標(biāo)題: Titlebook: Geodynamics of Lithosphere & Earth’s Mantle; Seismic Anisotropy a Jaroslava Plomerová,Robert C. Liebermann,Vladislav Conference proceedings [打印本頁(yè)] 作者: Daguerreotype 時(shí)間: 2025-3-21 16:07
書(shū)目名稱Geodynamics of Lithosphere & Earth’s Mantle影響因子(影響力)
書(shū)目名稱Geodynamics of Lithosphere & Earth’s Mantle影響因子(影響力)學(xué)科排名
書(shū)目名稱Geodynamics of Lithosphere & Earth’s Mantle網(wǎng)絡(luò)公開(kāi)度
書(shū)目名稱Geodynamics of Lithosphere & Earth’s Mantle網(wǎng)絡(luò)公開(kāi)度學(xué)科排名
書(shū)目名稱Geodynamics of Lithosphere & Earth’s Mantle被引頻次
書(shū)目名稱Geodynamics of Lithosphere & Earth’s Mantle被引頻次學(xué)科排名
書(shū)目名稱Geodynamics of Lithosphere & Earth’s Mantle年度引用
書(shū)目名稱Geodynamics of Lithosphere & Earth’s Mantle年度引用學(xué)科排名
書(shū)目名稱Geodynamics of Lithosphere & Earth’s Mantle讀者反饋
書(shū)目名稱Geodynamics of Lithosphere & Earth’s Mantle讀者反饋學(xué)科排名
作者: GRAZE 時(shí)間: 2025-3-21 23:18
,Die Geburtshilfe und Gyn?kologie,nly in boundary layers of convective mantle..We review in this paper, the seismic data sets which provide insight into the location at depth of large-scale anisotropy from the .-layer up to the lithosphere. In addition to the well-documented seismic anisotropy in the lithosphere and asthenosphere, t作者: 多產(chǎn)子 時(shí)間: 2025-3-22 03:33 作者: Cpr951 時(shí)間: 2025-3-22 04:58
https://doi.org/10.1007/978-3-662-06665-2ude of the delay time of the upper layer, the lower layer must lie within the asthenosphere. At other stations splitting parameters are consistent with an anisotropic one-layer model for the upper mantle. Stations near the Bohemian Massif show fast directions near EW. Throughout NE Germany the direc作者: 有惡意 時(shí)間: 2025-3-22 11:29
Meerwassertrinkkur und Mineralstoffwechsel,for adjacent stations, our results show a large scatter of the individual splitting parameters for the set of events used. The magnitude of the splitting time suggests that the deformation extends below the lithosphere and that the thickness of the anisotropic structure is at least 100–200 km..For s作者: 熔巖 時(shí)間: 2025-3-22 13:42 作者: 熔巖 時(shí)間: 2025-3-22 18:45
https://doi.org/10.1007/978-3-663-02187-2t polarization direction we determine is quite parallel to the opening of the Ross Sea, an active rift system, but also to the Absolute Plate Motion direction. Therefore, we assume that the identified anisotropy may be induced by the extension, activated by plate motion and is still related to it.作者: intrude 時(shí)間: 2025-3-23 00:04 作者: 贊美者 時(shí)間: 2025-3-23 01:41
https://doi.org/10.1007/978-3-642-94325-6iding plate extension. However, fast directions beneath the Japan Sea, western Honshu, and Sakhalin Island are highly oblique to subducting plate motion and parallel to present or past overriding plate shearing. Models of back-arc mantle flow that are driven by viscous coupling to local plate motion作者: 安慰 時(shí)間: 2025-3-23 08:44
Das ?Bild der Bilder?: Dürers , (1514)f the depth and geometry of the Moho through the receiver function technique is in progress. Tomographic results from the northernmost 1994 and the central 1995 teleseismic experiments confirm that a high-velocity anomaly (HVA) does exist in the upper 200–250 km and is confined to the northern Apenn作者: 細(xì)胞學(xué) 時(shí)間: 2025-3-23 12:11 作者: ironic 時(shí)間: 2025-3-23 15:07 作者: 殖民地 時(shí)間: 2025-3-23 18:38
Die animalischen Nahrungs- und Genussmittel,t was carried out for the region investigated. The characteristics of the “crust-mantle” transition have been investigated. Large blocks with different types of the earth’s crust were distinguished. Layers with inverse values of velocity, density and shear and Young modulus are revealed in the Tien-作者: Substitution 時(shí)間: 2025-3-24 00:07 作者: Lyme-disease 時(shí)間: 2025-3-24 04:37 作者: 閃光東本 時(shí)間: 2025-3-24 06:55
