FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2191523488> ?p ?o ?g. }

• W2191523488 endingPage "279" @default.
• W2191523488 startingPage "263" @default.
• W2191523488 abstract "The Amundsen Sea Embayment of West Antarctica is of particular interest as it provides critical geological boundary conditions in better understanding the dynamic behavior of the West Antarctic Ice Sheet, which is undergoing rapid ice loss in the Amundsen Sea sector. One of the highly debated hypothesis is whether this region has been affected by the West Antarctic Rift System, which is one of the largest in the world and the dominating tectonic feature in West Antarctica. Previous geophysical studies suggested an eastward continuation of this rift system into the Amundsen Sea Embayment. This geophysical study of the Amundsen Sea Embayment presents a compilation of data collected during two RV Polarstern expeditions in the Amundsen Sea Embayment of West Antarctica in 2006 and 2010. Bathymetry and satellite-derived gravity data of the Amundsen Sea Embayment complete the dataset. Our 3-D gravity and magnetic models of the lithospheric architecture and development of this Pacific margin improve previous interpretations from 2-D models of the region. The crust-mantle boundary beneath the continental rise and shelf is between 14 and 29 km deep. The imaged basement structure can be related to rift basins within the Amundsen Sea Embayment, some of which can be interpreted as products of the Cretaceous rift and break-up phase and some as products of later propagation of the West Antarctic Rift System into the region. An estimate of the flexural rigidity of the lithosphere reveals a thin elastic thickness in the eastern embayment which increases towards the west. The results are comparable to estimates in other rift systems such as the Basin and Range province or the East African Rift. Based on these results, we infer an arm of the West Antarctic Rift System is superposed on a distributed Cretaceous rift province in the Amundsen Sea Embayment. Finally, the embayment was affected by magmatism from discrete sources along the Pacific margin of West Antarctica in the Cenozoic." @default.
• W2191523488 created "2016-06-24" @default.
• W2191523488 creator A5016637147 @default.
• W2191523488 creator A5059748086 @default.
• W2191523488 creator A5080536004 @default.
• W2191523488 creator A5084234210 @default.
• W2191523488 date "2015-09-22" @default.
• W2191523488 modified "2023-10-14" @default.
• W2191523488 title "Rift processes and crustal structure of the Amundsen Sea Embayment, West Antarctica, from 3D potential field modelling" @default.
• W2191523488 cites W1549953565 @default.
• W2191523488 cites W1566500989 @default.
• W2191523488 cites W1582317163 @default.
• W2191523488 cites W1674953531 @default.
• W2191523488 cites W1893521577 @default.
• W2191523488 cites W1953685587 @default.
• W2191523488 cites W1972758960 @default.
• W2191523488 cites W1979281560 @default.
• W2191523488 cites W1980663642 @default.
• W2191523488 cites W1990365623 @default.
• W2191523488 cites W1994323983 @default.
• W2191523488 cites W2003991414 @default.
• W2191523488 cites W2010043692 @default.
• W2191523488 cites W2011667849 @default.
• W2191523488 cites W2011970992 @default.
• W2191523488 cites W2020093204 @default.
• W2191523488 cites W2025865560 @default.
• W2191523488 cites W2032366045 @default.
• W2191523488 cites W2033251889 @default.
• W2191523488 cites W2037906608 @default.
• W2191523488 cites W2039576656 @default.
• W2191523488 cites W2044612552 @default.
• W2191523488 cites W2052897915 @default.
• W2191523488 cites W2056848092 @default.
• W2191523488 cites W2058410188 @default.
• W2191523488 cites W2063937978 @default.
• W2191523488 cites W2067269796 @default.
• W2191523488 cites W2071244002 @default.
• W2191523488 cites W2082525917 @default.
• W2191523488 cites W2088528402 @default.
• W2191523488 cites W2092115534 @default.
• W2191523488 cites W2095036489 @default.
• W2191523488 cites W2095374616 @default.
• W2191523488 cites W2103396560 @default.
• W2191523488 cites W2106888819 @default.
• W2191523488 cites W2112167095 @default.
• W2191523488 cites W2116615769 @default.
• W2191523488 cites W2120714568 @default.
• W2191523488 cites W2132239511 @default.
• W2191523488 cites W2132684433 @default.
• W2191523488 cites W2137448996 @default.
• W2191523488 cites W2137978791 @default.
• W2191523488 cites W2145913308 @default.
• W2191523488 cites W2152297531 @default.
• W2191523488 cites W2153408818 @default.
• W2191523488 cites W2156752261 @default.
• W2191523488 cites W2159526919 @default.
• W2191523488 cites W2160868026 @default.
• W2191523488 cites W2166560736 @default.
• W2191523488 cites W2166666752 @default.
• W2191523488 cites W2167002594 @default.
• W2191523488 cites W2169627376 @default.
• W2191523488 cites W2482753456 @default.
• W2191523488 cites W3023268160 @default.
• W2191523488 cites W4241286055 @default.
• W2191523488 doi "https://doi.org/10.1007/s11001-015-9261-0" @default.
• W2191523488 hasPublicationYear "2015" @default.
• W2191523488 type Work @default.
• W2191523488 sameAs 2191523488 @default.
• W2191523488 citedByCount "8" @default.
• W2191523488 countsByYear W21915234882016 @default.
• W2191523488 countsByYear W21915234882017 @default.
• W2191523488 countsByYear W21915234882018 @default.
• W2191523488 countsByYear W21915234882019 @default.
• W2191523488 countsByYear W21915234882020 @default.
• W2191523488 countsByYear W21915234882022 @default.
• W2191523488 crossrefType "journal-article" @default.
• W2191523488 hasAuthorship W2191523488A5016637147 @default.
• W2191523488 hasAuthorship W2191523488A5059748086 @default.
• W2191523488 hasAuthorship W2191523488A5080536004 @default.
• W2191523488 hasAuthorship W2191523488A5084234210 @default.
• W2191523488 hasBestOaLocation W21915234882 @default.
• W2191523488 hasConcept C111368507 @default.
• W2191523488 hasConcept C127313418 @default.
• W2191523488 hasConcept C136894858 @default.
• W2191523488 hasConcept C151730666 @default.
• W2191523488 hasConcept C16942324 @default.
• W2191523488 hasConcept C174943157 @default.
• W2191523488 hasConcept C197435368 @default.
• W2191523488 hasConcept C201867031 @default.
• W2191523488 hasConcept C2776698055 @default.
• W2191523488 hasConcept C2780223605 @default.
• W2191523488 hasConcept C50682988 @default.
• W2191523488 hasConcept C67236022 @default.
• W2191523488 hasConcept C77928131 @default.
• W2191523488 hasConcept C8058405 @default.
• W2191523488 hasConceptScore W2191523488C111368507 @default.
• W2191523488 hasConceptScore W2191523488C127313418 @default.
• W2191523488 hasConceptScore W2191523488C136894858 @default.

• next