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1.
通过建立高频可控震源与大地相互作用的物理模型和数学模型,得到了高频可控震源的动力学方程,分析了高频可控震源与大地震动耦合过程,给出了不同物理参数对可控震源系统幅频特性影响的曲线,为高频可控震源系统的设计提供了理论依据。  相似文献   

2.
EH-4系统观测资料的非远区场校正研究   总被引:6,自引:1,他引:6  
EH-4系统实测的卡尼亚视电阻率在非远区场时应作必要的校正。基于导出的EH-4系统的卡尼亚电阻率ρxy和ρyx的表达式,采用多项式分段逼近的方法,建立EH-4系统测深数据的全频域的视电阻率算法。根据建立的算法对均匀大地、二层大地和三层大地模型的EH-4系统测深数据进行非远区场校正的结果表明:均匀大地时,全频域的视电阻率与真电阻率吻合很好,D型、K型和Q型断面的视电阻率曲线与MT法的接近,G型、H型和A型的视电阻率曲线得到很大改善。  相似文献   

3.
周友松  金昕 《地球科学》1994,19(4):509-517
在青海当金山口-四川黑水剖面(GGT)区带内大地热流测量的基础上,采用布拉德数值分析法对地温梯度进行了三维地形校正,对中-新生代孔隙岩石热导率样品进行了饱水校正,取得了满意的效果,获得了10个可信的大地热流值。青藏高原北部平均热流值为51mW.m^-2,变动于35~78mW.m^-2,柴达木北缘构造带和巴颜喀拉构造带处于二者之间,平均为49mW.m^-2。这种分布不均72mW.m^-2,柴达木北缘  相似文献   

4.
使用可控震源应注意三方面的问题:一是与大地的耦合,二是参数的最佳选取,三是在保证野外采集工作量近似不变情况下,提高地震剖面质量。解决方法是:配备可控震源力控装置、改变表层介质波阻抗可消除震源脱耦现象;选取参数应考虑清晰度、分辨率、信噪比,避免虚像出现在有效记录范围内;在野外数据采集时应减少振动次数、增加覆盖次数并注意压制不规则干扰和噪声,以提高地震剖面质量。  相似文献   

5.
一九九三年五月在日本西部的Kinkai湾复垦地段,用2m点距做了一条760m长的反射地震12次叠加剖面。用一台具50-1000Hz扫描频率的轻便型振动器作地震源,用100Hz的检波器作接收器。通过使用常规的数据处理程序,在10-50m深度范围内对三个明显的界面作了清晰的填图。  相似文献   

6.
利用人工振动技术增加石油产量的机理之一是地层的机械共振作用。提出了一种简化的地层模型,并将其转化为一个双自由度有阻尼振动系统。研究了各种不同厚度的地层的振幅与振动频率的关系、共振频率与固有频率的关系以及品质因素 Q 对地层振幅和共振频率的影响,得出有意义的结论。  相似文献   

7.
恒山鹿沟金矿形成的物理化学条件及同位素地球化学   总被引:2,自引:0,他引:2  
本文对恒山东段鹿沟金矿形成的温度,压力,fCO2,fO2,成矿溶液的成分,盐度,pH值,Eh值进行了系统的论述。同时利用硫、铅、氧、氢、锶同位素资料,对成矿时代、物质来源进行了论证,得出成矿物质主要来自围岩,成矿溶液以变质水为主的结论。溶液性质属Na^+-Ca^2+-CI^- -SO^2-4型,富CO2,高盐度,偏酸性。成矿时代与区域变质年龄一致,为2214.5±64.1Ma。燕山期岩浆活动对其有  相似文献   

8.
高向群  黄茂桓 《冰川冻土》1994,16(3):259-264
应用人造多晶冰开展了正弦振动荷载和恒荷载压缩蠕变实验。振动应力的最大值为0.50MPa,最小值为0.34MPa,对时间的平均值为0.42MPa,实验频率在10^-2-5Hz范围内变动。恒荷载实验的初始应力为0.42MPa,实验温度一律为-1℃。当应变很小时(低于~0.14%)样品在一个振动周期内发生的可恢复应变随应变的增加而增加。一个振动周期内可恢复应变的量级为10^-4。振动荷载下样品最小平均应  相似文献   

9.
应力波传递理论与弹性波动原理适用于桩基振动的动力分析,作者从工程学的等效观点出发,将完整桩土系统与破损桩土系统分别等效简化为单个自由度的“质量-弹簧-阻尼”模型与多单元(多自由度)的“质量-弹簧-阻尼”模型研究讨论。结果表明:完整桩或破损桩的理论模型结果分别与实际的好桩或断桩振动波形曲线吻合,并通过付氏变换后得到桩基的响应函数或频谱函数作桩基动力学参数反演计算,具有简单、快速、实用、准确等优点。  相似文献   

10.
可控震源参数选择及在煤田勘探中的应用   总被引:1,自引:0,他引:1  
介绍了如何选择可控震源的扫描长度和震源台数、振动次数以及扫描频宽等参数,指出采用数台可控震源组合,增加扫描的总时间和利用相关技术是提高可控震源地震资料信噪比的有效方法,也是可控震源取得成功的关键。  相似文献   

