• No results found

[PDF] Top 20 Determination of the Crust and Upper Mantle Structure in Anatolia by Surface Wave Data

Has 10000 "Determination of the Crust and Upper Mantle Structure in Anatolia by Surface Wave Data" found on our website. Below are the top 20 most common "Determination of the Crust and Upper Mantle Structure in Anatolia by Surface Wave Data".

Determination of the Crust and  Upper Mantle Structure in Anatolia by  Surface Wave Data

Determination of the Crust and Upper Mantle Structure in Anatolia by Surface Wave Data

... Discussion and Conclusions In this study, for an earthquake EZM occurred in eastern Anatolia, crust and upper mantle structure of Anatolia have been investigated by the inversion of disc[r] ... See full document

11

Surface-wave imaging of the weakly-extended Malawi Rift from ambient-noise and teleseismic Rayleigh waves from onshore and lake-bottom seismometers

Surface-wave imaging of the weakly-extended Malawi Rift from ambient-noise and teleseismic Rayleigh waves from onshore and lake-bottom seismometers

... the crust and uppermost mantle could be explained by local- ized fracturing and deformation associated with extension (Carlson & Gangi 1985) or elevated ...velocity upper-mantle ... See full document

14

Using Earth Deformation Caused by Surface Mass Loading to Constrain the Elastic Structure of the Crust and Mantle

Using Earth Deformation Caused by Surface Mass Loading to Constrain the Elastic Structure of the Crust and Mantle

... solid mantle and disregard the core ...the upper mantle and crust, thereby justifying our neglect of perturbations to core structure ...of surface-wave phase velocities in ... See full document

400

Heterogeneous crust and upper mantle across southern Kenya and the relationship to surface deformation as inferred from magnetoteluric imaging

Heterogeneous crust and upper mantle across southern Kenya and the relationship to surface deformation as inferred from magnetoteluric imaging

... uppermost mantle. Using wide-angle seismic reflection data and assuming the roughly layered crustal structure derived by Birt et ...discontinuous upper mantle reflectors (mimicked by ... See full document

19

Topography of the Moho Undulation in Cameroon from Gravity Data: Preliminary Insights into the Origin, the Age and the Structure of the Crust and the Upper Mantle across Cameroon and Adjacent Areas

Topography of the Moho Undulation in Cameroon from Gravity Data: Preliminary Insights into the Origin, the Age and the Structure of the Crust and the Upper Mantle across Cameroon and Adjacent Areas

... anomaly data from Cameroon and part of the neighboring countries has been examined to compute the topography of the Moho ...the crust and the upper mantle. Comparison with seismic data ... See full document

21

Adjoint tomography of the crust and upper mantle structure beneath the Kanto region using broadband seismograms

Adjoint tomography of the crust and upper mantle structure beneath the Kanto region using broadband seismograms

... After the disastrous 1995 Hyogoken-nanbu (Kobe) earthquake, numerous seismographs were installed in Japan by the National Research Institute for Earth Sci- ence and Disaster Prevention (NIED; renamed the Na- tional ... See full document

20

Three dimensional shear wave velocity structure in the upper mantle beneath the Philippine Sea region

Three dimensional shear wave velocity structure in the upper mantle beneath the Philippine Sea region

... dispersion data of surface waves travelling through the central portion of the Philippine Sea were used to construct a one-dimensional (1-D) upper mantle shear wave model, ...the ... See full document

14

Tomographic image of crust and upper mantle off the Boso Peninsula using data from an ocean bottom seismograph array

Tomographic image of crust and upper mantle off the Boso Peninsula using data from an ocean bottom seismograph array

... three-dimensional structure of the crust and upper mantle off the Boso Peninsula, Japan, by analyzing seismograms recorded by ocean-bottom seismometers and land stations between 2011 and ... See full document

10

Traces of the crustal units and the upper-mantle structure in the southwestern part of the East European Craton

Traces of the crustal units and the upper-mantle structure in the southwestern part of the East European Craton

... The data set of 4195 manually picked arrivals of teleseismic P waves of 101 earthquakes (EQs) recorded in the seismic stations deployed to the east of the TESZ was inverted using the non-linear teleseismic ... See full document

