FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2013430280> ?p ?o ?g. }

• W2013430280 endingPage "170" @default.
• W2013430280 startingPage "125" @default.
• W2013430280 abstract "The Mesozoic includes the later history of the New Zealand Geosyncline, the Rangitata Orogeny that ended the geosynclinal phase, superposing a new structural system, and the beginning of the transgression that followed. The main elements of the geosyncline, from west to east, are: (1) a foreland, metamorphosed and intruded by granite in a relatively high temperature/low pressure environment; (2) a geosynclinal margin or hinge-line, the median tectonic line of Landis and Coombs; (3) a western or marginal belt of geosynclinal sediments (Hokonui Facies) relatively fossiliferous, apparently deposited over the Pacific edge of the sial and now forming a western marginal syncline; (4) an abrupt facies junction marked by ultramafic intrusions and Permian volcanics, perhaps the early Mesozoic oceanic boundary of sialic crust; and (5) an eastern belt of relatively unfossiliferous deformed sediments of the greywacke suite (Torlesse Facies), metamorphosed in a high pressure environment, their lower parts to schist. The western or Hokonui zone records rapid and almost continuous marine sedimentation during the Triassic and Jurassic, with some brief local interruption during the Middle Jurassic. The eastern or Torlesse zone of thick quartzo–feldspathic greywackes and argillites, with some spilitic lavas, occupying a Pacificmargin trench, has proved difficult to interpret owing to structural complexity, lithological monotony and scarcity of fossils. The metamorphic boundaries vary in age in different places, and the known fossils show a nonrandom distribution in age and space, as if basins of rapid sedimentation migrated up and down its axis throughout Permian to Tithonian time, reacting to variable thermal gradients. The Rangitata Orogeny began with precursor movements in the Middle Jurassic but climaxed in the Lower Cretaceous. The orogeny led to the main metamorphism and folding of the geosyncline, long the East phases of granite intrusion in the foreland, and the torsion and rupture of the geosyncline along the transcurrent Alpine Fault. In the Aptian, basins within the New Zealand geosyncline received sediment still of geosynclinal facies, so that it remains uncertain whether deposition was locally continuous or whether the Cretaceous is everywhere unconformable on underlying rocks. Synorogenic breccias (pre-Campanian) locally overlie schist and foreland granites that have been dated isotopically as mid-Cretaceous, and thus point to rapid uplift and erosion. By the Macstrichtian, freshwater and marine sediments indicate peneplanation and dominantly chemical weathering. The Tasman Sea is first evident in the Cretaceous, and the Cretaceous transgression, continuing in the Tertiary, reduced the land to a changing archipelago. Early Mesozoic structures are consistent with a simple continent–ocean boundary and trench trending north-west, parallel to the Mesozoic Darwin Rise. The Cretaceous orogeny superposed north-east trending structures that have dominated later history; their northern parts face the Pacific and parallel a section of the East Pacific Rise, but their southern parts face the Tasman Sea in a kind of scissors or ‘anceps’ structure. The change from a single Pacific margin to the present anceps structure facing both the Pacific and Tasman is consistent with post-Jurassic development of the Tasman and other marginal ocean basins during the Cretaceous orogeny, which entailed considerable horizontal movements of the crust. New Zealand geology can be extrapolated onto the surrounding shallow sea-floors, underlain by subcontinental crust, using evidence from outlying islands, submarine geology, and geophysics. The speculative process of rationalizing Lower Mesozoic palaeogeography is made easier if it is assumed that the early Mesozoic arc, now sinuous, was originally straighter, and that the marginal ocean basins now interrupting its course developed during the Cretaceous deformation that led to its curvature." @default.
• W2013430280 created "2016-06-24" @default.
• W2013430280 creator A5002512199 @default.
• W2013430280 date "1969-12-01" @default.
• W2013430280 modified "2023-10-14" @default.
• W2013430280 title "The Mesozoic of New Zealand: Chapters in the history of the Circum-Pacific Mobile Belt" @default.
• W2013430280 cites W1965269128 @default.
• W2013430280 cites W1966741921 @default.
• W2013430280 cites W1978097237 @default.
• W2013430280 cites W1979023533 @default.
• W2013430280 cites W1980218846 @default.
• W2013430280 cites W1987922492 @default.
• W2013430280 cites W1993477842 @default.
• W2013430280 cites W2000092172 @default.
• W2013430280 cites W2001466654 @default.