On Presence of Seismic Anisotropy in the Asthenosphere beneath Continents and its Dependence on Platf asthenospheric anisotropy in addition to frozen anisotropy in the lithosphere. A critical plate velocity for the formation of anisotropy can be caused by the dislocation-diffusion transition as a function of strain rate on a deformation mechanism map of the upper mantle olivine.作者: BIBLE 時(shí)間: 2025-3-24 11:02
Backazimuthal Variations of Splitting Parameters of Teleseismic SKS Phases Observed at the Broadbandude of the delay time of the upper layer, the lower layer must lie within the asthenosphere. At other stations splitting parameters are consistent with an anisotropic one-layer model for the upper mantle. Stations near the Bohemian Massif show fast directions near EW. Throughout NE Germany the direc作者: Left-Atrium 時(shí)間: 2025-3-24 15:02 作者: VERT 時(shí)間: 2025-3-24 22:27
Anisotropy beneath the Iberian Peninsula: The Contribution of the ILIHA-NARS Broad-band Experimenthanisms, such as the absolute plate motion of Eurasia, can be invoked to explain the origin of anisotropic features in many sites, the regional variations observed in some domains imply that differentiated origins of the anisotropy have to be considered, probably related to the particular tectonics 作者: fringe 時(shí)間: 2025-3-25 00:51
Upper Mantle Anisotropy in Victoria Land (Antarctica)t polarization direction we determine is quite parallel to the opening of the Ross Sea, an active rift system, but also to the Absolute Plate Motion direction. Therefore, we assume that the identified anisotropy may be induced by the extension, activated by plate motion and is still related to it.作者: 他日關(guān)稅重重 時(shí)間: 2025-3-25 03:25 作者: BUOY 時(shí)間: 2025-3-25 10:52 作者: 大量 時(shí)間: 2025-3-25 11:43
Passive Seismology and Deep Structure in Central Italyf the depth and geometry of the Moho through the receiver function technique is in progress. Tomographic results from the northernmost 1994 and the central 1995 teleseismic experiments confirm that a high-velocity anomaly (HVA) does exist in the upper 200–250 km and is confined to the northern Apenn作者: AMOR 時(shí)間: 2025-3-25 16:29
New Perspectives on Mantle Dynamics from High-resolution Seismic Tomographic Model P1200r degrees exceeding around 10, the spectra at various depths decay with a power-law like dependence on the degree, with the logarithmic slopes in the asymptotic portion of the spectra containing values between 2 and 2.6. These spectral results may suggest the time-dependent nature of mantle convecti作者: hypnogram 時(shí)間: 2025-3-25 22:09
Regional Correlation Analysis between Seismic Heterogeneity in the Lower Mantle and Subduction in thion and in the mid-mantle for subduction younger than 120 Myr. An increase in the correlation close to the core-mantle boundary nevertheless indicates that, under certain circumstances, the slabs can reach the bottom of the mantle in the West Pacific and in the Alpine-Himalayan regions as well. The 作者: Brocas-Area 時(shí)間: 2025-3-26 03:38 作者: abject 時(shí)間: 2025-3-26 05:08
https://doi.org/10.1007/978-3-662-28967-9rface and those extending deep into the interior of the Earth. Seismic anisotropy provides some of the most diagnostic evidence for mapping past and present deformation of the entire crust-mantle system.作者: 危險(xiǎn) 時(shí)間: 2025-3-26 10:26 作者: GLARE 時(shí)間: 2025-3-26 14:20 作者: 一美元 時(shí)間: 2025-3-26 17:08 作者: myopia 時(shí)間: 2025-3-26 21:41
https://doi.org/10.1007/978-3-662-60956-9e age of continental provinces, and typical depth dependences of ξ. are determined. The relative radial anisotropy ξ. in the mantle lithosphere of Phanerozoic orogenic belts is characterized by .. > .., with its maximum depth of about 70 km, on the average, while beneath old shields and platforms, i作者: 朋黨派系 時(shí)間: 2025-3-27 02:06
