Matches in SemOpenAlex for { <https://semopenalex.org/work/W3213463375> ?p ?o ?g. }
- W3213463375 endingPage "1780" @default.
- W3213463375 startingPage "1760" @default.
- W3213463375 abstract "Abstract Triassic strata in the Greater Barents Sea Basin are important records of geodynamic activity in the surrounding catchments and sediment transport in the Arctic basins. This study is the first attempt to investigate the evolution of these source areas through time. Our analysis of sediment budgets from subsurface data in the Greater Barents Sea Basin and application of the BQART approach to estimate catchment properties shows that (1) during the Lower Triassic, sediment supply was at its peak in the basin and comparable to that of the biggest modern-day river systems, which are supplied by tectonically active orogens; (2) the Middle Triassic sediment load was significantly lower but still comparable to that of the top 10 largest modern rivers; (3) during the Upper Triassic, sediment load increased again in the Carnian; and (4) there is a large mismatch (70%) between the modeled and estimated sediment load of the Carnian. These results are consistent with the Triassic Greater Barents Sea Basin succession being deposited under the influence of the largest volcanic event ever at the Permian-Triassic boundary (Siberian Traps) and concurrent with the climatic changes of the Carnian Pluvial Event and the final stages of the Northern Ural orogeny. They also provide a better understanding of geodynamic impacts on sedimentary systems and improve our knowledge of continental-scale sediment transport. Finally, the study demonstrates bypass of sediment from the Ural Mountains and West Siberia into the adjacent Arctic Sverdrup, Chukotka, and Alaska Basins in Late Carnian and Late Norian time." @default.
- W3213463375 created "2021-11-22" @default.
- W3213463375 creator A5016423186 @default.
- W3213463375 creator A5018891825 @default.
- W3213463375 creator A5020205429 @default.
- W3213463375 creator A5039063978 @default.
- W3213463375 creator A5041923783 @default.
- W3213463375 creator A5076235640 @default.
- W3213463375 date "2021-11-05" @default.
- W3213463375 modified "2023-09-26" @default.
- W3213463375 title "Linking sediment supply variations and tectonic evolution in deep time, source-to-sink systems—The Triassic Greater Barents Sea Basin" @default.
- W3213463375 cites W1480445398 @default.
- W3213463375 cites W1531499868 @default.
- W3213463375 cites W1559850468 @default.
- W3213463375 cites W1576968033 @default.
- W3213463375 cites W1624599660 @default.
- W3213463375 cites W1625153604 @default.
- W3213463375 cites W1711607069 @default.
- W3213463375 cites W1770113505 @default.
- W3213463375 cites W1922855605 @default.
- W3213463375 cites W1967424909 @default.
- W3213463375 cites W1975503180 @default.
- W3213463375 cites W1984681559 @default.
- W3213463375 cites W1985027176 @default.
- W3213463375 cites W1985146991 @default.
- W3213463375 cites W1985698294 @default.
- W3213463375 cites W1991323502 @default.
- W3213463375 cites W2001061209 @default.
- W3213463375 cites W2019695435 @default.
- W3213463375 cites W2021800930 @default.
- W3213463375 cites W2038178933 @default.
- W3213463375 cites W2044430153 @default.
- W3213463375 cites W2046057274 @default.
- W3213463375 cites W2050612668 @default.
- W3213463375 cites W2070070314 @default.
- W3213463375 cites W2070370343 @default.
- W3213463375 cites W2078542443 @default.
- W3213463375 cites W2080071327 @default.
- W3213463375 cites W2080458803 @default.
- W3213463375 cites W2080487384 @default.
- W3213463375 cites W2089087243 @default.
- W3213463375 cites W2095483935 @default.
- W3213463375 cites W2102401605 @default.
- W3213463375 cites W2102900399 @default.
- W3213463375 cites W2108037464 @default.
- W3213463375 cites W2115497827 @default.
- W3213463375 cites W2119695127 @default.
- W3213463375 cites W2123399224 @default.
- W3213463375 cites W2123618140 @default.
- W3213463375 cites W2123823757 @default.
- W3213463375 cites W2141199096 @default.
- W3213463375 cites W2147204436 @default.
- W3213463375 cites W2158018179 @default.
- W3213463375 cites W2159884432 @default.
- W3213463375 cites W2162334444 @default.
- W3213463375 cites W2254863569 @default.
- W3213463375 cites W2294993874 @default.
- W3213463375 cites W2309082002 @default.
- W3213463375 cites W2316816482 @default.
- W3213463375 cites W2326460780 @default.
- W3213463375 cites W2336825809 @default.
- W3213463375 cites W2340659542 @default.
- W3213463375 cites W2499462499 @default.
- W3213463375 cites W2520789427 @default.
- W3213463375 cites W2529697602 @default.
- W3213463375 cites W2561539043 @default.
- W3213463375 cites W2727062246 @default.
- W3213463375 cites W2747785884 @default.
- W3213463375 cites W2760568025 @default.
- W3213463375 cites W2761552066 @default.
- W3213463375 cites W2788885160 @default.
- W3213463375 cites W2790977306 @default.
- W3213463375 cites W2802480577 @default.
- W3213463375 cites W2883509550 @default.
- W3213463375 cites W2893022262 @default.
- W3213463375 cites W2902113630 @default.
- W3213463375 cites W2939470080 @default.
- W3213463375 cites W2940815216 @default.
- W3213463375 cites W2954377702 @default.
- W3213463375 cites W2956268941 @default.
- W3213463375 cites W2971935503 @default.
- W3213463375 cites W2984873492 @default.
- W3213463375 cites W2996057996 @default.
- W3213463375 cites W3037120285 @default.
- W3213463375 cites W3102411056 @default.
- W3213463375 cites W3113053312 @default.
- W3213463375 cites W3143738360 @default.
- W3213463375 doi "https://doi.org/10.1130/b36090.1" @default.
- W3213463375 hasPublicationYear "2021" @default.
- W3213463375 type Work @default.
- W3213463375 sameAs 3213463375 @default.
- W3213463375 citedByCount "6" @default.
- W3213463375 countsByYear W32134633752022 @default.
- W3213463375 countsByYear W32134633752023 @default.
- W3213463375 crossrefType "journal-article" @default.
- W3213463375 hasAuthorship W3213463375A5016423186 @default.
- W3213463375 hasAuthorship W3213463375A5018891825 @default.
- W3213463375 hasAuthorship W3213463375A5020205429 @default.