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• W2894968742 endingPage "1382" @default.
• W2894968742 startingPage "1357" @default.
• W2894968742 abstract "Abstract A new stratigraphic model and estimated sedimentation rates of the western Amundsen Basin, Arctic Ocean, are presented based on multichannel seismic reflection data, seismic refraction data, magnetic data, and integrated with the sedimentary sequence from the central Arctic Ocean, obtained during the Arctic Coring Expedition. This places new constraints on the postbreakup Cenozoic depositional history of the basin, the adjacent Lomonosov Ridge, and improves the understanding of the tectonic, climatic, and oceanographic conditions in the central Arctic region. Four distinct phases of basin development are proposed. During the Paleocene‐mid‐Oligocene, high sedimentation rates are linked to terrestrial input and increased pelagic deposition in a restricted basin. Deposition of sedimentary wedges and mass transport into marginal depocenters reflect a period of tectonic instability linked to compression associated with the Eurekan Orogeny in the Arctic. During the late Oligocene‐early Miocene, widespread passive infill associated with hemipelagic deposition reflects a phase of limited tectonism, most likely in a freshwater estuarine setting. During the middle Miocene, mounded sedimentary buildups along the Lomonosov Ridge suggest the onset of geostrophic bottom currents that likely formed in response to a deepening and widening of the Fram Strait beginning around 18 Ma. In contrast, the Plio‐Pleistocene stage is characterized by erosional features such as scarps and channels adjacent to levee accumulations, indicative of a change to a higher‐energy environment. These deposits are suggested to be partly associated with dense shelf water‐mass plumes driven by supercooling and brine formation over the northern Greenland continental shelf." @default.
• W2894968742 created "2018-10-12" @default.
• W2894968742 creator A5026011171 @default.
• W2894968742 creator A5037667791 @default.
• W2894968742 creator A5048002445 @default.
• W2894968742 creator A5090013426 @default.
• W2894968742 date "2018-12-01" @default.
• W2894968742 modified "2023-09-25" @default.
• W2894968742 title "Depositional Evolution of the Western Amundsen Basin, Arctic Ocean: Paleoceanographic and Tectonic Implications" @default.
• W2894968742 cites W1493983059 @default.
• W2894968742 cites W1553859745 @default.
• W2894968742 cites W1561916422 @default.
• W2894968742 cites W1568327687 @default.
• W2894968742 cites W1580946720 @default.
• W2894968742 cites W1586314053 @default.
• W2894968742 cites W1587200101 @default.
• W2894968742 cites W1591602797 @default.
• W2894968742 cites W1868181626 @default.
• W2894968742 cites W1876939180 @default.
• W2894968742 cites W1918626762 @default.
• W2894968742 cites W1964070187 @default.
• W2894968742 cites W1965078451 @default.
• W2894968742 cites W1967562941 @default.
• W2894968742 cites W1971228562 @default.
• W2894968742 cites W1971441458 @default.
• W2894968742 cites W1971456699 @default.
• W2894968742 cites W1976217903 @default.
• W2894968742 cites W1976589119 @default.
• W2894968742 cites W1976781881 @default.
• W2894968742 cites W1976868752 @default.
• W2894968742 cites W1980090525 @default.
• W2894968742 cites W1982610910 @default.
• W2894968742 cites W1983743729 @default.
• W2894968742 cites W1988178310 @default.
• W2894968742 cites W1997604005 @default.
• W2894968742 cites W2000945942 @default.
• W2894968742 cites W2003833035 @default.
• W2894968742 cites W2004625961 @default.
• W2894968742 cites W2005463144 @default.
• W2894968742 cites W2016138414 @default.
• W2894968742 cites W2023150357 @default.
• W2894968742 cites W2025677918 @default.
• W2894968742 cites W2027735940 @default.
• W2894968742 cites W2028715359 @default.
• W2894968742 cites W2032652270 @default.
• W2894968742 cites W2034753142 @default.
• W2894968742 cites W2036279237 @default.
• W2894968742 cites W2036791057 @default.
• W2894968742 cites W2047842264 @default.
• W2894968742 cites W2051300487 @default.
• W2894968742 cites W2054368483 @default.
• W2894968742 cites W2055442076 @default.
• W2894968742 cites W2059950589 @default.
• W2894968742 cites W2063155650 @default.
• W2894968742 cites W2068551825 @default.
• W2894968742 cites W2073992599 @default.
• W2894968742 cites W2074303350 @default.
• W2894968742 cites W2080743915 @default.
• W2894968742 cites W2081937256 @default.
• W2894968742 cites W2084421054 @default.
• W2894968742 cites W2084962150 @default.
• W2894968742 cites W2085898986 @default.
• W2894968742 cites W2086259978 @default.
• W2894968742 cites W2089951841 @default.
• W2894968742 cites W2090180218 @default.
• W2894968742 cites W2092819194 @default.
• W2894968742 cites W2093318992 @default.
• W2894968742 cites W2094423512 @default.
• W2894968742 cites W2096557357 @default.
• W2894968742 cites W2101510715 @default.
• W2894968742 cites W2102234201 @default.
• W2894968742 cites W2104308583 @default.
• W2894968742 cites W2108316127 @default.
• W2894968742 cites W2113116836 @default.
• W2894968742 cites W2114830030 @default.
• W2894968742 cites W2115421030 @default.
• W2894968742 cites W2115575384 @default.
• W2894968742 cites W2115757528 @default.
• W2894968742 cites W2123445693 @default.
• W2894968742 cites W2123605377 @default.
• W2894968742 cites W2123741232 @default.
• W2894968742 cites W2124365512 @default.
• W2894968742 cites W2124977786 @default.
• W2894968742 cites W2130833734 @default.
• W2894968742 cites W2132360578 @default.
• W2894968742 cites W2132993231 @default.
• W2894968742 cites W2134685525 @default.
• W2894968742 cites W2135552548 @default.
• W2894968742 cites W2138511808 @default.
• W2894968742 cites W2138793715 @default.
• W2894968742 cites W2143656788 @default.
• W2894968742 cites W2145619152 @default.
• W2894968742 cites W2146995937 @default.
• W2894968742 cites W2153795153 @default.
• W2894968742 cites W2164711780 @default.
• W2894968742 cites W2167600455 @default.
• W2894968742 cites W2168959606 @default.
• W2894968742 cites W2258550461 @default.

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