FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2024113251> ?p ?o ?g. }

• W2024113251 endingPage "553" @default.
• W2024113251 startingPage "520" @default.
• W2024113251 abstract "The Derewo Metamorphic Belt (also known as the Ruffaer Metamorphic Belt) is a >500 km long, narrow (~10-30 km wide), roughly E-W-trending terrane composed mostly of slate and phyllite, on the northern flank of the Central Range of Papua, Indonesia (west New Guinea). This investigation, the first systematic petrologic study of the belt, is based on petrographic and mineral chemical analysis of 133 samples collected across the 1:250,000 scale Hitalipa Geologic Map Sheet. The southern edge of the Derewo Metamorphics (DM) is a structural boundary, the Derewo fault, in the western half of the map and gradational with unmetamorphosed passive margin strata in the eastern half. The northern boundary of the DM is a fault contact with the Irian Ophiolite Belt. The metamorphic protoliths are Jurassic-Cretaceous Australian passive-margin strata (Kembelangan Group). Most of the rock in the DM is of pelitic bulk composition. The common mineral assemblage is quartz + white mica + chlorite + pyrite + graphite, with many samples containing albite, mixed layer muscovite/paragonite, and/or calcite. Spessartine garnet and iron-rich chloritoid are present but rare. Volumetrically minor protoliths were siltstones or sandstones and rare probable mafic ash beds. Metamorphosed silt- and sandstones contain quartz + albite + potassium feldspar + white mica ± biotite ± calcite. Mafic compositions contain actinolite + epidote + chlorite + albite + white mica + calcite + quartz + titanite. Thermobarometry based on mineral assemblages and compositions indicates the DM in the Hitalipa area experienced peak metamorphic conditions of 250-350°C at 5-8 kbar (burial depths of 15 to 25 km). The DM formed as continental rise and slope sediments that entered a north-dipping subduction zone since 30 Ma. Major uplift from collisional orogenesis began at ~8 Ma when positively buoyant Australian continent-capped lithosphere began to bend downward to subduct. The present-day high topography of the Central Range was established by ~4 Ma when delamination of the subducting plate was complete, and collisional movements changed into a left-lateral transform fault system. Tens of km of strike-slip displacement occurred within the core of the Central Range, offsetting parts of the metamorphic belt along the Derewo and related faults." @default.
• W2024113251 created "2016-06-24" @default.
• W2024113251 creator A5015852000 @default.
• W2024113251 creator A5019331858 @default.
• W2024113251 date "2007-06-01" @default.
• W2024113251 modified "2023-10-16" @default.
• W2024113251 title "Petrology and Tectonics of the Derewo Metamorphic Belt, West New Guinea" @default.
• W2024113251 cites W1988181429 @default.
• W2024113251 cites W1994816727 @default.
• W2024113251 cites W1995733167 @default.
• W2024113251 cites W2003775021 @default.
• W2024113251 cites W2020587493 @default.
• W2024113251 cites W2022957944 @default.
• W2024113251 cites W2039817695 @default.
• W2024113251 cites W2041076515 @default.
• W2024113251 cites W2043429131 @default.
• W2024113251 cites W2048742589 @default.
• W2024113251 cites W2056645976 @default.
• W2024113251 cites W2061237804 @default.
• W2024113251 cites W2071908704 @default.
• W2024113251 cites W2075618665 @default.
• W2024113251 cites W2075788454 @default.
• W2024113251 cites W2088779208 @default.
• W2024113251 cites W2100629704 @default.
• W2024113251 cites W2111555634 @default.
• W2024113251 cites W2121440949 @default.
• W2024113251 cites W2128396588 @default.
• W2024113251 cites W2132593853 @default.
• W2024113251 cites W2136724508 @default.
• W2024113251 cites W2144222955 @default.
• W2024113251 cites W2145833815 @default.
• W2024113251 cites W2172263446 @default.
• W2024113251 cites W4210999665 @default.
• W2024113251 cites W4240401051 @default.
