FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2006338506> ?p ?o ?g. }

• W2006338506 endingPage "93" @default.
• W2006338506 startingPage "87" @default.
• W2006338506 abstract "We present initial results from three-dimensional inversion of long period EarthScope magnetotelluric (MT) transportable array data from 232 sites covering the north-central US. The study area covers the 1.1 Ga Mid-Continent Rift (MCR) system, which cuts across a series of Archean and Paleoproterozoic lithospheric blocks. The western arm of the MCR is clearly evident in shallow depth sections, with a narrow resistive core, flanked by elongate conductive basins. Other prominent upper-crustal features mapped include the moderately conductive Michigan and Illinois Basins, and extremely high conductivities in foreland basin rocks at the southern margin of the Superior craton. The most prominent conductive anomalies, in an otherwise relatively resistive mid-lower crust, are two elongate east–west oriented structures, which are closely aligned with previously inferred continental sutures. The first underlies the southern margin of the Superior craton just north of the Niagara Fault (NF), and can be associated with the ∼1.85 Ga Penokean Orogeny. A second, further south beneath Iowa and western Wisconsin, lies just south of the Spirit Lake tectonic zone (SLtz), and can be identified with Yavapai accretion at ∼1.75 Ga. Both of these conductive sutures are cleanly cut by the MCR, which is otherwise not clearly evident in the deeper parts of the resistivity model. The break in the anomalies is narrow, comparable to the surface expression of the MCR, indicating that rifting impacts on the entire crustal section were highly localized. Both suture-related anomalies are imaged as extending into, and perhaps through, the lithosphere as dipping diffuse zones of reduced mantle resistivity. Sense of dip of these structures (southward for the NF anomaly, northward for SLtz) agrees with previously inferred models for subduction and accretion, suggesting that a conductive phase (most likely carbon) has been thrust deep into the lower crust and uppermost mantle, providing a marker of the three-dimensional boundary between lithospheric blocks. Resistivities drop below ∼100 Ω m below ∼200 km depth, in rough agreement with the seismically determined lithosphere–asthenosphere boundary (LAB). There are modest lateral variations in this deep low-resistivity layer, but the reliability and significance of these are not yet clear." @default.
• W2006338506 created "2016-06-24" @default.
• W2006338506 creator A5025560323 @default.
• W2006338506 creator A5051727497 @default.
• W2006338506 creator A5075822850 @default.
• W2006338506 creator A5085981009 @default.
• W2006338506 date "2015-07-01" @default.
• W2006338506 modified "2023-10-15" @default.
• W2006338506 title "Three-dimensional electrical resistivity of the north-central USA from EarthScope long period magnetotelluric data" @default.
• W2006338506 cites W1551352350 @default.
• W2006338506 cites W1595554792 @default.
• W2006338506 cites W1603052012 @default.
• W2006338506 cites W1832967011 @default.
• W2006338506 cites W1959325106 @default.
• W2006338506 cites W1975258099 @default.
• W2006338506 cites W1984744184 @default.
• W2006338506 cites W1989986197 @default.
• W2006338506 cites W1990774794 @default.
• W2006338506 cites W1999033332 @default.
• W2006338506 cites W1999310631 @default.
• W2006338506 cites W2001782868 @default.
• W2006338506 cites W2005055602 @default.
• W2006338506 cites W2006275576 @default.
• W2006338506 cites W2016685653 @default.
• W2006338506 cites W2027393025 @default.
• W2006338506 cites W2033957733 @default.
• W2006338506 cites W2035598920 @default.
• W2006338506 cites W2051479138 @default.
• W2006338506 cites W2051734966 @default.
• W2006338506 cites W2058922119 @default.
• W2006338506 cites W2065158612 @default.
• W2006338506 cites W2077636394 @default.
• W2006338506 cites W2078031812 @default.
• W2006338506 cites W2078218873 @default.
• W2006338506 cites W2084600133 @default.
• W2006338506 cites W2085806165 @default.
• W2006338506 cites W2087319249 @default.
• W2006338506 cites W2090390158 @default.
• W2006338506 cites W2101051196 @default.
• W2006338506 cites W2108298625 @default.
• W2006338506 cites W2110040548 @default.
• W2006338506 cites W2113979318 @default.
• W2006338506 cites W2116568968 @default.
• W2006338506 cites W2119969303 @default.
• W2006338506 cites W2131056151 @default.
• W2006338506 cites W2138947960 @default.
• W2006338506 cites W2141304960 @default.
• W2006338506 cites W2144623998 @default.
• W2006338506 cites W2145370114 @default.
• W2006338506 cites W2148511446 @default.
• W2006338506 cites W2162450190 @default.
• W2006338506 cites W2168484983 @default.
• W2006338506 doi "https://doi.org/10.1016/j.epsl.2015.04.006" @default.
• W2006338506 hasPublicationYear "2015" @default.
• W2006338506 type Work @default.
• W2006338506 sameAs 2006338506 @default.
• W2006338506 citedByCount "77" @default.
• W2006338506 countsByYear W20063385062015 @default.
• W2006338506 countsByYear W20063385062016 @default.
• W2006338506 countsByYear W20063385062017 @default.
• W2006338506 countsByYear W20063385062018 @default.
• W2006338506 countsByYear W20063385062019 @default.
• W2006338506 countsByYear W20063385062020 @default.
• W2006338506 countsByYear W20063385062021 @default.
• W2006338506 countsByYear W20063385062022 @default.
• W2006338506 countsByYear W20063385062023 @default.
• W2006338506 crossrefType "journal-article" @default.
• W2006338506 hasAuthorship W2006338506A5025560323 @default.
• W2006338506 hasAuthorship W2006338506A5051727497 @default.
• W2006338506 hasAuthorship W2006338506A5075822850 @default.
• W2006338506 hasAuthorship W2006338506A5085981009 @default.
• W2006338506 hasConcept C105702510 @default.
• W2006338506 hasConcept C112313211 @default.
• W2006338506 hasConcept C119599485 @default.
• W2006338506 hasConcept C127313418 @default.
• W2006338506 hasConcept C127413603 @default.
• W2006338506 hasConcept C147717901 @default.
• W2006338506 hasConcept C149347711 @default.
• W2006338506 hasConcept C151730666 @default.
• W2006338506 hasConcept C165205528 @default.
• W2006338506 hasConcept C16942324 @default.
• W2006338506 hasConcept C193748577 @default.
• W2006338506 hasConcept C2776698055 @default.
• W2006338506 hasConcept C2777241186 @default.
• W2006338506 hasConcept C2777327002 @default.
• W2006338506 hasConcept C50682988 @default.
• W2006338506 hasConcept C69990965 @default.
• W2006338506 hasConcept C71924100 @default.
• W2006338506 hasConcept C77928131 @default.
• W2006338506 hasConceptScore W2006338506C105702510 @default.
• W2006338506 hasConceptScore W2006338506C112313211 @default.
• W2006338506 hasConceptScore W2006338506C119599485 @default.
• W2006338506 hasConceptScore W2006338506C127313418 @default.
• W2006338506 hasConceptScore W2006338506C127413603 @default.
• W2006338506 hasConceptScore W2006338506C147717901 @default.
• W2006338506 hasConceptScore W2006338506C149347711 @default.
• W2006338506 hasConceptScore W2006338506C151730666 @default.
• W2006338506 hasConceptScore W2006338506C165205528 @default.

• next