,Situationen und Entwicklungen 1945–1947,anisotropy correlate weakly with the directions of the absolute plate motion (APM) for all APM models. Weak correlation indicates the possibility of asthenospheric anisotropy as well as frozen anisotropy in the lithosphere. Detection of strain rate dependence of anisotropy is helpful to further conc作者: radiograph 時(shí)間: 2025-3-27 08:57
https://doi.org/10.1007/978-3-662-06665-2ing from 13 stations of the German Regional Seismic Network (GRSN), from 3 three-component stations of the Gr?fenberg array (GRF) and from one Austrian station (SQTA). The data reveal strong differences in the splitting parameters (fast direction ? and delay time δ.) from a single event at various s作者: 開(kāi)花期女 時(shí)間: 2025-3-27 13:26
Meerwassertrinkkur und Mineralstoffwechsel, semi-permanent long- and short-period and temporary short-period seismological stations located in two geodynamically important areas in western Europe, namely the Rhinegraben-Urach area and the French Massif Central volcanic field..While for the semi-permanent and the permanent stations there is a作者: 單純 時(shí)間: 2025-3-27 14:48
Rationalisierung durch Vereinheitlichungact zone of the Saxothuringicum and Moldanubicum in the western margin of the Bohemian Massif in central Europe. Spatial variations of .-wave velocities and lateral variations of the particle motion of split shear waves over the region monitor changes of structure and anisotropy within the deep lith作者: 臭了生氣 時(shí)間: 2025-3-27 21:09
Die Mehrwertsteuer in Buchhaltung und Bilanzr-wave splitting observed in the ILIHA-NARS experiment. In this experiment, an homogeneous data set is provided by a network of 14 broad-band stations deployed over the entire peninsula for about one year. Even if technical problems led to an amount of data smaller than expected, significant variati作者: nitric-oxide 時(shí)間: 2025-3-27 23:34
Notwendige Planungs- und Umstellungsarbeiten increase northward of the splitting delay, as well as of its first arrival residual. Both waves split by velocity anisotropy are slow relative to . and their waveform analysis may be interpreted to suggest attenuation anisotropy. The array here provides examples of residuals and splitting of other 作者: cravat 時(shí)間: 2025-3-28 03:38 作者: Amenable 時(shí)間: 2025-3-28 08:20 作者: 焦慮 時(shí)間: 2025-3-28 12:32
https://doi.org/10.1007/978-3-642-94325-6ction zones using shear-wave splitting in . phases from local earthquakes and in teleseismic core phases such as .. The observed splitting in all four subduction zones is consistent with a model in which the lower transition zone (520–660 km) and lower mantle are isotropic, and in which significant 作者: geriatrician 時(shí)間: 2025-3-28 14:56
Das ?Bild der Bilder?: Dürers , (1514)ain a clearer picture of the lithosphere-asthenosphere structure in peninsular Italy, between 1994 and 1996, we have deployed three teleseismic transects in northern, central, and southern Apennines, in the framework of the project . (European Community contract EV5V-CT94–0464). Some hundreds of tel作者: Tinea-Capitis 時(shí)間: 2025-3-28 20:32 作者: SHRIK 時(shí)間: 2025-3-29 00:06
Soziale Arbeit in der Tiermedizin, of the mantle. This model was used in diverse ways to study mantle viscosity structure and geodynamical processes. In the spatial domain there are lateral variations in the transition zone, suggesting interaction between the lower-mantle plumes and the region from 600 km to 1000 km. Some examples s作者: CARE 時(shí)間: 2025-3-29 05:13 作者: 慷慨援助 時(shí)間: 2025-3-29 08:17
Die animalischen Nahrungs- und Genussmittel,lithosphere heterogeneities (composition, rheological) create the prerequisites for the development of various phenomena of tectonic layering (lateral shearing, different deformation of layers). To study the distribution of velocity, density and other elastic parameters, the results from a seismic t作者: hieroglyphic 時(shí)間: 2025-3-29 14:19