16

Crustal heat production and estimate of terrestrial heat flow in central East Antarctica, with implications for thermal input to the East Antarctic ice sheet

Crustal heat production and estimate of terrestrial heat flow in central East Antarctica, with implications for thermal input to the East Antarctic ice sheet

... modeled surface heat flow by first correlating seismic velocity data from the crust and upper mantle in regions of known heat flow, and then extrapo- lating these results to a seismic ... See full document

14

Variations in the thickness of the crust of the Kaapvaal craton, and mantle structure below southern Africa

Variations in the thickness of the crust of the Kaapvaal craton, and mantle structure below southern Africa

... has upper mantle wavespeeds less than GNEM and SATZ to depths of about 220 and 270 km respectively, but higher than IASP91 to depths of 270 ...of data analysis (Simon et ...Kaapvaal data for P ... See full document

13

Upper mantle structure from long-period SH

Upper mantle structure from long-period SH

... mode surface waves, Crampin and King (1977) suggested 7% velocity anisotropy for P waves in central ...an upper limit on the depth to which the anisotropy exists, but suggest that as little as 10 km of ... See full document

271

Surface wave studies of the Australian upper mantle

Surface wave studies of the Australian upper mantle

... calculate surface wave dispersion from seismograms recorded at two stations were described in the preceding ...the crust-upper mantle structure throughout ... See full document

185

Crust and upper mantle resistivity structure in the southwestern end of the Kuril Arc as revealed by the joint analysis of conventional MT and network MT data

Crust and upper mantle resistivity structure in the southwestern end of the Kuril Arc as revealed by the joint analysis of conventional MT and network MT data

... The upper surface of the relatively high resistive layer (700–1,000 m) tends to be deeper towards the north (deep- ening from 55 to 100 km within the study ...the surface to 20 km in depth near site ... See full document

14

Seismic visibility of a deep subduction channel – insights from numerical simulation of high-frequency seismic waves emitted from intermediate depth earthquakes

Seismic visibility of a deep subduction channel – insights from numerical simulation of high-frequency seismic waves emitted from intermediate depth earthquakes

... We follow an approach by Stixrude and Lithgow-Bertelloni (2005) (SLB2005). They use an expression of the mineral’s free energy consisting of two parts: a “cold” part which con- tains an expansion of free energy to fourth ... See full document

19

Moder, Christoph
  

(2011):


	From Faults to Plate Boundaries: Insights from Computer Models.


Dissertation, LMU München: Fakultät für Geowissenschaften

Moder, Christoph (2011): From Faults to Plate Boundaries: Insights from Computer Models. Dissertation, LMU München: Fakultät für Geowissenschaften

... flow data: complex fault junctions and closely-spaced faults need a higher density of nodes, because they cannot otherwise be separated and represented in the ... See full document

146

The effect of pressure on the elastic properties and seismic anisotropy of diopside and jadeite from atomic scale simulation

The effect of pressure on the elastic properties and seismic anisotropy of diopside and jadeite from atomic scale simulation

... equilibrium structure and de- rived properties, of materials by finding an approximate solution to the many body time-independent Schr¨ odinger equation for a collection of electrons in the potential field of ... See full document

21

Regional Variations in Upper Mantle Structure Beneath North America

Regional Variations in Upper Mantle Structure Beneath North America

... in a comprehensive study of variations in upper mantle structure beneath North America, theoretical behavior of body wave travel times, apparent velocities, and amplitudes have been calc[r] ... See full document

216

Studying local earthquakes in the area Baltic-Bothnia Megashear using the data of the POLENET/LAPNET temporary array

Studying local earthquakes in the area Baltic-Bothnia Megashear using the data of the POLENET/LAPNET temporary array

... P wave velocity model of the uppermost crust (down to 20 km) for a se- lected region inside the study area and show that the ve- locity heterogeneities in the upper crust correlate well with ... See full document

14

Earthquake cycle deformation and the Moho: Implications for the rheology of continental lithosphere

Earthquake cycle deformation and the Moho: Implications for the rheology of continental lithosphere

... Figure 5: Histograms of earthquake rupture bottom depths (black bars) determined from InSAR-constrained coseismic slip models based upon the data in Tables 1–3, grouped by four continental regions shown in Figure ... See full document

86

Show all 10000 documents...