FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2016068404> ?p ?o ?g. }

• W2016068404 endingPage "78" @default.
• W2016068404 startingPage "45" @default.
• W2016068404 abstract "Interpretation of reprocessed seismic reflection profiles reveals three highly coherent, layered, unconformity-bounded sequences that overlie (or are incorporated within) the Proterozoic “granite–rhyolite province” beneath the Paleozoic Illinois basin and extend down into middle crustal depths. The sequences, which are situated in east–central Illinois and west–central Indiana, are bounded by strong, laterally continuous reflectors that are mappable over distances in excess of 200 km and are expressed as broad “basinal” packages that become areally more restricted with depth. Normal-fault reflector offsets progressively disrupt the sequences with depth along their outer margins. We interpret these sequences as being remnants of a Proterozoic rhyolitic caldera complex and/or rift episode related to the original thermal event that produced the granite–rhyolite province. The overall thickness and distribution of the sequences mimic closely those of the overlying Mt. Simon (Late Cambrian) clastic sediments and indicate that an episode of localized subsidence was underway before deposition of the post-Cambrian Illinois basin stratigraphic succession, which is centered farther south over the “New Madrid rift system” (i.e., Reelfoot rift and Rough Creek graben). The present configuration of the Illinois basin was therefore shaped by the cumulative effects of subsidence in two separate regions, the Proterozoic caldera complex and/or rift in east–central Illinois and west–central Indiana and the New Madrid rift system to the south. Filtered isostatic gravity and magnetic intensity data preclude a large mafic igneous component to the crust so that any Proterozoic volcanic or rift episode must not have tapped deeply or significantly into the lower crust or upper mantle during the heating event responsible for the granite–rhyolite." @default.
• W2016068404 created "2016-06-24" @default.
• W2016068404 creator A5028144037 @default.
• W2016068404 creator A5028607010 @default.
• W2016068404 creator A5043490352 @default.
• W2016068404 date "2003-02-01" @default.
• W2016068404 modified "2023-10-17" @default.
• W2016068404 title "Geophysical constraints on understanding the origin of the Illinois basin and its underlying crust" @default.
• W2016068404 cites W1964286516 @default.
• W2016068404 cites W1969989885 @default.
• W2016068404 cites W1983900011 @default.
• W2016068404 cites W1986348313 @default.
• W2016068404 cites W1993516692 @default.
• W2016068404 cites W1997764654 @default.
• W2016068404 cites W1999806243 @default.
• W2016068404 cites W2002879435 @default.
• W2016068404 cites W2013411947 @default.
• W2016068404 cites W2014273112 @default.
• W2016068404 cites W2015519679 @default.
• W2016068404 cites W2031484793 @default.
• W2016068404 cites W2035594215 @default.
• W2016068404 cites W2039426898 @default.
• W2016068404 cites W2040728587 @default.
• W2016068404 cites W2053180730 @default.
• W2016068404 cites W2058632905 @default.
• W2016068404 cites W2060476005 @default.
• W2016068404 cites W2066699442 @default.
• W2016068404 cites W2071757103 @default.
• W2016068404 cites W2073262550 @default.
• W2016068404 cites W2078111943 @default.
• W2016068404 cites W2090390158 @default.
• W2016068404 cites W2093839271 @default.
• W2016068404 cites W2101492786 @default.
• W2016068404 cites W2105158415 @default.
• W2016068404 cites W2109179076 @default.
• W2016068404 cites W2117028130 @default.
• W2016068404 cites W2137267729 @default.
• W2016068404 cites W2141211561 @default.
• W2016068404 cites W2144460094 @default.
• W2016068404 cites W2149161928 @default.
• W2016068404 cites W2149729749 @default.
• W2016068404 cites W2164803645 @default.
• W2016068404 cites W2264050337 @default.
• W2016068404 cites W2320395462 @default.
• W2016068404 cites W2644132672 @default.
• W2016068404 cites W4241857839 @default.
• W2016068404 doi "https://doi.org/10.1016/s0040-1951(02)00653-4" @default.
• W2016068404 hasPublicationYear "2003" @default.
• W2016068404 type Work @default.
• W2016068404 sameAs 2016068404 @default.
• W2016068404 citedByCount "30" @default.
• W2016068404 countsByYear W20160684042013 @default.
• W2016068404 countsByYear W20160684042014 @default.
• W2016068404 countsByYear W20160684042015 @default.
• W2016068404 countsByYear W20160684042016 @default.
• W2016068404 countsByYear W20160684042017 @default.
• W2016068404 countsByYear W20160684042019 @default.
• W2016068404 countsByYear W20160684042020 @default.
• W2016068404 countsByYear W20160684042021 @default.
• W2016068404 countsByYear W20160684042022 @default.
• W2016068404 crossrefType "journal-article" @default.
• W2016068404 hasAuthorship W2016068404A5028144037 @default.
• W2016068404 hasAuthorship W2016068404A5028607010 @default.
• W2016068404 hasAuthorship W2016068404A5043490352 @default.
• W2016068404 hasConcept C109007969 @default.
• W2016068404 hasConcept C120806208 @default.
• W2016068404 hasConcept C127313418 @default.
• W2016068404 hasConcept C151730666 @default.
• W2016068404 hasConcept C165205528 @default.
• W2016068404 hasConcept C166839181 @default.
• W2016068404 hasConcept C191735495 @default.
• W2016068404 hasConcept C192241223 @default.
• W2016068404 hasConcept C200646496 @default.
• W2016068404 hasConcept C25822816 @default.
• W2016068404 hasConcept C2776698055 @default.
• W2016068404 hasConcept C42787717 @default.
• W2016068404 hasConcept C49708893 @default.
• W2016068404 hasConcept C50682988 @default.
• W2016068404 hasConcept C77928131 @default.
• W2016068404 hasConcept C93033518 @default.
• W2016068404 hasConceptScore W2016068404C109007969 @default.
• W2016068404 hasConceptScore W2016068404C120806208 @default.
• W2016068404 hasConceptScore W2016068404C127313418 @default.
• W2016068404 hasConceptScore W2016068404C151730666 @default.
• W2016068404 hasConceptScore W2016068404C165205528 @default.
• W2016068404 hasConceptScore W2016068404C166839181 @default.
• W2016068404 hasConceptScore W2016068404C191735495 @default.
• W2016068404 hasConceptScore W2016068404C192241223 @default.
• W2016068404 hasConceptScore W2016068404C200646496 @default.
• W2016068404 hasConceptScore W2016068404C25822816 @default.
• W2016068404 hasConceptScore W2016068404C2776698055 @default.
• W2016068404 hasConceptScore W2016068404C42787717 @default.
• W2016068404 hasConceptScore W2016068404C49708893 @default.
• W2016068404 hasConceptScore W2016068404C50682988 @default.
• W2016068404 hasConceptScore W2016068404C77928131 @default.
• W2016068404 hasConceptScore W2016068404C93033518 @default.
• W2016068404 hasIssue "1-2" @default.
• W2016068404 hasLocation W20160684041 @default.

• next