• W2013430280 cites W2008413421 @default.
• W2013430280 cites W2011203266 @default.
• W2013430280 cites W2011799644 @default.
• W2013430280 cites W2028636945 @default.
• W2013430280 cites W2033462979 @default.
• W2013430280 cites W2035826387 @default.
• W2013430280 cites W2039331441 @default.
• W2013430280 cites W2040158180 @default.
• W2013430280 cites W2041379989 @default.
• W2013430280 cites W2041479912 @default.
• W2013430280 cites W2043546840 @default.
• W2013430280 cites W2044061895 @default.
• W2013430280 cites W2045110270 @default.
• W2013430280 cites W2056835610 @default.
• W2013430280 cites W2057128030 @default.
• W2013430280 cites W2064170118 @default.
• W2013430280 cites W2064576463 @default.
• W2013430280 cites W2066221588 @default.
• W2013430280 cites W2069648328 @default.
• W2013430280 cites W2069873041 @default.
• W2013430280 cites W2075122827 @default.
• W2013430280 cites W2077701949 @default.
• W2013430280 cites W2077941595 @default.
• W2013430280 cites W2078021456 @default.
• W2013430280 cites W2078205555 @default.
• W2013430280 cites W2079303087 @default.
• W2013430280 cites W2081453548 @default.
• W2013430280 cites W2087345889 @default.
• W2013430280 cites W2088287350 @default.
• W2013430280 cites W2089242468 @default.
• W2013430280 cites W2092451095 @default.
• W2013430280 cites W2094264745 @default.
• W2013430280 cites W2095164511 @default.
• W2013430280 cites W2095493942 @default.
• W2013430280 cites W2119390240 @default.
• W2013430280 cites W2128288920 @default.
• W2013430280 cites W2138058376 @default.
• W2013430280 cites W2146544818 @default.
• W2013430280 cites W2166192172 @default.
• W2013430280 cites W2169951910 @default.
• W2013430280 cites W2332444858 @default.
• W2013430280 cites W566811452 @default.
• W2013430280 doi "https://doi.org/10.1144/gsjgs.125.1.0125" @default.
• W2013430280 hasPublicationYear "1969" @default.
• W2013430280 type Work @default.
• W2013430280 sameAs 2013430280 @default.
• W2013430280 citedByCount "110" @default.
• W2013430280 countsByYear W20134302802012 @default.
• W2013430280 countsByYear W20134302802013 @default.
• W2013430280 countsByYear W20134302802015 @default.
• W2013430280 countsByYear W20134302802018 @default.
• W2013430280 countsByYear W20134302802019 @default.
• W2013430280 countsByYear W20134302802022 @default.
• W2013430280 crossrefType "journal-article" @default.
• W2013430280 hasAuthorship W2013430280A5002512199 @default.
• W2013430280 hasConcept C109007969 @default.
• W2013430280 hasConcept C127313418 @default.
• W2013430280 hasConcept C151730666 @default.
• W2013430280 hasConcept C202783661 @default.
• W2013430280 hasConceptScore W2013430280C109007969 @default.
• W2013430280 hasConceptScore W2013430280C127313418 @default.
• W2013430280 hasConceptScore W2013430280C151730666 @default.
• W2013430280 hasConceptScore W2013430280C202783661 @default.
• W2013430280 hasIssue "1-4" @default.
• W2013430280 hasLocation W20134302801 @default.
• W2013430280 hasOpenAccess W2013430280 @default.
• W2013430280 hasPrimaryLocation W20134302801 @default.
• W2013430280 hasRelatedWork W2046928950 @default.
• W2013430280 hasRelatedWork W2124551279 @default.
• W2013430280 hasRelatedWork W2314915748 @default.
• W2013430280 hasRelatedWork W2325222095 @default.
• W2013430280 hasRelatedWork W2472547998 @default.
• W2013430280 hasRelatedWork W2610605778 @default.
• W2013430280 hasRelatedWork W2808650887 @default.
• W2013430280 hasRelatedWork W2911869918 @default.
• W2013430280 hasRelatedWork W3084275675 @default.
• W2013430280 hasRelatedWork W2526090718 @default.
• W2013430280 hasVolume "125" @default.
• W2013430280 isParatext "false" @default.
• W2013430280 isRetracted "false" @default.
• W2013430280 magId "2013430280" @default.
• W2013430280 workType "article" @default.