FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2045491687> ?p ?o ?g. }

• W2045491687 endingPage "126" @default.
• W2045491687 startingPage "109" @default.
• W2045491687 abstract "Abstract The Solomon Islands lie along the India-Pacific plates' margin and have recorded a history of deformation resulting from the interaction of these two plates. Various kinematic models have been proposed for the Solomons and these have involved a variety of plate tectonic processes. It is pointed out that almost without exception these models have been based on a provincial geological classification of the island group in which it is assumed that two of these provinces—Pacific and Central provinces—commenced their geological development in regions distant from one another. Invariably such models require that Santa Isabel represents part of a collision zone between these two provinces, though field evidence from Santa Isabel for such a collision has in the past been largely lacking. These various kinematic models are examined in the light of more recent field evidence, and a premise on which they have been based—initial separate development for two of the provinces—is questioned. Rather it is here suggested that the Central and Pacific provinces developed in roughly similar positions, one with the other as they occur today, and that they were at least in part separated from Oligocene time onward by a linear peridotite-gabbro ridge, Korighole-Florida high, which acted as a sediment barrier to much of the coarser clastic and volcanogenic sedimentation. The initial development of the Solomon Islands began in an oceanic environment with the extrusion of extensive submarine tholeiitic ‘flood basalts’ and intrusion of associated gabbroic and ultramafic rocks at depth, during the Late Mesozoic to Early Tertiary. This igneous phase occurred with the whole of the island group representing the western margin of the Ontong Java Plateau. Subsequent asymmetric development of the Solomons during the Eocene and Oligocene resulted in uplift, shearing, and the initiation of arc volcanism, plutonism, and arc-related sedimentation in the Central province to the west. In contrast, through much of the Tertiary the Pacific province to the east continued to receive dominantly pelagic sediments before undergoing uplift and renewed deformation in the Pliocene. The recognition that the ophiolite crust in the Solomon Islands represents an autochthonous entity, which has acted as basement to subsequent arc volcanism, has significant implications on geochemical studies of these islands now being undertaken." @default.
• W2045491687 created "2016-06-24" @default.
• W2045491687 creator A5070966976 @default.
• W2045491687 date "1982-08-01" @default.
• W2045491687 modified "2023-09-25" @default.
• W2045491687 title "Crustal strain phenomena in the Solomon Islands, constraints from field evidence, and relationship to the India-Pacific plates' boundary" @default.
• W2045491687 cites W1963563659 @default.
• W2045491687 cites W1964766248 @default.
• W2045491687 cites W1968129135 @default.
• W2045491687 cites W1968145287 @default.
• W2045491687 cites W1972584846 @default.
• W2045491687 cites W1973707086 @default.
• W2045491687 cites W1978866236 @default.
• W2045491687 cites W1997435136 @default.
• W2045491687 cites W1999644999 @default.
• W2045491687 cites W2013144763 @default.
• W2045491687 cites W2022754373 @default.
• W2045491687 cites W2034039671 @default.
• W2045491687 cites W2038422013 @default.
• W2045491687 cites W2038801689 @default.
• W2045491687 cites W2040163630 @default.
• W2045491687 cites W2043170963 @default.
• W2045491687 cites W2047465867 @default.
• W2045491687 cites W2051718064 @default.
• W2045491687 cites W2061057540 @default.
• W2045491687 cites W2061185749 @default.
• W2045491687 cites W2063920449 @default.
• W2045491687 cites W2065982630 @default.
• W2045491687 cites W2070667160 @default.
• W2045491687 cites W2125860465 @default.
• W2045491687 cites W2138058376 @default.
• W2045491687 cites W2153560876 @default.
• W2045491687 cites W2318152314 @default.
• W2045491687 cites W2338336510 @default.
• W2045491687 cites W2489548358 @default.
• W2045491687 cites W2498555786 @default.
• W2045491687 cites W580465713 @default.
• W2045491687 doi "https://doi.org/10.1016/0040-1951(82)90223-2" @default.
• W2045491687 hasPublicationYear "1982" @default.
• W2045491687 type Work @default.
• W2045491687 sameAs 2045491687 @default.
• W2045491687 citedByCount "12" @default.
• W2045491687 countsByYear W20454916872013 @default.
• W2045491687 crossrefType "journal-article" @default.
• W2045491687 hasAuthorship W2045491687A5070966976 @default.
• W2045491687 hasConcept C119477230 @default.
• W2045491687 hasConcept C126322002 @default.
• W2045491687 hasConcept C127313418 @default.
• W2045491687 hasConcept C134306372 @default.
• W2045491687 hasConcept C165205528 @default.
• W2045491687 hasConcept C202444582 @default.
• W2045491687 hasConcept C2778022156 @default.
• W2045491687 hasConcept C33923547 @default.
• W2045491687 hasConcept C62354387 @default.
• W2045491687 hasConcept C71924100 @default.
• W2045491687 hasConcept C77928131 @default.
• W2045491687 hasConcept C9652623 @default.
• W2045491687 hasConceptScore W2045491687C119477230 @default.
• W2045491687 hasConceptScore W2045491687C126322002 @default.
• W2045491687 hasConceptScore W2045491687C127313418 @default.
• W2045491687 hasConceptScore W2045491687C134306372 @default.
• W2045491687 hasConceptScore W2045491687C165205528 @default.
• W2045491687 hasConceptScore W2045491687C202444582 @default.
• W2045491687 hasConceptScore W2045491687C2778022156 @default.
• W2045491687 hasConceptScore W2045491687C33923547 @default.
• W2045491687 hasConceptScore W2045491687C62354387 @default.
• W2045491687 hasConceptScore W2045491687C71924100 @default.
• W2045491687 hasConceptScore W2045491687C77928131 @default.
• W2045491687 hasConceptScore W2045491687C9652623 @default.
• W2045491687 hasIssue "1-4" @default.
• W2045491687 hasLocation W20454916871 @default.
• W2045491687 hasOpenAccess W2045491687 @default.
• W2045491687 hasPrimaryLocation W20454916871 @default.
• W2045491687 hasRelatedWork W1835804368 @default.
• W2045491687 hasRelatedWork W1996539453 @default.
• W2045491687 hasRelatedWork W2020996000 @default.
• W2045491687 hasRelatedWork W2068691254 @default.
• W2045491687 hasRelatedWork W2081799716 @default.
• W2045491687 hasRelatedWork W2092739438 @default.
• W2045491687 hasRelatedWork W2326141141 @default.
• W2045491687 hasRelatedWork W2780068850 @default.
• W2045491687 hasRelatedWork W2889647951 @default.
• W2045491687 hasRelatedWork W3087925122 @default.
• W2045491687 hasVolume "87" @default.
• W2045491687 isParatext "false" @default.
• W2045491687 isRetracted "false" @default.
• W2045491687 magId "2045491687" @default.
• W2045491687 workType "article" @default.