FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2805839897> ?p ?o ?g. }

• W2805839897 endingPage "76" @default.
• W2805839897 startingPage "45" @default.
• W2805839897 abstract "The Proterozoic to early Palaeozoic Pearya Terrane at the northern margin of Ellesmere Island is composed of several crustal fragments and is built up by five tectono-stratigraphic successions. This study focusses on parts of Successions 1–3 and related intrusions, including the Cape Fanshawe Martin Pluton (CFMP). Petrographical, geochemical, and geochronological data reveal a protracted, complex with in parts different geological history of these Pearya segments. Succession 1 is dominated by c. 1000–950 Ma old orthogneisses, which are part of a Stenian-Tonian magmatic arc. The arc was later intruded by mafic dykes probably related to the opening of the Iapetus Ocean. Post-tectonic leucogranite bodies were emplaced at c. 360 Ma. Succession 2 comprises Neoproterozoic to early Ordovician clastic sediments. It is subdivided in different units, for which the detrital zircon U–Pb ages reveal different source areas. Unit W with main ages at c. 1800–1050 Ma, and a youngest population at 1067 Ma, older than the biostratigraphic maximum depositional age of <600 Ma, was sourced from a continent that experienced the Grenvillian Orogeny. Unit A with ages mainly in the range of 1800–1000 Ma, and a maximum depositional age at 920 Ma, and Unit M2 with numerous age peaks between 2940 and 570 Ma and the maximum depositional age at 572 Ma received detritus from both the continental source and the Stenian-Tonian magmatic arc, and Unit M2 additionally from a Timanian island arc. Unit A was intruded by A-type granites at c. 485 Ma, which were migmatised at 454 Ma. The ultramafic to felsic CFMP at the coast of the Arctic Ocean northeast of Unit A comprises charnockites intruded at 458–456 Ma and granites emplaced at 441 Ma. The boundary with Unit A is probably tectonic. Succession 3 includes volcaniclastic sediments with detrital zircon ages of 621–492 Ma peaking at 573 Ma, which are dominantly sourced from an intra-oceanic Timanian island arc, and two genetically different igneous suites, an ophiolitic E-MORB suite of unknown age and a subduction-related suite formed at c. 500–470 Ma (Thores Suite). Both suites were juxtaposed during the M'Clintock Orogeny at c. 470–454 Ma. After the probably stepwise accretion of Pearya blocks to the northern margin of Laurentia during the Devonian to early Carboniferous Ellesmerian Orogeny, the Pearya Terrane was affected by thermal events during the Mesozoic, such as the intrusion of Triassic/Jurassic alkali-basaltic dykes and the Cretaceous magmatism of the High Arctic Large Igneous Province (HALIP). This study supports previous models that the Pearya Terrane is composed of crustal fragments, which are exotic to the Canadian Arctic margin." @default.
• W2805839897 created "2018-06-13" @default.
• W2805839897 creator A5007022117 @default.
• W2805839897 creator A5009092598 @default.
• W2805839897 creator A5015098753 @default.
• W2805839897 creator A5030081327 @default.
• W2805839897 creator A5039858005 @default.
• W2805839897 creator A5046983335 @default.
• W2805839897 creator A5055313905 @default.
• W2805839897 creator A5059748086 @default.
• W2805839897 date "2018-10-01" @default.
• W2805839897 modified "2023-10-10" @default.
• W2805839897 title "Proterozoic to Cretaceous evolution of the western and central Pearya Terrane (Canadian High Arctic)" @default.
• W2805839897 cites W1514994218 @default.
• W2805839897 cites W1760780020 @default.
• W2805839897 cites W1964018887 @default.
• W2805839897 cites W1964909252 @default.
• W2805839897 cites W1967080607 @default.
• W2805839897 cites W1971685925 @default.
• W2805839897 cites W1974155292 @default.
• W2805839897 cites W1977179325 @default.
• W2805839897 cites W1977650828 @default.
• W2805839897 cites W1982739504 @default.
• W2805839897 cites W1986672338 @default.
• W2805839897 cites W1989915748 @default.
• W2805839897 cites W1992403626 @default.
• W2805839897 cites W1993774984 @default.
• W2805839897 cites W1994793643 @default.
• W2805839897 cites W1997018906 @default.
• W2805839897 cites W1997796597 @default.
• W2805839897 cites W1999448338 @default.
• W2805839897 cites W2000403740 @default.
• W2805839897 cites W2000821124 @default.
• W2805839897 cites W2002094001 @default.
• W2805839897 cites W2006789003 @default.
• W2805839897 cites W2008373173 @default.
• W2805839897 cites W2012437090 @default.
• W2805839897 cites W2015057002 @default.
• W2805839897 cites W2016565796 @default.
• W2805839897 cites W2019034794 @default.
• W2805839897 cites W2020139762 @default.
• W2805839897 cites W2020148154 @default.
• W2805839897 cites W2021754290 @default.
• W2805839897 cites W2027807145 @default.
• W2805839897 cites W2028904790 @default.
• W2805839897 cites W2031814274 @default.
• W2805839897 cites W2034608326 @default.
• W2805839897 cites W2035048900 @default.
• W2805839897 cites W2036702727 @default.
• W2805839897 cites W2042491214 @default.
• W2805839897 cites W2046153938 @default.
• W2805839897 cites W2046388680 @default.
• W2805839897 cites W2047290022 @default.
• W2805839897 cites W2048240400 @default.
• W2805839897 cites W2055388906 @default.
• W2805839897 cites W2055939594 @default.
• W2805839897 cites W2059356468 @default.
• W2805839897 cites W2061458258 @default.
• W2805839897 cites W2061651505 @default.
• W2805839897 cites W2071420241 @default.
• W2805839897 cites W2074008199 @default.
• W2805839897 cites W2075683682 @default.
• W2805839897 cites W2080743915 @default.
• W2805839897 cites W2081675936 @default.
• W2805839897 cites W2084362152 @default.
• W2805839897 cites W2088657878 @default.
• W2805839897 cites W2093208298 @default.
• W2805839897 cites W2093816695 @default.
• W2805839897 cites W2102045200 @default.
• W2805839897 cites W2102311915 @default.
• W2805839897 cites W2102413566 @default.
• W2805839897 cites W2103108238 @default.
• W2805839897 cites W2108971421 @default.
• W2805839897 cites W2111391921 @default.
• W2805839897 cites W2112435406 @default.
• W2805839897 cites W2115421030 @default.
• W2805839897 cites W2118269966 @default.
• W2805839897 cites W2118355280 @default.
• W2805839897 cites W2122213004 @default.
• W2805839897 cites W2133535793 @default.
• W2805839897 cites W2134581078 @default.
• W2805839897 cites W2134638205 @default.
• W2805839897 cites W2136627811 @default.
• W2805839897 cites W2137335623 @default.
• W2805839897 cites W2138522501 @default.
• W2805839897 cites W2138912540 @default.
• W2805839897 cites W2141421348 @default.
• W2805839897 cites W2141819832 @default.
• W2805839897 cites W2148151176 @default.
• W2805839897 cites W2151570992 @default.
• W2805839897 cites W2153795153 @default.
• W2805839897 cites W2158468162 @default.
• W2805839897 cites W2159669043 @default.
• W2805839897 cites W2160622562 @default.
• W2805839897 cites W2162490868 @default.
• W2805839897 cites W2164486758 @default.
• W2805839897 cites W2169462252 @default.
• W2805839897 cites W2244750437 @default.

• next