• No results found

receiver function

Crustal Thickness of Funafuti Using Receiver Function Analysis

Crustal Thickness of Funafuti Using Receiver Function Analysis

... a receiver station from very large distance ...near receiver function effects and due to the instrument ...near receiver effects are due to the local geological conditions near the ...

6

Imaging the Deep Structure of the Central DeathValley Basin Using Receiver Function, Gravity,and Magnetic Data

Imaging the Deep Structure of the Central DeathValley Basin Using Receiver Function, Gravity,and Magnetic Data

... use receiver function, gravity, and magnetic data to image the deep structures of central Death ...Valley. Receiver function analysis suggests the Moho is 24 km deep in the central part of the ...

13

Crustal Structure of the Salton Trough: Incorporation of Receiver Function, Gravity and Magnetic Data

Crustal Structure of the Salton Trough: Incorporation of Receiver Function, Gravity and Magnetic Data

... of receiver functions, gravity, and aero- magnetic data enable us to study a broad area of the Sal- ton Trough to determine its deep structure and answer important questions regarding the evolution of the Salton ...

11

Receiver function images of the central Chugoku region in the Japanese islands using Hi net data

Receiver function images of the central Chugoku region in the Japanese islands using Hi net data

... the receiver function approach using short-period Hi-net ...short-period receiver functions bring out discernible variations in average composition of the crust and its thickness in the study ...

10

Crust and uppermost mantle structure beneath central Japan inferred from receiver function analysis

Crust and uppermost mantle structure beneath central Japan inferred from receiver function analysis

... Our receiver function anal- ysis basically estimated S wave structures using Ps con- verted waves with a dominant frequency of about 1 Hz, while the explosion analysis uses reflected and/or refracted P waves ...

7

Crustal structure of western Hispaniola (Haiti) from a teleseismic receiver function study

Crustal structure of western Hispaniola (Haiti) from a teleseismic receiver function study

... A receiver function study of 23 stations is used to determine the crustal structure across Haiti, in order to place better constraints on the history and geometry of late Cretaceous to recent terrane ...

43

Lithospheric and sublithospheric deformation under the Borborema Province of northeastern Brazil from receiver function harmonic stripping

Lithospheric and sublithospheric deformation under the Borborema Province of northeastern Brazil from receiver function harmonic stripping

... interior, receiver function stripping reveal fast-axis orientations consistent with major regional shear zones, suggesting their continua- tion at depth into the lithospheric ...

13

Detailed structure of the upper mantle discontinuities around the Japan subduction zone imaged by receiver function analyses

Detailed structure of the upper mantle discontinuities around the Japan subduction zone imaged by receiver function analyses

... of 50 km under the influence of the stagnating PAC as a large cold thermal anomaly. These features could also be recognized in the topographical contour maps of the dis- continuities. The frequency dependence of the RFs ...

10

High resolution receiver function imaging of the seismic velocity discontinuities in the crust and the uppermost mantle beneath southwest Japan

High resolution receiver function imaging of the seismic velocity discontinuities in the crust and the uppermost mantle beneath southwest Japan

... Clear images of the seismic velocity discontinuities in the crust and the uppermost mantle beneath southwest Japan have been obtained with Receiver Function (RF) analyses of teleseismic waveforms observed ...

6

Receiver function images of the Hellenic subduction zone and comparison to microseismicity

Receiver function images of the Hellenic subduction zone and comparison to microseismicity

... The EGELADOS network consists of 56 on-shore stations deployed on the Greek mainland, on most of the southern Aegean islands and in western Turkey from October 2005 to April 2007. In addition, 24 off-shore stations were ...

17

Crustal Composition Beneath Southern Idaho: Insights from Teleseismic Receiver Functions

Crustal Composition Beneath Southern Idaho: Insights from Teleseismic Receiver Functions

... performed receiver function analyses to image the crustal structure of the HLP region using 206 seismic stations to perform both H-k stacking and Gaussian-weighted common conversion point ...

98

Constraints on the interpretation of S-to-P receiver functions

Constraints on the interpretation of S-to-P receiver functions

... Sp receiver functions for a range of epicentral distances might enhance true Sp receiver function phases and de-emphasize (or cancel) any erroneous phases, we have created a series of stacked traces ...

18

Evidence for partial melt in the crust beneath Mt  Paektu (Changbaishan), Democratic People's Republic of Korea and China

Evidence for partial melt in the crust beneath Mt Paektu (Changbaishan), Democratic People's Republic of Korea and China

... Mt. Paektu (also known as Changbaishan) is an enigmatic volcano on the border between the Democratic People ’ s Republic of Korea (DPRK) and China. Despite being responsible for one of the largest eruptions in history, ...

8

Lithospheric structure of the Arabian and Eurasian collision zone in eastern Turkey from S-wave receiver functions

Lithospheric structure of the Arabian and Eurasian collision zone in eastern Turkey from S-wave receiver functions

... P–wave receiver function studies have suggested that the crustal thickness in eastern Turkey is, on average, less than 45 km (C ¸ akir et al., 2003; Zor et al., 2003; C ¸ akir et al., 2004). The crustal ...

21

Depth Variation of the Lithosphere beneath Garoua Rift Region (Cameroon Volcanic Line) Studied from Teleseismic P Waves

Depth Variation of the Lithosphere beneath Garoua Rift Region (Cameroon Volcanic Line) Studied from Teleseismic P Waves

... the receiver function followed by the different values coming from Table 4 for the Garoua rift sector allow us to say that the crust is thin with a mean S-waves velocity of the of ...

16

Digital Communication Receivers Using Gaussian Processes for Machine Learning

Digital Communication Receivers Using Gaussian Processes for Machine Learning

... performance. Also, it makes the length of the training sequence hard to predict, as it depends on how well the chosen structure or hypeparameters fits the current problem. For example, SVM with a Gaussian kernel needs to ...

12

Glonass Software Receiver

Glonass Software Receiver

... GNSS receiver processes the GLONASS or GPS signal at the radio frequency or intermediate frequency depending on the hardware configuration of the ...software receiver, the front-end part converts the radio ...

7

Analysis and evaluation of uncertainty for conducted and radiated emissions tests

Analysis and evaluation of uncertainty for conducted and radiated emissions tests

... the receiver errors, its pulse amplitude response, variation with pulse repetition rate, sine wave voltage accuracy, noise floor and reading resolution should all be ...

33

A Sigma Delta ADC with Decimation and Gain Control Function for a Bluetooth Receiver in 130 nm Digital CMOS

A Sigma Delta ADC with Decimation and Gain Control Function for a Bluetooth Receiver in 130 nm Digital CMOS

... the receiver architecture more susceptible to noise folding and clock jitter e ff ects, it also provides significant advantages that make this technique very ...

8

Propagation Models for Wireless Communication System

Propagation Models for Wireless Communication System

... The free space path loss model is not directly related with the indoor propagation. As it is required to compute the path loss at a close-in reference distance as desired by the models. The free space model gives a ...

6

Show all 10000 documents...

Related subjects