• W2024113251 cites W4298437071 @default.
• W2024113251 doi "https://doi.org/10.2747/0020-6814.49.6.520" @default.
• W2024113251 hasPublicationYear "2007" @default.
• W2024113251 type Work @default.
• W2024113251 sameAs 2024113251 @default.
• W2024113251 citedByCount "10" @default.
• W2024113251 countsByYear W20241132512012 @default.
• W2024113251 countsByYear W20241132512013 @default.
• W2024113251 countsByYear W20241132512018 @default.
• W2024113251 countsByYear W20241132512019 @default.
• W2024113251 countsByYear W20241132512020 @default.
• W2024113251 countsByYear W20241132512021 @default.
• W2024113251 countsByYear W20241132512022 @default.
• W2024113251 crossrefType "journal-article" @default.
• W2024113251 hasAuthorship W2024113251A5015852000 @default.
• W2024113251 hasAuthorship W2024113251A5019331858 @default.
• W2024113251 hasConcept C101139013 @default.
• W2024113251 hasConcept C109007969 @default.
• W2024113251 hasConcept C114793014 @default.
• W2024113251 hasConcept C127313418 @default.
• W2024113251 hasConcept C146588470 @default.
• W2024113251 hasConcept C150999391 @default.
• W2024113251 hasConcept C151730666 @default.
• W2024113251 hasConcept C165205528 @default.
• W2024113251 hasConcept C167284885 @default.
• W2024113251 hasConcept C17409809 @default.
• W2024113251 hasConcept C26687426 @default.
• W2024113251 hasConcept C26815474 @default.
• W2024113251 hasConcept C2777844515 @default.
• W2024113251 hasConcept C2778357522 @default.
• W2024113251 hasConcept C2779870107 @default.
• W2024113251 hasConcept C5900021 @default.
• W2024113251 hasConcept C77928131 @default.
• W2024113251 hasConcept C79927612 @default.
• W2024113251 hasConcept C95628711 @default.
• W2024113251 hasConceptScore W2024113251C101139013 @default.
• W2024113251 hasConceptScore W2024113251C109007969 @default.
• W2024113251 hasConceptScore W2024113251C114793014 @default.
• W2024113251 hasConceptScore W2024113251C127313418 @default.
• W2024113251 hasConceptScore W2024113251C146588470 @default.
• W2024113251 hasConceptScore W2024113251C150999391 @default.
• W2024113251 hasConceptScore W2024113251C151730666 @default.
• W2024113251 hasConceptScore W2024113251C165205528 @default.
• W2024113251 hasConceptScore W2024113251C167284885 @default.
• W2024113251 hasConceptScore W2024113251C17409809 @default.
• W2024113251 hasConceptScore W2024113251C26687426 @default.
• W2024113251 hasConceptScore W2024113251C26815474 @default.
• W2024113251 hasConceptScore W2024113251C2777844515 @default.
• W2024113251 hasConceptScore W2024113251C2778357522 @default.
• W2024113251 hasConceptScore W2024113251C2779870107 @default.
• W2024113251 hasConceptScore W2024113251C5900021 @default.
• W2024113251 hasConceptScore W2024113251C77928131 @default.
• W2024113251 hasConceptScore W2024113251C79927612 @default.
• W2024113251 hasConceptScore W2024113251C95628711 @default.
• W2024113251 hasIssue "6" @default.
• W2024113251 hasLocation W20241132511 @default.
• W2024113251 hasOpenAccess W2024113251 @default.
• W2024113251 hasPrimaryLocation W20241132511 @default.
• W2024113251 hasRelatedWork W2009029744 @default.
• W2024113251 hasRelatedWork W2009936239 @default.
• W2024113251 hasRelatedWork W2018947826 @default.
• W2024113251 hasRelatedWork W2163755453 @default.
• W2024113251 hasRelatedWork W3004204397 @default.
• W2024113251 hasRelatedWork W3080339418 @default.

• next