FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2567207823> ?p ?o ?g. }

• W2567207823 endingPage "114" @default.
• W2567207823 startingPage "99" @default.
• W2567207823 abstract "This study examines the velocity structure of Makarov Basin and the adjacent Alpha Ridge to determine the tectonic origins of these features and link them to the larger Amerasia Basin. Seismic data from sonobuoys distributed along a 650 km-long line extending from Alpha Ridge and across Makarov Basin to the Lomonosov Ridge were analyzed for this purpose. Forward modelling of traveltimes, supported by coincident multi-channel seismic reflection and shipborne gravity data, were used to determine the P-wave velocity structure along the line. The sedimentary cover averages 0.5 km-thick on Alpha Ridge and 1.9 km-thick in Makarov Basin, but reaches up to 5 km-thick at the base of Lomonosov Ridge. Velocities in the sedimentary section range from 1.6 to 4.3 km s− 1. As suggested by relatively high velocities, interbedded volcaniclastic or volcanic rock may occur in the deep sedimentary section. The shallow basement of Alpha Ridge (3.3 to 3.6 km s− 1) is characterized by semi-continuous high amplitude reflections and is interpreted as volcanic rock possibly intercalated with sedimentary rock. Velocities do not vary significantly in the upper and mid-crustal layers between Alpha Ridge and Makarov Basin. Total crustal thickness decreases from 27 km beneath Alpha Ridge to 5 km-thick in Makarov Basin then thickens to > 20 km over a short distance as part of Lomonosov Ridge. The crustal structure of Alpha Ridge is consistent with previous studies suggesting that the Alpha-Mendeleev ridge complex is part of a large igneous province (LIP) with thick igneous crust. The lack of change in crustal velocities between Alpha Ridge and Makarov Basin suggests that the basin, at least partly, either formed during or was influenced by LIP-related magmatism. The rapid transition of crustal thicknesses from Makarov Basin to Lomonosov Ridge supports the interpretation that this section of the ridge is a transform margin." @default.
• W2567207823 created "2017-01-06" @default.
• W2567207823 creator A5009457889 @default.
• W2567207823 creator A5015477254 @default.
• W2567207823 creator A5026011171 @default.
• W2567207823 date "2017-01-01" @default.
• W2567207823 modified "2023-10-18" @default.
• W2567207823 title "The sedimentary and crustal velocity structure of Makarov Basin and adjacent Alpha Ridge" @default.
• W2567207823 cites W1554512646 @default.
• W2567207823 cites W1580946720 @default.
• W2567207823 cites W1586314053 @default.
• W2567207823 cites W1918626762 @default.
• W2567207823 cites W1964070187 @default.
• W2567207823 cites W1968882799 @default.
• W2567207823 cites W1969599221 @default.
• W2567207823 cites W1976664390 @default.
• W2567207823 cites W1983292848 @default.
• W2567207823 cites W1985722522 @default.
• W2567207823 cites W1989915748 @default.
• W2567207823 cites W1991128154 @default.
• W2567207823 cites W1991856657 @default.
• W2567207823 cites W1992350939 @default.
• W2567207823 cites W1996925758 @default.
• W2567207823 cites W2000945942 @default.
• W2567207823 cites W2003399972 @default.
• W2567207823 cites W2006145696 @default.
• W2567207823 cites W2011848086 @default.
• W2567207823 cites W2011863281 @default.
• W2567207823 cites W2015432225 @default.
• W2567207823 cites W2015628445 @default.
• W2567207823 cites W2019549339 @default.
• W2567207823 cites W2021754290 @default.
• W2567207823 cites W2022577453 @default.
• W2567207823 cites W2023923449 @default.
• W2567207823 cites W2031678817 @default.
• W2567207823 cites W2034839657 @default.
• W2567207823 cites W2035564636 @default.
• W2567207823 cites W2043179375 @default.
• W2567207823 cites W2046821357 @default.
• W2567207823 cites W2047501871 @default.
• W2567207823 cites W2049595169 @default.
• W2567207823 cites W2066112144 @default.
• W2567207823 cites W2067363266 @default.
• W2567207823 cites W2068551825 @default.
• W2567207823 cites W2073497282 @default.
• W2567207823 cites W2080743915 @default.
• W2567207823 cites W2086259978 @default.
• W2567207823 cites W2091207439 @default.
• W2567207823 cites W2091579300 @default.
• W2567207823 cites W2093318992 @default.
• W2567207823 cites W2094457132 @default.
• W2567207823 cites W2095815346 @default.
• W2567207823 cites W2096962492 @default.
• W2567207823 cites W2097213524 @default.
• W2567207823 cites W2098679480 @default.
• W2567207823 cites W2103510367 @default.
• W2567207823 cites W2114660893 @default.
• W2567207823 cites W2115421030 @default.
• W2567207823 cites W2121064335 @default.
• W2567207823 cites W2123741232 @default.
• W2567207823 cites W2127080669 @default.
• W2567207823 cites W2130317456 @default.
• W2567207823 cites W2134728822 @default.
• W2567207823 cites W2141739359 @default.
• W2567207823 cites W2142857120 @default.
• W2567207823 cites W2144542802 @default.
• W2567207823 cites W2145896048 @default.
• W2567207823 cites W2159584112 @default.
• W2567207823 cites W2160744589 @default.
• W2567207823 cites W2168959606 @default.
• W2567207823 cites W2172364918 @default.
• W2567207823 cites W2257009632 @default.
• W2567207823 cites W2278369218 @default.
• W2567207823 cites W2278931765 @default.
• W2567207823 cites W2518606999 @default.
• W2567207823 cites W4230686011 @default.
• W2567207823 cites W4232396042 @default.
• W2567207823 cites W4384637648 @default.
• W2567207823 doi "https://doi.org/10.1016/j.tecto.2016.12.026" @default.
• W2567207823 hasPublicationYear "2017" @default.
• W2567207823 type Work @default.
• W2567207823 sameAs 2567207823 @default.
• W2567207823 citedByCount "19" @default.
• W2567207823 countsByYear W25672078232017 @default.
• W2567207823 countsByYear W25672078232018 @default.
• W2567207823 countsByYear W25672078232019 @default.
• W2567207823 countsByYear W25672078232020 @default.
• W2567207823 countsByYear W25672078232021 @default.
• W2567207823 countsByYear W25672078232022 @default.
• W2567207823 countsByYear W25672078232023 @default.
• W2567207823 crossrefType "journal-article" @default.
• W2567207823 hasAuthorship W2567207823A5009457889 @default.
• W2567207823 hasAuthorship W2567207823A5015477254 @default.
• W2567207823 hasAuthorship W2567207823A5026011171 @default.
• W2567207823 hasConcept C109007969 @default.
• W2567207823 hasConcept C114793014 @default.
• W2567207823 hasConcept C120806208 @default.
• W2567207823 hasConcept C127313418 @default.

• next