????????????о??м????????????ε??????????????????????????????????????????????????????Э??????????????????????????б????????С??????????????????????????????????????????????о??????????????????????????????????????Σ?????б?????????????  相似文献   
209.
Knowledge of long-term movements of water-masses in the English Channel has been substantially improved using hydrodynamic modelling coupled with radio-tracers studies; nevertheless, the precision of results so obtained is still largely dependent on measurement precision. New tools are now available to make more accurate determinations of radio-tracer distribution: (1) Repositioning of station locations at the same tide reference-time, giving a homogeneous spatial data set, coupled with the possibility of interpolating and quantifying the amounts of dissolved radioactivity flowing through the English Channel; (2) the first measurements of tritium (3H) in seawater on a large scale in the English Channel demonstrate that this fully conservative radionuclide is a clearly identifiable marker of industrial releases; (3) recent campaigns carried out during the FLUXMANCHE II CCE (1994) programme show the general distribution of dissolved radionuclides 137Cs, 134Cs, 60Co, 125Sb, 106Ru and 3H in the English Channel and the Irish Sea; and (4) the re-utilisation of data from previous campaigns (1983, 1986, 1988) provides indications, at any given location in the English Channel, about the average dilution and distribution of releases derived from the La Hague reprocessing plant. Excesses and losses of radionuclides are now quantified with respect to known source terms; estimates of losses are provided for non-conservative radionuclides, while an excess of 137Cs was observed in the English Channel during the period 1983–1994. This excess, which has the same order of magnitude as the quantities released from La Hague plant in the English Channel, could be explained by about 1% of the Sellafield reprocessing plant releases entering the Channel. These results confirm and give a more detailed picture of the previously known distribution of water masses in the English Channel. They lead to clear information about transit times and dilution at this scale, and provide directly comparable data for the validation of hydrodynamic models.  相似文献   
210.
We examined whether adults of three species of sea urchins species (Diadema antillarum, Arbacia lixula, and Paracentrotus lividus) exhibit a consistent depth-dependent partitioning pattern on rocky reefs of the Canarian Archipelago (eastern Atlantic). Hydrodynamic experiments were carried out to quantify the resistance to flow-induced dislodgement in these three species. We tested the model that different morphology can result in habitat partitioning among these sea urchins. Abundances of D. antillarum increased with depth. In contrast, A. lixula and P. lividus showed the opposite zonation pattern, coexisting in high abundances in the shallowest depths (<5 m), and occurring in low densities in the deepest part of reefs (>7 m). Both A. lixula and P. lividus had greater adhesion-surface to body-height ratios than D. antillarum. Similarly, A. lixula and P. lividus showed a greater ability to resist flow-induced dislodgement compared with D. antillarum. The mean “velocity of dislodgement” was 300% and 50% greater for A. lixula and P. lividus, respectively, relative to D. antillarum, for any particular size. As a result, A. lixula and P. lividus are better fitted to life in high-flow environments than D. antillarum. We conclude that the risk of dislodgement by water motion likely play a relevant role in the vertical distribution patterns of these sea urchins in the eastern Atlantic.  相似文献   
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