FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2888896057> ?p ?o ?g. }

• W2888896057 endingPage "77" @default.
• W2888896057 startingPage "67" @default.
• W2888896057 abstract "The mechanisms underpinning the formation of a focused volcanic arc above subduction zones are debated. Suggestions include controls by: (i) where the subducting plate releases water, lowering the solidus in the overlying mantle wedge; (ii) the location where the mantle wedge melts to the highest degree; and (iii) a limit on melt formation and migration imposed by the cool shallow corner of the wedge. Here, we evaluate these three proposed mechanisms using a set of kinematically-driven 2D thermo-mechanical mantle-wedge models in which subduction velocity, slab dip and age, overriding-plate thickness and the depth of decoupling between the two plates are systematically varied. All mechanisms predict, on the basis of model geometry, that the arc-trench distance, D, decreases strongly with increasing dip, consistent with the negative D-dip correlations found in global subduction data. Model trends of sub-arc slab depth, H, with dip are positive if H is wedge-temperature controlled and overriding-plate thickness does not exceed the decoupling depth by more than 50 km, and negative if H is slab-temperature controlled. Observed global H-dip trends are overall positive. With increasing overriding plate thickness, the position of maximum melting shifts to smaller H and D, while the position of the trenchward limit of the melt zone, controlled by the wedge's cold corner, shifts to larger H and D, similar to the trend in the data for oceanic subduction zones. Thus, the limit imposed by the wedge corner on melting and melt migration seems to exert the first-order control on arc position." @default.
• W2888896057 created "2018-09-07" @default.
• W2888896057 creator A5016684626 @default.
• W2888896057 creator A5067901321 @default.
• W2888896057 creator A5080374258 @default.
• W2888896057 creator A5081461300 @default.
• W2888896057 creator A5091065111 @default.
• W2888896057 date "2018-11-01" @default.
• W2888896057 modified "2023-09-27" @default.
• W2888896057 title "Mantle wedge temperatures and their potential relation to volcanic arc location" @default.
• W2888896057 cites W1512403705 @default.
• W2888896057 cites W1521394556 @default.
• W2888896057 cites W1532952932 @default.
• W2888896057 cites W1561659903 @default.
• W2888896057 cites W1636995053 @default.
• W2888896057 cites W1821593081 @default.
• W2888896057 cites W1830358639 @default.
• W2888896057 cites W1939540231 @default.
• W2888896057 cites W1969768838 @default.
• W2888896057 cites W1974881268 @default.
• W2888896057 cites W1975546571 @default.
• W2888896057 cites W1980796709 @default.
• W2888896057 cites W1991760432 @default.
• W2888896057 cites W1994457548 @default.
• W2888896057 cites W1996412456 @default.
• W2888896057 cites W1998601546 @default.
• W2888896057 cites W2000446883 @default.
• W2888896057 cites W2003605988 @default.
• W2888896057 cites W2008935602 @default.
• W2888896057 cites W2009279133 @default.
• W2888896057 cites W2009307089 @default.
• W2888896057 cites W2010809235 @default.
• W2888896057 cites W2017178470 @default.
• W2888896057 cites W2017649324 @default.
• W2888896057 cites W2032764136 @default.
• W2888896057 cites W2047136803 @default.
• W2888896057 cites W2048254804 @default.
• W2888896057 cites W2052079943 @default.
• W2888896057 cites W2057430531 @default.
• W2888896057 cites W2060886682 @default.
• W2888896057 cites W2063503947 @default.
• W2888896057 cites W2064985255 @default.
• W2888896057 cites W2070854336 @default.
• W2888896057 cites W2080872690 @default.
• W2888896057 cites W2084153237 @default.
• W2888896057 cites W2098031509 @default.
• W2888896057 cites W2108597026 @default.
• W2888896057 cites W2113469927 @default.
• W2888896057 cites W2118172271 @default.
• W2888896057 cites W2124139363 @default.
• W2888896057 cites W2138534190 @default.
• W2888896057 cites W2148372410 @default.
• W2888896057 cites W2153132363 @default.
• W2888896057 cites W2155383135 @default.
• W2888896057 cites W2162179574 @default.
• W2888896057 cites W2163820899 @default.
• W2888896057 cites W2266100410 @default.
• W2888896057 cites W2512451499 @default.
• W2888896057 cites W2528710430 @default.
• W2888896057 cites W2606717285 @default.
• W2888896057 cites W2738254706 @default.
• W2888896057 doi "https://doi.org/10.1016/j.epsl.2018.08.011" @default.
• W2888896057 hasPublicationYear "2018" @default.
• W2888896057 type Work @default.
• W2888896057 sameAs 2888896057 @default.
• W2888896057 citedByCount "33" @default.
• W2888896057 countsByYear W28888960572019 @default.
• W2888896057 countsByYear W28888960572020 @default.
• W2888896057 countsByYear W28888960572021 @default.
• W2888896057 countsByYear W28888960572022 @default.
• W2888896057 countsByYear W28888960572023 @default.
• W2888896057 crossrefType "journal-article" @default.
• W2888896057 hasAuthorship W2888896057A5016684626 @default.
• W2888896057 hasAuthorship W2888896057A5067901321 @default.
• W2888896057 hasAuthorship W2888896057A5080374258 @default.
• W2888896057 hasAuthorship W2888896057A5081461300 @default.
• W2888896057 hasAuthorship W2888896057A5091065111 @default.
• W2888896057 hasBestOaLocation W28888960571 @default.
• W2888896057 hasConcept C113740112 @default.
• W2888896057 hasConcept C127313418 @default.
• W2888896057 hasConcept C127413603 @default.
• W2888896057 hasConcept C133731056 @default.
• W2888896057 hasConcept C154200439 @default.
• W2888896057 hasConcept C163686574 @default.
• W2888896057 hasConcept C165205528 @default.
• W2888896057 hasConcept C180492444 @default.
• W2888896057 hasConcept C190799397 @default.
• W2888896057 hasConcept C205606062 @default.
• W2888896057 hasConcept C2524010 @default.
• W2888896057 hasConcept C33923547 @default.
• W2888896057 hasConcept C47422493 @default.
• W2888896057 hasConcept C58097730 @default.
• W2888896057 hasConcept C5900021 @default.
• W2888896057 hasConcept C67236022 @default.
• W2888896057 hasConcept C73462661 @default.
• W2888896057 hasConcept C77928131 @default.
• W2888896057 hasConcept C8058405 @default.
• W2888896057 hasConcept C90523207 @default.

• next