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1.
The generation and propagation of surface waves resulting from suddenly created disturbances over water surfaces is investigated. The initial boundary conditions defining the disturbance are given either by a velocity of the free surface, an initial elevation of the free surface or a pressure impulsively applied on the free surface. It is shown that the corresponding three forms of solutions are related by a simple time derivative. Linear solutions are obtained in the cases where the wave motion is assumed to be nondispersive, mildly dispersive and fully dispersive, as well as in the case where the motion is given by the method of stationary phase. Criteria are established to indicate the limit of validity of each method. 相似文献
2.
The application of neural networks as classifiers of seismic events is described with the aim of developing an automatic system for the classification of explosion quakes at the Stromboli volcano. The architecture of the network that we trained to identify four different classes of shocks was a Multi-Layer Perceptron, using the Back Error Propagation algorithm. Five different approaches for representing the information embedded in the seismograms, both in the time and in the frequency domain, were considered, and the results compared. The direct use of the time series of the shocks was not satisfactory. The auto-correlation function worked well, but in some cases it was misleading. A better performance was obtained with a frequency domain representation. Finally, the use of the envelope function did not work well. Combining parameters such as the auto-correlation and envelope functions can improve one source of error, but it may introduce new ones. The performance obtained highlights the importance of the data attributes used for the training of the network. Topologies with eight neurons in a single hidden layer gave, on average, the best results among the considered neural network structures. The overall results provide a large number of events (89% with the best performance) correctly classified, indicating that this automatic technique is reliable, and encouraging further applications in the field of volcanic seismology. 相似文献
3.
湖南及邻区地壳旋转的可能成因、对大地构造演化的影响及其与大规模成矿作用关系初探 总被引:4,自引:0,他引:4
在湖南及邻区,无论从地表的地质构造还是地球物理场上,都表现出明显的环状分布特征。这种特征可能是地壳的旋转运动所造成,它对湖南及邻区大地构造的演化、大规模成矿作用等具有重大的影响。本文对这种旋转运动的可能成因,以及所伴随的一系列地质作用、与大规模成矿作用的关系等进行了初步探讨。 相似文献
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5.
Shear wave statics using receiver functions 总被引:1,自引:0,他引:1
6.
本文综述了我国第 1 5次 ( 1 998/ 1 999)、1 6次 ( 1 999/ 2 0 0 0 )南极科学考察队在东南极格罗夫山冰区回收的 32块陨石的岩石矿物学特征及其分类。这些陨石包括 :2 3块平衡型普通球粒陨石、6块非平衡型普通球粒陨石、1块二辉橄榄岩质火星陨石、1块钙长辉长无球粒陨石、1块未分群的铁陨石。文中还对南极格罗山冰区的陨石富集机制、GRV 980 0 4 (H5 )球粒陨石异常低的宇宙射线暴露年龄、火星陨石的溅射年龄等进行了初步的讨论 ,并对今后格罗夫山陨石的研究提出一些初步想法。 相似文献
7.
内蒙古虎拉林爆破角砾岩型金矿床特征 总被引:5,自引:0,他引:5
虎拉林金矿区主要地层为中侏罗统绣峰组陆源碎屑岩,岩浆岩以燕山期花岗斑岩和石英斑岩为主。在地层与岩体接触带附近发育爆破角砾岩,金矿(化)体主要受断裂控制而产于爆破角砾岩筒(带)中。矿区内已圈出6条矿(化)体,总体走向近SN,以1、2号为主要矿体。成矿与爆破角砾岩有关,形成一体多型的矿化分布形式。δ^34S变化范围为-0.2‰-0.8‰,具有深源岩浆S特征。S和Pb同位素、流体包裹体、稀土元素等特征表明,成矿物质来自地壳深部或地幔,成矿流体以深部岩浆热液为主。^39Al/^40Ari法测得金矿成矿年龄为135.5Ma。 相似文献
8.
2002年上半年,伴随着厄尔尼诺现象的日益加剧,全球性重大自然灾害频繁发生.6月20日发生在中国黑龙江省鸡西煤矿的瓦斯爆炸事件和6月22日发生在伊朗的强烈地震,时间恰逢月亮近地潮的6月19日和太阳潮半日形变最大值的夏至的6月21日附近,是地球形变和排气较强烈的时段.据国内外有关资料,月球与地球发震有关系的重要条件是“近地点兼朔、望”以及各大行星特定位置的配合,张元东称之为“特殊天象组合期”[1];郭增建等提出,月亮赤纬角或太阳黄赤交角最大时地球形变和排气最强烈[2~5].在此期间,中国各种大的突发性灾难,如空难、海难、火车事故、矿… 相似文献
9.
L. A. Morgan W. C. Shanks III D. A. Lovalvo S. Y. Johnson W. J. Stephenson K. L. Pierce S. S. Harlan C. A. Finn G. Lee M. Webring B. Schulze J. Dühn R. Sweeney L. Balistrieri 《Journal of Volcanology and Geothermal Research》2003,122(3-4):221-242
‘No portion of the American continent is perhaps so rich in wonders as the Yellow Stone’ (F.V. Hayden, September 2, 1874)Discoveries from multi-beam sonar mapping and seismic reflection surveys of the northern, central, and West Thumb basins of Yellowstone Lake provide new insight into the extent of post-collapse volcanism and active hydrothermal processes occurring in a large lake environment above a large magma chamber. Yellowstone Lake has an irregular bottom covered with dozens of features directly related to hydrothermal, tectonic, volcanic, and sedimentary processes. Detailed bathymetric, seismic reflection, and magnetic evidence reveals that rhyolitic lava flows underlie much of Yellowstone Lake and exert fundamental control on lake bathymetry and localization of hydrothermal activity. Many previously unknown features have been identified and include over 250 hydrothermal vents, several very large (>500 m diameter) hydrothermal explosion craters, many small hydrothermal vent craters (1–200 m diameter), domed lacustrine sediments related to hydrothermal activity, elongate fissures cutting post-glacial sediments, siliceous hydrothermal spire structures, sublacustrine landslide deposits, submerged former shorelines, and a recently active graben. Sampling and observations with a submersible remotely operated vehicle confirm and extend our understanding of the identified features. Faults, fissures, hydrothermally inflated domal structures, hydrothermal explosion craters, and sublacustrine landslides constitute potentially significant geologic hazards. Toxic elements derived from hydrothermal processes also may significantly affect the Yellowstone ecosystem. 相似文献
10.
Recent seismological studies have presented evidence for the existence of a layer with ultra-low seismic velocities at the core-mantle boundary at ca. 2900 km depth. We report high-amplitude, high-frequency, and laterally coherent seismic arrivals from three nuclear explosions in Siberia. With recording station intervals of 15 km, the seismic phases are readily correlated and show the presence of a thin, ultra-low velocity zone in a region where it was not previously reported. The duration and complexity of the arrivals are inconsistent with a simple core-mantle boundary and require a hitherto unidentified, kilometre-scale, fine structure in the ultra-low velocity zone. The observations may be explained by a ca. 7 km thick, two-layer, ultra-low velocity zone with exceptional low velocities, which indicate the presence of high percentages of melt (>15%), in particular in the lower part of the zone. Waveform variation implies lateral change in the thickness and physical properties of the ultra-low velocity zone with a wavelength of less than 100 km. 相似文献