11.
Pant-y-ffynnon Quarry in South Wales yielded a rich cache of fossils in the early 1950s, including articulated specimens of new species (the small sauropodomorph dinosaur Pantydraco caducus and the crocodylomorph Terrestrisuchus gracilis), but no substantial study of the wider fauna of the Pant-y-ffynnon fissure systems has been published. Here, our overview of existing specimens, a few described but mostly undescribed, as well as freshly processed material, provides a comprehensive picture of the Pant-y-ffynnon palaeo-island of the Late Triassic. This was an island with a relatively impoverished fauna dominated by small clevosaurs (rhynchocephalians), including a new species, Clevosaurus cambrica, described here from a partially articulated specimen and isolated bones. The new species has a dental morphology that is intermediate between the Late Triassic Clevosaurus hudsoni, from Cromhall Quarry to the east, and the younger C. convallis from Pant Quarry to the west, suggesting adaptive radiation of clevosaurs in the palaeo-archipelago. The larger reptiles on the palaeo-island do not exceed 1.5?m in length, including a small carnivorous crocodylomorph, Terrestrisuchus, and a possible example of insular dwarfism in the basal dinosaur Pantydraco.  相似文献   

12.
Lithostratigraphy, physicochemical stratigraphy, biostratigraphy, and geochronology of the 77–70 Ma old series bracketing the Campanian–Maastrichtian boundary have been investigated by 70 experts. For the first time, direct relationships between macro- and microfossils have been established, as well as direct and indirect relationships between chemo-physical and biostratigraphical tools. A combination of criteria for selecting the boundary level, duration estimates, uncertainties on durations and on the location of biohorizons have been considered; new chronostratigraphic units are proposed. The geological site at Tercis is accepted by the Commission on Stratigraphy as the international reference for the stratigraphy of the studied interval. To cite this article: G.S. Odin, C. R. Geoscience 334 (2002) 409–414.  相似文献   

13.
Robert L. Linnen   《Lithos》2005,80(1-4):267-280
The solubilities of columbite, tantalite, wolframite, rutile, zircon and hafnon were determined as a function of the water contents in peralkaline and subaluminous granite melts. All experiments were conducted at 1035 °C and 2 kbar and the water contents of the melts ranged from nominally dry to approximately 6 wt.% H2O. Accessory phase solubilities are not affected by the water content of the peralkaline melt. By contrast, solubilities are affected by the water content of the subaluminous melt, where the solubilities of all the accessory phases examined increase with the water content of the melt, up to 2 wt.% H2O. At higher water contents, solubilities are nearly constant. It can be concluded that water is not an important control of accessory phase solubility, although the water content will affect diffusivities of components in the melt, thus whether or not accessory phases will be present as restite material. The solubility behaviour in the subaluminous and peralkaline melts supports previous spectroscopic studies, which have observed differences in the coordination of high field strength elements in dry vs. wet subaluminous granitic glasses, but not for peralkaline granitic glasses. Lastly, the fact that wolframite solubility increases with increasing water content in the subaluminous melt suggests that tungsten dissolved as a hexavalent species.  相似文献   

14.
Some olistolites reworked in a Tertiary flysch of Mount Parnon (Peloponnesus, Greece) exhibit a Late Permian assemblage, dominated by Paradunbarula (Shindella) shindensis, Hemigordiopsis cf. luquensis and Colaniella aff. minima. This association corresponds to the Late Wuchiapingian (=Late Dzhulfian), a substage whose algae and foraminifera are generally little known. Contemporaneous limestones crop out in the middle part of the Episkopi Formation in Hydra, but they are rather commonly reworked in Mesozoic and Cainozoic sequences. The palaeobiogeographical affinities shared by the foraminiferal markers of Greece, southeastern Pamir, and southern China, are very strong (up to the specific level), and are congruent with the Pangea B reconstructions. To cite this article: E. Skourtsos et al., C. R. Geoscience 334 (2002) 925–931.  相似文献   

15.
PALEONTOLOGY     
正20141596 Liu Yunhuan(School of Earth Sciences and Resources,Chang’an University,Xi’an 710054,China);Shao Tiequan Early Cambrian Quadrapyrgites Fossils of Xixiang Boita in Southern Shaanxi Province(Journal of Earth Sciences and Environment,ISSN1672-6561,CN61-1423/P,35(3),2013,p.39-43,3 illus.,20 refs.)  相似文献   

16.
正20141719 Chen Zhijun(State Key Laboratory of Geological Processes and Mineral Resources,China University of Geosciences,Wuhan 430074,China);Chen Jianguo Automated Batch Mapping Solution for Serial Maps:A Case Study of Exploration Geochemistry Maps(Journal of Geology,ISSN1674-3636,CN32-1796/P,37(3),2013,p.456-464,2 illus.,2 tables,10 refs.)  相似文献   

17.
正20140962 Chen Fenning(Xi’an Institute of Geology and Mineral Resources,Xi’an710054,China);Chen Ruiming Late Miocene-Early Pleistocene Ostracoda Fauna of Gyirong Basin,Southern Tibet(Acta Geologica Sinica,ISSN0001-5717,CN11-1951/P,87(6),2013,p.872-886,6illus.,56refs.)  相似文献   

18.
PETROLOGY     
正1.IGNEOUS PETROLOGY20142008Cai Jinhui(Wuhan Center,China Geological Survey,Wuhan 430205,China);Liu Wei Zircon U-Pb Geochronology and Mineralization Significance of Granodiorites from Fuzichong Pb-Zn Deposit,Guangxi,South China(Geology and Mineral Resources of South China,ISSN1007-3701,CN42-1417/P,29(4),2013,p.271-281,7illus.,  相似文献   

19.
正20141205Cheng Weiming(State Key Laboratory of Resources and Environmental Information System,Institute of Geographic Sciences and Natural Resources Research,CAS,Beijing 100101,China);Xia Yao Regional Hazard Assessment of Disaster Environment for Debris Flows:Taking Jundu Mountain,Beijing as an  相似文献   

20.
正20141266Fan Chaoyan(Guangdong Provincial Key Laboratory of Mineral Resources and Geological Processes,Guangzhou 510275,China);Wang Zhenghai On Error Analysis and Correction Method of Measured Strata Section with Wire Projection Method(Journal of  相似文献   

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