Matches in SemOpenAlex for { <https://semopenalex.org/work/W2094723215> ?p ?o ?g. }
Showing items 1 to 76 of
76
with 100 items per page.
- W2094723215 endingPage "129" @default.
- W2094723215 startingPage "119" @default.
- W2094723215 abstract "Abstract Two aseismically creeping long vertical surface-breaking parallel strike-slip faults are taken to be situated in an elastic layer, resting on and in welded contact with a visco-elastic halfspace, representing the lithosphere-asthenosphere system. Solutions are obtained for the displacements, stresses and strains, using a technique involving the use of Green's functions and integral transforms, for three possible cases—the case of the absence of any fault creep, the case in which one fault is creeping and the other is locked and the case in which both faults are creeping, taking into account the displacements and stresses present initially, and assuming that the tectonic forces maintain a shear strain far away from the faults. The types of fault creep for which the displacements, stresses and strains are finite everywhere in the model near the faults are identified, and the conditions satisfied by these types of fault creep are determined in a simple form. Fault creep across a fault is generally found to reduce the rate of accumulation of shear stress near the fault. The effect of aseismic creep across one fault on the shear stress near the other fault is found to depend on the distance, dimensions, relative position and other characteristics of the two faults. Fault creep across one fault is generally found to reduce the rate of shear stress accumulation near the neighbouring fault in the theoretical model considered. Under suitable circumstances, aseismic creep across one of the faults is found to result in aseismic release of shear stress near both faults, thus reducing progressively the possibility of a sudden fault movement generating an earthquake. The influence of one creeping fault on another is found to decrease rapidly with increase in the distance between the faults. The possible uses of the model in the study of the interaction between neighbouring strike-slip faults in a layered model representing the lithosphere-asthenosphere system and in the estimation of return times of earthquakes is examined." @default.
- W2094723215 created "2016-06-24" @default.
- W2094723215 creator A5005843734 @default.
- W2094723215 creator A5013155794 @default.
- W2094723215 creator A5069322368 @default.
- W2094723215 date "1992-02-01" @default.
- W2094723215 modified "2023-09-24" @default.
- W2094723215 title "On two interacting creeping vertical surface-breaking strike-slip faults in a two-layer model of the lithosphere" @default.
- W2094723215 cites W1967488184 @default.
- W2094723215 cites W1968292600 @default.
- W2094723215 cites W2101584727 @default.
- W2094723215 cites W2469240176 @default.
- W2094723215 doi "https://doi.org/10.1016/0031-9201(92)90166-s" @default.
- W2094723215 hasPublicationYear "1992" @default.
- W2094723215 type Work @default.
- W2094723215 sameAs 2094723215 @default.
- W2094723215 citedByCount "16" @default.
- W2094723215 countsByYear W20947232152013 @default.
- W2094723215 countsByYear W20947232152017 @default.
- W2094723215 countsByYear W20947232152019 @default.
- W2094723215 countsByYear W20947232152020 @default.
- W2094723215 crossrefType "journal-article" @default.
- W2094723215 hasAuthorship W2094723215A5005843734 @default.
- W2094723215 hasAuthorship W2094723215A5013155794 @default.
- W2094723215 hasAuthorship W2094723215A5069322368 @default.
- W2094723215 hasConcept C121332964 @default.
- W2094723215 hasConcept C127313418 @default.
- W2094723215 hasConcept C159985019 @default.
- W2094723215 hasConcept C165205528 @default.
- W2094723215 hasConcept C169162353 @default.
- W2094723215 hasConcept C16942324 @default.
- W2094723215 hasConcept C175551986 @default.
- W2094723215 hasConcept C192562407 @default.
- W2094723215 hasConcept C195268267 @default.
- W2094723215 hasConcept C2524010 @default.
- W2094723215 hasConcept C2779227376 @default.
- W2094723215 hasConcept C33923547 @default.
- W2094723215 hasConcept C77928131 @default.
- W2094723215 hasConcept C8058405 @default.
- W2094723215 hasConcept C97355855 @default.
- W2094723215 hasConceptScore W2094723215C121332964 @default.
- W2094723215 hasConceptScore W2094723215C127313418 @default.
- W2094723215 hasConceptScore W2094723215C159985019 @default.
- W2094723215 hasConceptScore W2094723215C165205528 @default.
- W2094723215 hasConceptScore W2094723215C169162353 @default.
- W2094723215 hasConceptScore W2094723215C16942324 @default.
- W2094723215 hasConceptScore W2094723215C175551986 @default.
- W2094723215 hasConceptScore W2094723215C192562407 @default.
- W2094723215 hasConceptScore W2094723215C195268267 @default.
- W2094723215 hasConceptScore W2094723215C2524010 @default.
- W2094723215 hasConceptScore W2094723215C2779227376 @default.
- W2094723215 hasConceptScore W2094723215C33923547 @default.
- W2094723215 hasConceptScore W2094723215C77928131 @default.
- W2094723215 hasConceptScore W2094723215C8058405 @default.
- W2094723215 hasConceptScore W2094723215C97355855 @default.
- W2094723215 hasIssue "1-2" @default.
- W2094723215 hasLocation W20947232151 @default.
- W2094723215 hasOpenAccess W2094723215 @default.
- W2094723215 hasPrimaryLocation W20947232151 @default.
- W2094723215 hasRelatedWork W1965098282 @default.
- W2094723215 hasRelatedWork W2011865941 @default.
- W2094723215 hasRelatedWork W2035438132 @default.
- W2094723215 hasRelatedWork W2125913561 @default.
- W2094723215 hasRelatedWork W2150931249 @default.
- W2094723215 hasRelatedWork W2355282060 @default.
- W2094723215 hasRelatedWork W2381232108 @default.
- W2094723215 hasRelatedWork W2393073071 @default.
- W2094723215 hasRelatedWork W4211118788 @default.
- W2094723215 hasRelatedWork W4220675906 @default.
- W2094723215 hasVolume "70" @default.
- W2094723215 isParatext "false" @default.
- W2094723215 isRetracted "false" @default.
- W2094723215 magId "2094723215" @default.
- W2094723215 workType "article" @default.