https://doi.org/10.1007/978-3-0348-8777-9Deformation; Seismic Anisotropy; evolution; geodynamics; geology; geophysics; lithosphere; mineral; modellin作者: Dungeon 時(shí)間: 2025-3-29 16:49
978-3-0348-9770-9Springer Basel AG 1998作者: 數(shù)量 時(shí)間: 2025-3-29 21:54
Geodynamics of Lithosphere & Earth’s Mantle978-3-0348-8777-9Series ISSN 2504-3625 Series E-ISSN 2504-3633 作者: DIS 時(shí)間: 2025-3-30 01:55
Geodynamics of Lithosphere and Earth’s Mantle: Seismic Anisotropy as a Record of the Past and Presenrface and those extending deep into the interior of the Earth. Seismic anisotropy provides some of the most diagnostic evidence for mapping past and present deformation of the entire crust-mantle system.作者: Bumptious 時(shí)間: 2025-3-30 07:41 作者: 不再流行 時(shí)間: 2025-3-30 08:44
Age-dependent Large-scale Fabric of the Mantle Lithosphere as Derived from Surface-wave Velocity Anie age of continental provinces, and typical depth dependences of ξ. are determined. The relative radial anisotropy ξ. in the mantle lithosphere of Phanerozoic orogenic belts is characterized by .. > .., with its maximum depth of about 70 km, on the average, while beneath old shields and platforms, i作者: 男學(xué)院 時(shí)間: 2025-3-30 14:13
On Presence of Seismic Anisotropy in the Asthenosphere beneath Continents and its Dependence on Platanisotropy correlate weakly with the directions of the absolute plate motion (APM) for all APM models. Weak correlation indicates the possibility of asthenospheric anisotropy as well as frozen anisotropy in the lithosphere. Detection of strain rate dependence of anisotropy is helpful to further conc作者: defibrillator 時(shí)間: 2025-3-30 17:42
Backazimuthal Variations of Splitting Parameters of Teleseismic SKS Phases Observed at the Broadbanding from 13 stations of the German Regional Seismic Network (GRSN), from 3 three-component stations of the Gr?fenberg array (GRF) and from one Austrian station (SQTA). The data reveal strong differences in the splitting parameters (fast direction ? and delay time δ.) from a single event at various s作者: arrhythmic 時(shí)間: 2025-3-30 23:53 作者: 銀版照相 時(shí)間: 2025-3-31 01:04 作者: aptitude 時(shí)間: 2025-3-31 09:05 作者: antecedence 時(shí)間: 2025-3-31 12:23
Variation of Shear-wave Residuals and Splitting Parameters from Array Observations in Southern Tibet increase northward of the splitting delay, as well as of its first arrival residual. Both waves split by velocity anisotropy are slow relative to . and their waveform analysis may be interpreted to suggest attenuation anisotropy. The array here provides examples of residuals and splitting of other 作者: pacific 時(shí)間: 2025-3-31 15:10
Upper Mantle Anisotropy in Victoria Land (Antarctica)d around the Mt. Melbourne volcano, near Terra Nova Bay, and the second southward, along the ACRUP1 Geotraverse. The aim of these experiments was to provide additional constraints on the Moho geometry and on lithosphere-asthenosphere structure in this zone. For this reason, a number of techniques we作者: Urologist 時(shí)間: 2025-3-31 19:39
Anisotropy of the Yellowstone Hot Spot Wake, Eastern Snake River Plain, Idaho Plain crust and creating a wider, wake-like “tectonic parabola” of seismicity and uplift. Analysis of SKS arrivals to a line array of 55 mostly broadband stations, distribution across the tectonic parabola, reveals a nearly uniform orientation of anisotropy, with an average fast axis orientation of作者: Adulterate 時(shí)間: 2025-3-31 23:38 作者: 場(chǎng)所 時(shí)間: 2025-4-1 05:39
Passive Seismology and Deep Structure in Central Italyain a clearer picture of the lithosphere-asthenosphere structure in peninsular Italy, between 1994 and 1996, we have deployed three teleseismic transects in northern, central, and southern Apennines, in the framework of the project . (European Community contract EV5V-CT94–0464). Some hundreds of tel作者: 緩解 時(shí)間: 2025-4-1 08:40
