FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W4298620721> ?p ?o ?g. }

• W4298620721 endingPage "708" @default.
• W4298620721 startingPage "700" @default.
• W4298620721 abstract "Teleseismic receiver function (RF) analysis traditionally has targeted deep earth structures in the context of observational seismology, allowing the detection of converted seismic phases originating from major boundaries of impedance. Recent efforts to adapt this passive-source seismic imaging technique to basin-scale subsurface characterization have retrieved primary basin geometries and key stratigraphic boundaries by relying on densely deployed broadband seismometer networks. While accurate interpretation of RF time series on Earth benefitted from complementary subsurface constraints (e.g., core and well logs), lack of such resources and instrumental limitations must be considered in the context of planetary geophysics, where passive-source imaging may emerge as a key frontier exploration technique. Thus, it is important to establish an analysis framework in which observed RF signals are interpreted by relying on first-order suppositions about the physical properties of the underlying subsurface. In this work, we seek to simulate this approach in single-station scenarios and qualitatively examine the baseline information inferable from the RF time series. Our results suggest that signals observed in the sedimentary interval can be reasonably attributed to major impedance changes expected from the generalized lithostratigraphy of the local subsurface, including the transition to the underlying crust. We also find patterns of anisotropy-related directional variations in high-frequency signals as well as unique frequency-dependent responses likely associated with the depth and vertical dimension of converting boundaries. Together, these seismic observables enable inference of various geologic attributes within the underlying sedimentary unit, proving it to be a critical tool in future efforts of planetary exploration." @default.
• W4298620721 created "2022-10-02" @default.
• W4298620721 creator A5036381161 @default.
• W4298620721 creator A5067548058 @default.
• W4298620721 date "2022-10-01" @default.
• W4298620721 modified "2023-09-27" @default.
• W4298620721 title "Basin-scale subsurface characterization using single-station teleseismic receiver function analysis" @default.
• W4298620721 cites W1596847809 @default.
• W4298620721 cites W1956866179 @default.
• W4298620721 cites W1964565818 @default.
• W4298620721 cites W1993910965 @default.
• W4298620721 cites W2009578631 @default.
• W4298620721 cites W2032905426 @default.
• W4298620721 cites W2036003398 @default.
• W4298620721 cites W2096728475 @default.
• W4298620721 cites W2103113534 @default.
• W4298620721 cites W2123854137 @default.
• W4298620721 cites W2136138284 @default.
• W4298620721 cites W2146376665 @default.
• W4298620721 cites W2401221840 @default.
• W4298620721 cites W2484222816 @default.
• W4298620721 cites W2595718594 @default.
• W4298620721 cites W2939096408 @default.
• W4298620721 cites W3006706642 @default.
• W4298620721 cites W3040588332 @default.
• W4298620721 cites W3101298231 @default.
• W4298620721 cites W3103810916 @default.
• W4298620721 cites W3175553812 @default.
• W4298620721 cites W3184973091 @default.
• W4298620721 cites W3206920089 @default.
• W4298620721 cites W4243049017 @default.
• W4298620721 cites W4361805491 @default.
• W4298620721 doi "https://doi.org/10.1190/tle41100700.1" @default.
• W4298620721 hasPublicationYear "2022" @default.
• W4298620721 type Work @default.
• W4298620721 citedByCount "0" @default.
• W4298620721 crossrefType "journal-article" @default.
• W4298620721 hasAuthorship W4298620721A5036381161 @default.
• W4298620721 hasAuthorship W4298620721A5067548058 @default.
• W4298620721 hasConcept C109007969 @default.
• W4298620721 hasConcept C114793014 @default.
• W4298620721 hasConcept C119217923 @default.
• W4298620721 hasConcept C127313418 @default.
• W4298620721 hasConcept C151730666 @default.
• W4298620721 hasConcept C165205528 @default.
• W4298620721 hasConcept C2779343474 @default.
• W4298620721 hasConcept C8058405 @default.
• W4298620721 hasConceptScore W4298620721C109007969 @default.
• W4298620721 hasConceptScore W4298620721C114793014 @default.
• W4298620721 hasConceptScore W4298620721C119217923 @default.
• W4298620721 hasConceptScore W4298620721C127313418 @default.
• W4298620721 hasConceptScore W4298620721C151730666 @default.
• W4298620721 hasConceptScore W4298620721C165205528 @default.
• W4298620721 hasConceptScore W4298620721C2779343474 @default.
• W4298620721 hasConceptScore W4298620721C8058405 @default.
• W4298620721 hasIssue "10" @default.
• W4298620721 hasLocation W42986207211 @default.
• W4298620721 hasOpenAccess W4298620721 @default.
• W4298620721 hasPrimaryLocation W42986207211 @default.
• W4298620721 hasRelatedWork W1600609014 @default.
• W4298620721 hasRelatedWork W1979427886 @default.
• W4298620721 hasRelatedWork W2053983673 @default.
• W4298620721 hasRelatedWork W2075653097 @default.
• W4298620721 hasRelatedWork W2164879895 @default.
• W4298620721 hasRelatedWork W2942079230 @default.
• W4298620721 hasRelatedWork W2952681387 @default.
• W4298620721 hasRelatedWork W3016255354 @default.
• W4298620721 hasRelatedWork W3113596969 @default.
• W4298620721 hasRelatedWork W4253374395 @default.
• W4298620721 hasVolume "41" @default.
• W4298620721 isParatext "false" @default.
• W4298620721 isRetracted "false" @default.
• W4298620721 workType "article" @default.