Titlebook: Geodynamics of Lithosphere & Earth’s Mantle; Seismic Anisotropy a Jaroslava Plomerová,Robert C. Liebermann,Vladislav Conference proceedings

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書目名稱Geodynamics of Lithosphere & Earth’s Mantle影響因子(影響力)




書目名稱Geodynamics of Lithosphere & Earth’s Mantle影響因子(影響力)學(xué)科排名




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書目名稱Geodynamics of Lithosphere & Earth’s Mantle網(wǎng)絡(luò)公開度學(xué)科排名




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書目名稱Geodynamics of Lithosphere & Earth’s Mantle讀者反饋




書目名稱Geodynamics of Lithosphere & Earth’s Mantle讀者反饋學(xué)科排名

GRAZE

,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

多產(chǎn)子

Cpr951

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

有惡意

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

熔巖

熔巖

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.

intrude

贊美者

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

安慰

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