FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2102045145> ?p ?o ?g. }

• W2102045145 endingPage "45" @default.
• W2102045145 startingPage "22" @default.
• W2102045145 abstract "Dehydration of subducting lithosphere likely transports fluid into the mantle wedge where the viscosity is decreased. Such a decrease in viscosity could form a low viscosity wedge (LVW) or a low viscosity channel (LVC) on top of the subducting slab. Using numerical models, we investigate the influence of low viscosity wedges and channels on subduction zone structure. Slab dip changes substantially with the viscosity reduction within the LVWs and LVCs. For models with or without trench rollback, overthickening of slabs is greatly reduced by LVWs or LVCs. Two divergent evolutionary pathways have been found depending on the maximum depth extent of the LVW and wedge viscosity. Assuming a viscosity contrast of 0.1 with background asthenosphere, models with a LVW that extends down to 400 km depth show a steeply dipping slab, while models with an LVW that extends to much shallower depth, such as 200 km, can produce slabs that are flat lying beneath the overriding plate. There is a narrow range of mantle viscosities that produces flat slabs (5 to10 × 1019 Pa s) and the slab flattening process is enhanced by trench rollback. Slab can be decoupled from the overriding plate with a LVC if the thickness is at least a few 10 s of km, the viscosity reduction is at least a factor of two and the depth extent of the LVC is several hundred km. These models have important implications for the geochemical and spatial evolution of volcanic arcs and the state of stress within the overriding plate. The models explain the poor correlation between traditional geodynamic controls, subducting plate age and convergence rates, on slab dip. We predict that when volcanic arcs change their distance from the trench, they could be preceded by changes in arc chemistry. We predict that there could be a larger volatile input into the wedge when arcs migrate toward the trench and visa-versa. The transition of a subduction zone into the flat-lying regime could be preceded by changes in the volatile budget such that the dehydration front moves to shallower depths. Our flat-slab models shed some light on puzzling flat subduction systems, like in Central Mexico, where there is no deformation within the overriding plate above the flat segment. The lack of in-plane compression in Central Mexico suggests the presence of a low viscosity shear zone above the flat slab." @default.
• W2102045145 created "2016-06-24" @default.
• W2102045145 creator A5001928350 @default.
• W2102045145 creator A5044736391 @default.
• W2102045145 date "2007-12-01" @default.
• W2102045145 modified "2023-10-16" @default.
• W2102045145 title "Subduction zone evolution and low viscosity wedges and channels" @default.
• W2102045145 cites W1517626857 @default.
• W2102045145 cites W1617336291 @default.
• W2102045145 cites W1636995053 @default.
• W2102045145 cites W1705777835 @default.
• W2102045145 cites W1802372289 @default.
• W2102045145 cites W1881271118 @default.
• W2102045145 cites W1914216370 @default.
• W2102045145 cites W1966667510 @default.
• W2102045145 cites W1977202349 @default.
• W2102045145 cites W1981858666 @default.
• W2102045145 cites W1990807634 @default.
• W2102045145 cites W1996412456 @default.
• W2102045145 cites W1997541643 @default.
• W2102045145 cites W2003605988 @default.
• W2102045145 cites W2014133740 @default.
• W2102045145 cites W2015503578 @default.
• W2102045145 cites W2021952952 @default.
• W2102045145 cites W2028983145 @default.
• W2102045145 cites W2032764136 @default.
• W2102045145 cites W2035144837 @default.
• W2102045145 cites W2039802692 @default.
• W2102045145 cites W2040779729 @default.
• W2102045145 cites W2048663634 @default.
• W2102045145 cites W2049007541 @default.
• W2102045145 cites W2050740966 @default.
• W2102045145 cites W2063503947 @default.
• W2102045145 cites W2065305425 @default.
• W2102045145 cites W2067819561 @default.
• W2102045145 cites W2080872690 @default.
• W2102045145 cites W2082691900 @default.
• W2102045145 cites W2083935149 @default.
• W2102045145 cites W2127172635 @default.
• W2102045145 cites W2131004501 @default.
• W2102045145 cites W2138359451 @default.
• W2102045145 cites W2139854519 @default.
• W2102045145 cites W2150579713 @default.
• W2102045145 cites W2167204394 @default.
• W2102045145 doi "https://doi.org/10.1016/j.epsl.2007.08.030" @default.
• W2102045145 hasPublicationYear "2007" @default.
• W2102045145 type Work @default.
• W2102045145 sameAs 2102045145 @default.
• W2102045145 citedByCount "102" @default.
• W2102045145 countsByYear W21020451452012 @default.
• W2102045145 countsByYear W21020451452013 @default.
• W2102045145 countsByYear W21020451452014 @default.
• W2102045145 countsByYear W21020451452015 @default.
• W2102045145 countsByYear W21020451452016 @default.
• W2102045145 countsByYear W21020451452017 @default.
• W2102045145 countsByYear W21020451452018 @default.
• W2102045145 countsByYear W21020451452019 @default.
• W2102045145 countsByYear W21020451452020 @default.
• W2102045145 countsByYear W21020451452021 @default.
• W2102045145 countsByYear W21020451452022 @default.
• W2102045145 countsByYear W21020451452023 @default.
• W2102045145 crossrefType "journal-article" @default.
• W2102045145 hasAuthorship W2102045145A5001928350 @default.
• W2102045145 hasAuthorship W2102045145A5044736391 @default.
• W2102045145 hasConcept C113740112 @default.
• W2102045145 hasConcept C121332964 @default.
• W2102045145 hasConcept C127172972 @default.
• W2102045145 hasConcept C127313418 @default.
• W2102045145 hasConcept C13495919 @default.
• W2102045145 hasConcept C154200439 @default.
• W2102045145 hasConcept C155310634 @default.
• W2102045145 hasConcept C165205528 @default.
• W2102045145 hasConcept C16942324 @default.
• W2102045145 hasConcept C178790620 @default.
• W2102045145 hasConcept C185592680 @default.
• W2102045145 hasConcept C190799397 @default.
• W2102045145 hasConcept C2524010 @default.
• W2102045145 hasConcept C2779227376 @default.
• W2102045145 hasConcept C33923547 @default.
• W2102045145 hasConcept C47422493 @default.
• W2102045145 hasConcept C58097730 @default.
• W2102045145 hasConcept C5900021 @default.
• W2102045145 hasConcept C67236022 @default.
• W2102045145 hasConcept C73462661 @default.
• W2102045145 hasConcept C77928131 @default.
• W2102045145 hasConcept C8058405 @default.
• W2102045145 hasConcept C90523207 @default.
• W2102045145 hasConcept C97355855 @default.
• W2102045145 hasConceptScore W2102045145C113740112 @default.
• W2102045145 hasConceptScore W2102045145C121332964 @default.
• W2102045145 hasConceptScore W2102045145C127172972 @default.
• W2102045145 hasConceptScore W2102045145C127313418 @default.
• W2102045145 hasConceptScore W2102045145C13495919 @default.
• W2102045145 hasConceptScore W2102045145C154200439 @default.
• W2102045145 hasConceptScore W2102045145C155310634 @default.
• W2102045145 hasConceptScore W2102045145C165205528 @default.
• W2102045145 hasConceptScore W2102045145C16942324 @default.
• W2102045145 hasConceptScore W2102045145C178790620 @default.

• next