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481.
We present a detailed study of Western Bohemia Love waves generated by blasts with an intention to estimate the uppermost
crust structure for a more detailed layer distribution than previous studies have used. The use of short-period (4 s and shorter)
Love waves represents a new approach in the studied region. Properties of multiple filtering as a tool of frequency–time analysis
are discussed. A new method of selecting the dispersion ridges is introduced. Tests of filtering are provided by analyzing
signals with analytically known dispersion. The isometric algorithm for the inversion problem is applied, the problem of non-uniqueness
is discussed, and tests of reliability of the inversion are presented. During the inversion, the forward problem is solved
by use of the matrix method. Six records of blasts from the Western Bohemia region are analyzed to separate the fundamental
modes of Love wavegroups, and shear wave velocity distributions down to a depth of 3.0 km are inferred. Modal summation is
used to compute synthetic velocigrams, which are compared to measured ones. The lateral heterogeneity of the region is discussed
and the presented models are compared to those of previous studies and to the geological setting of the region. 相似文献
482.
Carlos Roberto de Souza Filho Alfredo Rossetto Nunes Emilson Pereira Leite Lena Virgínia Soares Monteiro Roberto Perez Xavier 《Surveys in Geophysics》2007,28(5-6):377-405
The Serra Leste region, located in the northeast portion of Carajás Mineral Province (PA), hosts important chrome-PGE, Au–Pd–Pt,
Cu–Mo–Au, iron, and manganese deposits and occurrences related to different geological settings. We present a regional prospective
model with focus on PGE mineralizations based on airborne geophysics (magnetometry, gamma-ray spectrometry and time domain
electromagnetometry) and geological data. Geological and geophysics data analysis indicate a plausible correspondence between
areas with meta-mafic–ultramafic rocks and low values in gamma spectrometry, mainly for the thorium channel. The meta-ultramafic
units of the complexes, the main host rock of the PGE mineralization, are well defined by analytic signal from the anomalous
magnetic field and by the apparent conductance anomalies derived from the GEOTEM system. The combination of the derivative
products with updated geological data of the Serra Leste region and PGE-Luanga deposit enable to establish a regional prospective
model for PGE and the identification of new targets within the studied area. 相似文献
483.
A set of two hundred shear-wave velocity models of the crust and uppermost mantle in southeast Europe is determined by application
of a sequence of methods for surface-waves analysis. Group velocities for about 350 paths have been obtained after analysis
of more than 600 broadband waveform records. Two-dimensional surface-wave tomography is applied to the group-velocity measurements
at selected periods and after regionalisation, two sets of local dispersion curves (for Rayleigh and Love waves) are constructed
in the period range 8–40 s. The shear-wave velocity models are derived by applying non-linear iterative inversion of local
dispersion curves for grid cells predetermined by the resolving power of data. The period range of observations limits the
velocity models to depths of 70 km in accordance to the penetration of the surface waves with a maximum period of 40 s. Maps
of the Moho boundary depth, velocity distribution above and below Moho boundary, as well as velocity distribution at different
depths are constructed. Well-known geomorphologic units (e.g. the Pannonian basin, southeastern Carpathians, Dinarides, Hellenides,
Rodophean massif, Aegean Sea, western Turkey) are delineated in the obtained models. Specific patterns in the velocity models
characterise the southeast Carpathians and adjacent areas, coast of Albania, Adriatic coast of southern Italy and the southern
coast of the Black Sea. The models obtained in this study for the western Black Sea basin shows the presence of layers with
shear-wave velocities of 3.5 km/s–3.7 km/s in the crust and thus do not support the hypothesis of existence of oceanic structure
in this region. 相似文献
484.
On the basis of photographs from the 6 m Large Azimuthal Telescope and the Hubble Space Telescope, VRI photometry of stars in 11 galaxies in the NGC 1023 group has been carried out. The distances to these galaxies were determined by the method of brightest stars. The distances to NGC 925 and NGC 1023 were determined from the position of the top of the red giant branch (the TRGB method). From the calculated average and root-mean-square distances to the NGC 1023 group (10.3 ± 2.2 Mpc and 9.7 ± 0.5 Mpc) the Hubble constant in this direction was determined: H
0R
= 75 ± 8 km·sec-1·Mpc-1 and H
0M
= 81 ± 5 km ·sec-1·Mpc-1. 相似文献
485.
486.
几种弱向异性介质中qSV波速度和偏振异常 总被引:2,自引:2,他引:0
研究了在具有生趣对称轴的横向各向同性介质(TIV介质)中qSV波群速度及偏振矢量,给出了相应的精确和近似公式,进一步讨论了用较简单的近似公式来代替复杂精确公式的可靠性;最后展示了地球内部几种常见各向异性岩石矿物中地震sSV波速度各向异性因子、偏振信息及其与传播方向之间的偏差。 相似文献
487.
新疆东天山地区蓟县系原卡瓦布拉克群为一套岩性复杂、变质程度差异很大的变质岩系,通过大黑山幅1:25万区调的调查研究将其进行了解体,根据岩石组合,变质程度及所含叠层石的组合重新厘定了层序,它包括了未分太古界、下元古界兴地塔格岩群(Pt1x)、长城系杨吉布拉克岩群(Chy)、蓟县系爱尔基干岩群(Jxa)和青白口系帕尔岗塔格岩群(Qmp),同时对各岩群的岩石组合、变质、变形进行了区域性的对比研究。 相似文献
488.
预防底板突水的目的含水层水文地质试验研究——鲁中煤田下组煤水文地质补充勘探方法 总被引:4,自引:0,他引:4
针对淄博、济东、肥城等华北型石炭二叠系煤田大水矿区原有煤田水文地质勘探阶段资料程度难以满足下组煤带压开采防治水的情况下,选择了预防底板突水中间指示含水层--处于下组煤层与奥灰之间的徐家庄灰岩进行了的采掘前矿井水文地质勘探.充分利用井下巷道,以井下放水试验(包括示踪试验)为主,井上、下结合同步观测,分块(分片、分区)、分层、分阶段及局部、联合放水试验分步骤逐渐暴露水文地质条件,肥城和济东等矿区的实际勘探效果证明针对中间指示含水层进行综合水文地质勘探可达到事半功倍的效果. 相似文献
489.
通过对沙沟街地区商丹构造带北部原划秦岭群进行 1∶ 5万区调填图 ,从前人划分的副变质片麻岩中解体出一套变质中酸性古侵入体 - TTG岩系。划分和圈定出 5个片麻岩体 ,归并为 2个片麻杂岩 ,建立了老安子沟片麻岩套 ,并从岩石、地球化学等方面综合进行了探讨。 相似文献
490.