Non-uniqueness in the determination of crustal and upper-mantle velocity structure from receiver function;Kabuk ve üst-manto hiz yapisinin saptanmasinda alici fonksiyonun çok çözümlülüǧü

Yerbilimleri

Volumn , Issue 23, 2001, Pages 99-112

  Erduran, M ^a   Cakir O ^a  

^a KARADENIZ TECHNICAL UNIVERSITY   (Turkey)

Author keywords

Initial model; Inversion; Non uniqueness; Receiver function; Surface waves; Tele seismic

Indexed keywords

CRUST; DATA PROCESSING; SEISMIC DATA; SEISMIC VELOCITY; UPPER MANTLE;

EID: 0034914325     PISSN: 13012894     EISSN: None     Source Type: Journal    
DOI: None     Document Type: Article

References (24)

1. The isolation of receiver effects from teleseismic P waveforms
2. Receiver structure beneath the Southern Mojave Block, California
3. On the nonuniqueness of receiver function inversions
4. Numerical experiments in broadband receiver function analysis
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6. The effect of the initial earthquake phase shift on the inversion of regional surface wave recordings for the estimation of crustal structure
7. Numerical Analysis of Dispersed Seismic Waves
8. Crustal reflection of plane P and SV waves
9. The receiver structure beneath the Ebro Basin, Iberian Peninsula
10. Receiver functions for the Tien Shan analog broadband network: Contrasts in the evolution of structures across the Talasso-Fergana fault
11. Structure under mount rainier, Washington, inferred from teleseismic body waves
12. Scattering of teleseismic body waves under Pasadena, California
13. Source effects on surface wave group travel times and group velocity maps
14. The receiver structure beneath Mina, Nevada
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16. The reflectivity method: A tutorial
17. Crustal structure of the Adirondacks determined from broadband teleseismic waveform modeling
18. Seismic evidence for an ancient rift beneath the Cumberland Plateau, Tennessee: A detailed analysis of broadband telesismic P waveforms
19. Shear wave velocity structure in the northern Basin and range Province from the combined analysis of receiver functions and surface waves
20. Grid search modeling of receiver functions: Implications for crustal structure in the Middle East and North Africa
21. Crustal thickness variations across the colorado rocky mountains from teleseismic receiver functions
22. Lateral variation in crustal structure of the northern Tibetan Plateau inferred from teleseismic receiver functions