FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W1989890219> ?p ?o ?g. }

• W1989890219 endingPage "67" @default.
• W1989890219 startingPage "49" @default.
• W1989890219 abstract "We modelled the state of stress in the Indo-Australian plate in order to investigate quantitatively variations observed in tectonic style. The numerical procedure incorporates the dependence of slab pull and ridge push on the age of the oceanic lithosphere. Estimates are presented for the average net resistive forces at the Himalayan collision zone, the suction force acting on the overriding Indo-Australian plate segment at the Tonga-Kermadec trench and the drag at the base of the lithosphere. Our modelling shows a concentration of compressive stresses of the order of 3–5 kbar in the Ninetyeast Ridge area; the effects of the compressive resistance associated with Himalayan collision and subduction of young lithosphere off the northern part of the Sunda arc are focused in this region. The stress field as calculated gives a consistent explanation for the observed concentration of seismic activity (Stein and Okal, 1978) and significant deformation in the oceanic crust (Weissel et al., 1980; McAdoo and Sandwell, 1985) in the area. The calculated stress field in the area adjacent to the Southeast and Central India ridges is characterized by tension parallel to the spreading axis. This explains the concentration of near-ridge normal faulting seismicity (with T-axes subparallel to the spreading ridge) in the Indian Ocean as recently observed by Bergman et al. (1984) and Wiens and Stein (1984). The regional stress field along the strike of the Sunda arc varies from compression seaward of and parallel to the Sumatra trench segment, to tension perpendicular to the Java-Flores segment. This explains the selective occurrence of well developed grabens seaward off the Java-Flores segment of the trench, observed by Hilde (1983). Our modelling shows that the observed rotation of the stress field (Denham et al., 1979) in the Australian continent is mainly the consequence of its geographic position relative to the surrounding trench segments and the variations of the forces acting on the down-going slab in each of these. The state of compression in west and central Australia is induced by the action of resistive forces at the Himalayan and Banda arc collision zones. The joint occurrence of high levels of compression in the plate's interior and normal faulting seismicity in the near-ridge areas, is a transient feature unique to the present dynamic situation of the Indo-Australian plate." @default.
• W1989890219 created "2016-06-24" @default.
• W1989890219 creator A5034750019 @default.
• W1989890219 creator A5053199599 @default.
• W1989890219 date "1986-12-01" @default.
• W1989890219 modified "2023-10-18" @default.
• W1989890219 title "Stress in the Indo-Australian plate" @default.
• W1989890219 cites W1964531948 @default.
• W1989890219 cites W1968771872 @default.
• W1989890219 cites W1973831400 @default.
• W1989890219 cites W1975467990 @default.
• W1989890219 cites W1975531310 @default.
• W1989890219 cites W1978752202 @default.
• W1989890219 cites W1980013965 @default.
• W1989890219 cites W1981318751 @default.
• W1989890219 cites W1983105885 @default.
• W1989890219 cites W1991794762 @default.
• W1989890219 cites W1992357382 @default.
• W1989890219 cites W1997028645 @default.
• W1989890219 cites W1997639965 @default.
• W1989890219 cites W1998171101 @default.
• W1989890219 cites W1999221527 @default.
• W1989890219 cites W2004758340 @default.
• W1989890219 cites W2006120514 @default.
• W1989890219 cites W2007522187 @default.
• W1989890219 cites W2007738582 @default.
• W1989890219 cites W2009930154 @default.
• W1989890219 cites W2011849025 @default.
• W1989890219 cites W2011893217 @default.
• W1989890219 cites W2012056720 @default.
• W1989890219 cites W2012364516 @default.
• W1989890219 cites W2020607039 @default.
• W1989890219 cites W2025244602 @default.
• W1989890219 cites W2026702414 @default.
• W1989890219 cites W2039675144 @default.
• W1989890219 cites W2046040521 @default.
• W1989890219 cites W2047390315 @default.
• W1989890219 cites W2047712588 @default.
• W1989890219 cites W2054301859 @default.
• W1989890219 cites W2056627155 @default.
• W1989890219 cites W2059122312 @default.
• W1989890219 cites W2060968338 @default.
• W1989890219 cites W2061261978 @default.
• W1989890219 cites W2068654805 @default.
• W1989890219 cites W2073180550 @default.
• W1989890219 cites W2074105632 @default.
• W1989890219 cites W2079276733 @default.
• W1989890219 cites W2079460275 @default.
• W1989890219 cites W2093208210 @default.
• W1989890219 cites W2094268781 @default.
• W1989890219 cites W2105511586 @default.
• W1989890219 cites W2121329342 @default.
• W1989890219 cites W2126039538 @default.
• W1989890219 cites W2138663870 @default.
• W1989890219 cites W2139668189 @default.
• W1989890219 cites W2162584013 @default.
• W1989890219 cites W2167008662 @default.
• W1989890219 cites W2168052720 @default.
• W1989890219 cites W2170219059 @default.
• W1989890219 cites W2170434968 @default.
• W1989890219 doi "https://doi.org/10.1016/0040-1951(86)90024-7" @default.
• W1989890219 hasPublicationYear "1986" @default.
• W1989890219 type Work @default.
• W1989890219 sameAs 1989890219 @default.
• W1989890219 citedByCount "315" @default.
• W1989890219 countsByYear W19898902192012 @default.
• W1989890219 countsByYear W19898902192013 @default.
• W1989890219 countsByYear W19898902192014 @default.
• W1989890219 countsByYear W19898902192015 @default.
• W1989890219 countsByYear W19898902192016 @default.
• W1989890219 countsByYear W19898902192017 @default.
• W1989890219 countsByYear W19898902192018 @default.
• W1989890219 countsByYear W19898902192019 @default.
• W1989890219 countsByYear W19898902192020 @default.
• W1989890219 countsByYear W19898902192021 @default.
• W1989890219 countsByYear W19898902192022 @default.
• W1989890219 countsByYear W19898902192023 @default.
• W1989890219 crossrefType "journal-article" @default.
• W1989890219 hasAuthorship W1989890219A5034750019 @default.
• W1989890219 hasAuthorship W1989890219A5053199599 @default.
• W1989890219 hasBestOaLocation W19898902192 @default.
• W1989890219 hasConcept C113740112 @default.
• W1989890219 hasConcept C121332964 @default.
• W1989890219 hasConcept C127313418 @default.
• W1989890219 hasConcept C135628077 @default.
• W1989890219 hasConcept C151730666 @default.
• W1989890219 hasConcept C154200439 @default.
• W1989890219 hasConcept C155310634 @default.
• W1989890219 hasConcept C159985019 @default.
• W1989890219 hasConcept C165205528 @default.
• W1989890219 hasConcept C16942324 @default.
• W1989890219 hasConcept C178790620 @default.
• W1989890219 hasConcept C180016635 @default.
• W1989890219 hasConcept C185592680 @default.
• W1989890219 hasConcept C186068551 @default.
• W1989890219 hasConcept C192367031 @default.
• W1989890219 hasConcept C192562407 @default.
• W1989890219 hasConcept C2776698055 @default.

• next