FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2055143212> ?p ?o ?g. }

• W2055143212 endingPage "197" @default.
• W2055143212 startingPage "187" @default.
• W2055143212 abstract "Although subparallel swarms of dikes are thought to be the primary feeders to voluminous volcanic eruptions, increasing recognition of volumetrically significant sill complexes suggests that they too play an important role in magma ascent through the shallow crust. However, the extent to which sills and interconnected, sill-fed dikes actually transport magma to the earth's surface in many large igneous provinces (LIP) is presently unclear. By analyzing field relationships and dimensions of intrusions of the Ferrar LIP in South Victoria Land, Antarctica, we show that sill-fed dikes were the likely feeders for voluminous flood basalt eruptions. These intrusions are small but numerous, with cumulative dimensions equivalent to a feeder network 308,000 km long and 1.8 m wide. Due to the tremendous aerial extent of this intrusive network, each individual dike-feeder segment would only be required to actively feed magma for 2 to 3 days on average to erupt the 70,000 km3 of flood lavas represented by the Kirkpatrick basalts. The Ferrar intrusions form a broadly-distributed array of small, moderately dipping dikes (<2 km long, 1.8 m wide, 56° mean dip) exhibiting almost any orientation. This sill-fed dike network contrasts with dike swarms conventionally depicted to feed flood basalt provinces, and has the appearance of a variably “cracked lid” atop a sill complex. The cracked lid model may apply to a range of shallow feeder systems (<4 km depth) intruding sedimentary basins, where the effects of far-field tectonic stresses are negligible and sill intrusions exert the dominant control on dike orientations. We conclude that sill inflation, and resulting deformation of surrounding host rock, plays a critical role in the ascent of magma in shallow volcanic systems that span the full spectrum of eruptive volumes." @default.
• W2055143212 created "2016-06-24" @default.
• W2055143212 creator A5009296479 @default.
• W2055143212 creator A5047223498 @default.
• W2055143212 creator A5067288162 @default.
• W2055143212 creator A5075572289 @default.
• W2055143212 date "2014-11-01" @default.
• W2055143212 modified "2023-09-27" @default.
• W2055143212 title "Cracking the lid: Sill-fed dikes are the likely feeders of flood basalt eruptions" @default.
• W2055143212 cites W1622540209 @default.
• W2055143212 cites W1630852356 @default.
• W2055143212 cites W1823958478 @default.
• W2055143212 cites W1964057323 @default.
• W2055143212 cites W1965125081 @default.
• W2055143212 cites W1970621880 @default.
• W2055143212 cites W1979525539 @default.
• W2055143212 cites W1982547142 @default.
• W2055143212 cites W1982863321 @default.
• W2055143212 cites W1983586586 @default.
• W2055143212 cites W1984278815 @default.
• W2055143212 cites W1985003499 @default.
• W2055143212 cites W1989704967 @default.
• W2055143212 cites W1990247717 @default.
• W2055143212 cites W1991169017 @default.
• W2055143212 cites W1996288929 @default.
• W2055143212 cites W1999435969 @default.
• W2055143212 cites W1999647445 @default.
• W2055143212 cites W2001931685 @default.
• W2055143212 cites W2002783931 @default.
• W2055143212 cites W2003197391 @default.
• W2055143212 cites W2003929138 @default.
• W2055143212 cites W2004994580 @default.
• W2055143212 cites W2006452390 @default.
• W2055143212 cites W2007035194 @default.
• W2055143212 cites W2007185774 @default.
• W2055143212 cites W2008101170 @default.
• W2055143212 cites W2009046419 @default.
• W2055143212 cites W2011011904 @default.
• W2055143212 cites W2012987873 @default.
• W2055143212 cites W2013540757 @default.
• W2055143212 cites W2015651542 @default.
• W2055143212 cites W2017244727 @default.
• W2055143212 cites W2024203368 @default.
• W2055143212 cites W2025394267 @default.
• W2055143212 cites W2028557000 @default.
• W2055143212 cites W2035249692 @default.
• W2055143212 cites W2041183756 @default.
• W2055143212 cites W2042813819 @default.
• W2055143212 cites W2046081579 @default.
• W2055143212 cites W2056082591 @default.
• W2055143212 cites W2056615483 @default.
• W2055143212 cites W2056893699 @default.
• W2055143212 cites W2066708113 @default.
• W2055143212 cites W2066735401 @default.
• W2055143212 cites W2067477118 @default.
• W2055143212 cites W2067814308 @default.
• W2055143212 cites W2070613300 @default.
• W2055143212 cites W2071453911 @default.
• W2055143212 cites W2071549314 @default.
• W2055143212 cites W2073424164 @default.
• W2055143212 cites W2073866201 @default.
• W2055143212 cites W2076362145 @default.
• W2055143212 cites W2079617843 @default.
• W2055143212 cites W2081766809 @default.
• W2055143212 cites W2082375708 @default.
• W2055143212 cites W2083018176 @default.
• W2055143212 cites W2083583609 @default.
• W2055143212 cites W2088914497 @default.
• W2055143212 cites W2089865309 @default.
• W2055143212 cites W2090933028 @default.
• W2055143212 cites W2098283269 @default.
• W2055143212 cites W2102972282 @default.
• W2055143212 cites W2103951198 @default.
• W2055143212 cites W2109996424 @default.
• W2055143212 cites W2110338571 @default.
• W2055143212 cites W2115949964 @default.
• W2055143212 cites W2120795287 @default.
• W2055143212 cites W2122924553 @default.
• W2055143212 cites W2134425350 @default.
• W2055143212 cites W2134904666 @default.
• W2055143212 cites W2139062884 @default.
• W2055143212 cites W2146367475 @default.
• W2055143212 cites W2146860462 @default.
• W2055143212 cites W2150229553 @default.
• W2055143212 cites W2151203838 @default.
• W2055143212 cites W2153234819 @default.
• W2055143212 cites W2153953550 @default.
• W2055143212 cites W2163555075 @default.
• W2055143212 cites W2314237877 @default.
• W2055143212 cites W2323636640 @default.
• W2055143212 cites W4250227819 @default.
• W2055143212 doi "https://doi.org/10.1016/j.epsl.2014.08.036" @default.
• W2055143212 hasPublicationYear "2014" @default.
• W2055143212 type Work @default.
• W2055143212 sameAs 2055143212 @default.
• W2055143212 citedByCount "54" @default.
• W2055143212 countsByYear W20551432122015 @default.
• W2055143212 countsByYear W20551432122016 @default.

• next