FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W1567865327> ?p ?o ?g. }

• W1567865327 endingPage "623" @default.
• W1567865327 startingPage "603" @default.
• W1567865327 abstract "Abstract Cambrian orogenesis (550–490 Ma) in the Lambert Province of the southern Prince Charles Mountains resulted in three successive stages of deformation. The earliest of these deformations resulted in the development of a layer‐parallel foliation (S1) that was folded into macro‐scale recumbent folds (F2). Subsequent deformation buckled the rocks into long‐wavelength ( c . 20 km), SW‐ to NW‐trending antiformal closures (F3) mostly separated from each other by west to SW trending, steeply dipping, high‐strain zones. Metapelitic rocks from the region are divisible into two compositional types: a high‐Al, ‐Fe and ‐K type and a high‐Mg, ‐Ca and ‐Na type. In rocks of both composition, relic staurolite preceded the formation of upper amphibolite facies garnet + biotite + sillimanite ± muscovite mineral assemblages that record peak pressures and temperatures of c. 650–700 °C and 6–7 kbar. Subsequent decompression of c. 3 kbar is implied from texturally late plagioclase and a reduction in the modal abundance of garnet in the high‐Al, ‐Fe and ‐K metapelites, and from texturally late cordierite in the more magnesium rocks. This clockwise P–T–t path, with prograde heating followed by rapid decompression, is: (i) equivalent to that recorded in the same‐aged rocks at Prydz Bay located 600 km to the north, and (ii) similar to the modelled response of the crust to thickening following continent–continent collision. These results indicate that large areas of East Antarctica were thickened and rapidly exhumed, probably in response to collisional orogenesis during the Early Cambrian. This supports the inference that Early Cambrian orogenesis in the Prydz Bay–Prince Charles Mountains region of East Antarctica marks one of the fundamental lithospheric boundaries within Gondwana." @default.
• W1567865327 created "2016-06-24" @default.
• W1567865327 creator A5040379333 @default.
• W1567865327 creator A5083528925 @default.
• W1567865327 date "2005-08-25" @default.
• W1567865327 modified "2023-10-13" @default.
• W1567865327 title "Early Cambrian crustal shortening and a clockwise P-T-t path from the southern Prince Charles Mountains, East Antarctica: implications for the formation of Gondwana" @default.
• W1567865327 cites W1544416913 @default.
• W1567865327 cites W1564250183 @default.
• W1567865327 cites W1830358639 @default.
• W1567865327 cites W1968704350 @default.
• W1567865327 cites W1971356165 @default.
• W1567865327 cites W1972909865 @default.
• W1567865327 cites W1973281201 @default.
• W1567865327 cites W1979638106 @default.
• W1567865327 cites W1985160890 @default.
• W1567865327 cites W1991914664 @default.
• W1567865327 cites W1994792156 @default.
• W1567865327 cites W1998977948 @default.
• W1567865327 cites W2002922526 @default.
• W1567865327 cites W2007557466 @default.
• W1567865327 cites W2007782740 @default.
• W1567865327 cites W2010898859 @default.
• W1567865327 cites W2014934612 @default.
• W1567865327 cites W2016529524 @default.
• W1567865327 cites W2034472228 @default.
• W1567865327 cites W2036121092 @default.
• W1567865327 cites W2045287269 @default.
• W1567865327 cites W2046223350 @default.
• W1567865327 cites W2046362351 @default.
• W1567865327 cites W2049486454 @default.
• W1567865327 cites W2051658565 @default.
• W1567865327 cites W2052069498 @default.
• W1567865327 cites W2052310716 @default.
• W1567865327 cites W2054654291 @default.
• W1567865327 cites W2058741861 @default.
• W1567865327 cites W2060202408 @default.
• W1567865327 cites W2063176235 @default.
• W1567865327 cites W2063589322 @default.
• W1567865327 cites W2067996674 @default.
• W1567865327 cites W2069865961 @default.
• W1567865327 cites W2075026240 @default.
• W1567865327 cites W2078992461 @default.
• W1567865327 cites W2080506700 @default.
• W1567865327 cites W2080997920 @default.
• W1567865327 cites W2081069181 @default.
• W1567865327 cites W2081760487 @default.
• W1567865327 cites W2084854595 @default.
• W1567865327 cites W2086513665 @default.
• W1567865327 cites W2089328511 @default.
• W1567865327 cites W2089514169 @default.
• W1567865327 cites W2094414093 @default.
• W1567865327 cites W2095430403 @default.
• W1567865327 cites W2109473548 @default.
• W1567865327 cites W2125181521 @default.
• W1567865327 cites W2127494192 @default.
• W1567865327 cites W2129161355 @default.
• W1567865327 cites W2130579490 @default.
• W1567865327 cites W2132593853 @default.
• W1567865327 cites W2135183977 @default.
• W1567865327 cites W2137179628 @default.
• W1567865327 cites W2141789556 @default.
• W1567865327 cites W2153263119 @default.
• W1567865327 cites W2153315663 @default.
• W1567865327 cites W2419450098 @default.
• W1567865327 cites W2519418821 @default.
• W1567865327 cites W2916634178 @default.
• W1567865327 cites W3085608497 @default.
• W1567865327 cites W4231872186 @default.
• W1567865327 doi "https://doi.org/10.1111/j.1525-1314.2005.00598.x" @default.
• W1567865327 hasPublicationYear "2005" @default.
• W1567865327 type Work @default.
• W1567865327 sameAs 1567865327 @default.
• W1567865327 citedByCount "44" @default.
• W1567865327 countsByYear W15678653272013 @default.
• W1567865327 countsByYear W15678653272014 @default.
• W1567865327 countsByYear W15678653272015 @default.
• W1567865327 countsByYear W15678653272016 @default.
• W1567865327 countsByYear W15678653272017 @default.
• W1567865327 countsByYear W15678653272019 @default.
• W1567865327 countsByYear W15678653272020 @default.
• W1567865327 countsByYear W15678653272021 @default.
• W1567865327 countsByYear W15678653272022 @default.
• W1567865327 countsByYear W15678653272023 @default.
• W1567865327 crossrefType "journal-article" @default.
• W1567865327 hasAuthorship W1567865327A5040379333 @default.
• W1567865327 hasAuthorship W1567865327A5083528925 @default.
• W1567865327 hasConcept C127313418 @default.
• W1567865327 hasConcept C151730666 @default.
• W1567865327 hasConcept C17409809 @default.
• W1567865327 hasConcept C2776698055 @default.
• W1567865327 hasConcept C2777229588 @default.
• W1567865327 hasConcept C2777241186 @default.
• W1567865327 hasConcept C2779870107 @default.
• W1567865327 hasConcept C2781148125 @default.
• W1567865327 hasConcept C77928131 @default.
• W1567865327 hasConceptScore W1567865327C127313418 @default.
• W1567865327 hasConceptScore W1567865327C151730666 @default.

• next