FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2113754355> ?p ?o ?g. }

• W2113754355 endingPage "250" @default.
• W2113754355 startingPage "229" @default.
• W2113754355 abstract "The Philippine Sea Plate is the one major plate whose Tertiary motion is poorly constrained and whose origin is problematical. Its southern boundary is the Sorong Fault system which is part of a major left-lateral fault system at the northern margin of the Australian plate. The southern part of the plate in eastern Indonesia has been neglected in most syntheses but includes some of the oldest rocks within the plate which are separated from remnant arcs of the Daito Ridge province of the northern Philippine Sea by the West Philippine Central Basin. The east Indonesian islands of the Halmahera-Waigeo region contain a good Mesozoic and Tertiary stratigraphic record indicating a long arc history for the southern part of the plate. New palaeomagnetic data from these islands define two sub-areas: an area forming part of the Philippine Sea Plate north of the Sorong Fault, and an area within the Sorong Fault system. The area north of the fault records a long-term clockwise rotation history whereas that within the fault zone records local rotations interpreted as due to deformation at the plate edge. Rocks of Philippine Sea Plate origin within both areas record similar latitudinal shifts. The rotation of the area north of the Sorong Fault is considered to represent the motion of the southern part of the Philippine Sea Plate. The new data indicate large Tertiary clockwise rotations similar to earlier suggestions for other parts of the plate but record a discontinuous and more complex motion history than previously suggested. For the southern part of the plate there was 40° rotation with northward translation between 0 and 25 Ma, no significant rotation between 25 and 40 Ma, and there was 50° rotation with southward translation between 40 and 50 Ma. We show that the new palaeomagnetic data form part of a single set with earlier palaeomagnetic data from elsewhere in the plate. The translation history of the southern part of the plate in eastern Indonesia can be reconciled with northward motions recorded elsewhere and can be used to determine rotation poles for the plate (15°N, 160°E for the interval 5–25 Ma, and 10°N, 150°E for the interval 40–50 Ma). Reconstructions based on these poles predict that at ∼ 45 Ma the Palau-Kyushu Ridge had a WNW-ESE orientation which is very different from that postulated by many models used to explain the widespread boninite volcanism in the Izu-Bonin-Marians forearc at this time. The long arc history of the southern part of the plate and the reconstructions based on the rotation poles calculated from the palaeomagnetic data favour an origin for the West Philippine Basin by spreading in a backarc basin." @default.
• W2113754355 created "2016-06-24" @default.
• W2113754355 creator A5029279057 @default.
• W2113754355 creator A5061943510 @default.
• W2113754355 creator A5071547804 @default.
• W2113754355 creator A5078474965 @default.
• W2113754355 date "1995-12-01" @default.
• W2113754355 modified "2023-10-17" @default.
• W2113754355 title "Origin and motion history of the Philippine Sea Plate" @default.
• W2113754355 cites W1975610806 @default.
• W2113754355 cites W1979995210 @default.
• W2113754355 cites W1980336881 @default.
• W2113754355 cites W1987480649 @default.
• W2113754355 cites W1990539053 @default.
• W2113754355 cites W1994162068 @default.
• W2113754355 cites W2000820683 @default.
• W2113754355 cites W2001409771 @default.
• W2113754355 cites W2003689738 @default.
• W2113754355 cites W2009074071 @default.
• W2113754355 cites W2011449231 @default.
• W2113754355 cites W2011828112 @default.
• W2113754355 cites W2014086849 @default.
• W2113754355 cites W2016405844 @default.
• W2113754355 cites W2018840589 @default.
• W2113754355 cites W2021926308 @default.
• W2113754355 cites W2026511343 @default.
• W2113754355 cites W2029331927 @default.
• W2113754355 cites W2031179521 @default.
• W2113754355 cites W2032112226 @default.
• W2113754355 cites W2042822656 @default.
• W2113754355 cites W2047519592 @default.
• W2113754355 cites W2047850677 @default.
• W2113754355 cites W2053444229 @default.
• W2113754355 cites W2055763953 @default.
• W2113754355 cites W2063697073 @default.
• W2113754355 cites W2066948777 @default.
• W2113754355 cites W2069812478 @default.
• W2113754355 cites W2073347403 @default.
• W2113754355 cites W2073572165 @default.
• W2113754355 cites W2075861798 @default.
• W2113754355 cites W2078167445 @default.
• W2113754355 cites W2086526440 @default.
• W2113754355 cites W2097707258 @default.
• W2113754355 cites W2102203717 @default.
• W2113754355 cites W2103655542 @default.
• W2113754355 cites W2127630063 @default.
• W2113754355 cites W2133303366 @default.
• W2113754355 cites W2149028004 @default.
• W2113754355 cites W2151289207 @default.
• W2113754355 cites W2151646049 @default.
• W2113754355 doi "https://doi.org/10.1016/0040-1951(95)00038-0" @default.
• W2113754355 hasPublicationYear "1995" @default.
• W2113754355 type Work @default.
• W2113754355 sameAs 2113754355 @default.
• W2113754355 citedByCount "254" @default.
• W2113754355 countsByYear W21137543552012 @default.
• W2113754355 countsByYear W21137543552013 @default.
• W2113754355 countsByYear W21137543552014 @default.
• W2113754355 countsByYear W21137543552015 @default.
• W2113754355 countsByYear W21137543552016 @default.
• W2113754355 countsByYear W21137543552017 @default.
• W2113754355 countsByYear W21137543552018 @default.
• W2113754355 countsByYear W21137543552019 @default.
• W2113754355 countsByYear W21137543552020 @default.
• W2113754355 countsByYear W21137543552021 @default.
• W2113754355 countsByYear W21137543552022 @default.
• W2113754355 countsByYear W21137543552023 @default.
• W2113754355 crossrefType "journal-article" @default.
• W2113754355 hasAuthorship W2113754355A5029279057 @default.
• W2113754355 hasAuthorship W2113754355A5061943510 @default.
• W2113754355 hasAuthorship W2113754355A5071547804 @default.
• W2113754355 hasAuthorship W2113754355A5078474965 @default.
• W2113754355 hasConcept C106973953 @default.
• W2113754355 hasConcept C109007969 @default.
• W2113754355 hasConcept C119477230 @default.
• W2113754355 hasConcept C127313418 @default.
• W2113754355 hasConcept C151730666 @default.
• W2113754355 hasConcept C165205528 @default.
• W2113754355 hasConcept C175551986 @default.
• W2113754355 hasConcept C2524010 @default.
• W2113754355 hasConcept C2778261408 @default.
• W2113754355 hasConcept C32277403 @default.
• W2113754355 hasConcept C33923547 @default.
• W2113754355 hasConcept C58097730 @default.
• W2113754355 hasConcept C70026782 @default.
• W2113754355 hasConcept C74050887 @default.
• W2113754355 hasConcept C77928131 @default.
• W2113754355 hasConceptScore W2113754355C106973953 @default.
• W2113754355 hasConceptScore W2113754355C109007969 @default.
• W2113754355 hasConceptScore W2113754355C119477230 @default.
• W2113754355 hasConceptScore W2113754355C127313418 @default.
• W2113754355 hasConceptScore W2113754355C151730666 @default.
• W2113754355 hasConceptScore W2113754355C165205528 @default.
• W2113754355 hasConceptScore W2113754355C175551986 @default.
• W2113754355 hasConceptScore W2113754355C2524010 @default.
• W2113754355 hasConceptScore W2113754355C2778261408 @default.
• W2113754355 hasConceptScore W2113754355C32277403 @default.
• W2113754355 hasConceptScore W2113754355C33923547 @default.

• next