FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W4313461262> ?p ?o ?g. }

• W4313461262 abstract "The formation of new subduction zones is a key element of plate tectonics and the Wilson cycle, and many different controlling mechanisms have been proposed to initiate subduction. Here, we provide a brief overview of the known scenarios of subduction initiation in intra-oceanic and ocean-continent tectonic settings. Intra-oceanic subduction is most commonly associated with mechanical heterogeneities within the oceanic lithosphere, such as pre-existing fracture zones, spreading ridges, and transform faults. Numerous and well-recognized examples of new active subduction zones formed in intra-oceanic environments during the Cenozoic, suggesting that the initiation of ocean-ocean subduction must be a routine process that occurs “easily and frequently” in the mode of plate tectonics currently operating on Earth. On the contrary, the most traditional mechanisms for the establishment of classic self-sustaining ocean-continent subduction—passive margin collapse and subduction transference—are surprisingly rare in observations and difficult to reproduce in numerical models. Two alternative scenarios—polarity reversal and lateral propagation-induced subduction initiation—are in contrast much better documented in nature and experimentally. However, switching of subduction polarity due to arc-continent collision and lateral transmission of subducting plate boundaries are both inextricably linked to pre-existing intra-oceanic convergence. We, therefore, conclude that the onset of classic ocean-continent subduction zones is possible only through the transition from a former intra-oceanic subduction system. This transition is likely facilitated by the ductile damage accumulation and stress concentration across the aging continental margin. From this perspective, the future closure of the Atlantic Ocean can be viewed as an archetypal example of the role of transitional process between intra-oceanic subduction (Lesser Antilles) and the development of a new subduction zone at a passive continental margin (eastern North America)." @default.
• W4313461262 created "2023-01-06" @default.
• W4313461262 creator A5034750019 @default.
• W4313461262 creator A5041024418 @default.
• W4313461262 creator A5049736310 @default.
• W4313461262 creator A5050510608 @default.
• W4313461262 creator A5066630823 @default.
• W4313461262 date "2022-12-21" @default.
• W4313461262 modified "2023-09-26" @default.
• W4313461262 title "Ocean-continent subduction cannot be initiated without preceding intra-oceanic subduction!" @default.
• W4313461262 cites W1530366628 @default.
• W4313461262 cites W1579920087 @default.
• W4313461262 cites W1751400788 @default.
• W4313461262 cites W1939540231 @default.
• W4313461262 cites W1963648072 @default.
• W4313461262 cites W1971450949 @default.
• W4313461262 cites W1971806945 @default.
• W4313461262 cites W1976907465 @default.
• W4313461262 cites W1979892553 @default.
• W4313461262 cites W1980446862 @default.
• W4313461262 cites W1989462364 @default.
• W4313461262 cites W1993052821 @default.
• W4313461262 cites W2010696145 @default.
• W4313461262 cites W2012502888 @default.
• W4313461262 cites W2014883687 @default.
• W4313461262 cites W2019960479 @default.
• W4313461262 cites W2021211260 @default.
• W4313461262 cites W2026963820 @default.
• W4313461262 cites W2029814562 @default.
• W4313461262 cites W2032112226 @default.
• W4313461262 cites W2033378407 @default.
• W4313461262 cites W2036474896 @default.
• W4313461262 cites W2045878430 @default.
• W4313461262 cites W2047519592 @default.
• W4313461262 cites W2057748380 @default.
• W4313461262 cites W2061112693 @default.
• W4313461262 cites W2068495563 @default.
• W4313461262 cites W2075085181 @default.
• W4313461262 cites W2077360518 @default.
• W4313461262 cites W2081868334 @default.
• W4313461262 cites W2090835305 @default.
• W4313461262 cites W2091523110 @default.
• W4313461262 cites W2094268781 @default.
• W4313461262 cites W2103057627 @default.
• W4313461262 cites W2103643797 @default.
• W4313461262 cites W2104837834 @default.
• W4313461262 cites W2106656683 @default.
• W4313461262 cites W2108767568 @default.
• W4313461262 cites W2109027182 @default.
• W4313461262 cites W2120210811 @default.
• W4313461262 cites W2125802015 @default.
• W4313461262 cites W2126039538 @default.
• W4313461262 cites W2132309483 @default.
• W4313461262 cites W2140047497 @default.
• W4313461262 cites W2141384043 @default.
• W4313461262 cites W2143688475 @default.
• W4313461262 cites W2145232227 @default.
• W4313461262 cites W2306725948 @default.
• W4313461262 cites W2319700611 @default.
• W4313461262 cites W2496259675 @default.
• W4313461262 cites W2518035602 @default.
• W4313461262 cites W2748664829 @default.
• W4313461262 cites W2765248296 @default.
• W4313461262 cites W2768156632 @default.
• W4313461262 cites W2803090262 @default.
• W4313461262 cites W2805085867 @default.
• W4313461262 cites W2807327141 @default.
• W4313461262 cites W2883096560 @default.
• W4313461262 cites W2891857590 @default.
• W4313461262 cites W2901582080 @default.
• W4313461262 cites W2902410532 @default.
• W4313461262 cites W2911847179 @default.
• W4313461262 cites W2940576611 @default.
• W4313461262 cites W2940825575 @default.
• W4313461262 cites W2968148426 @default.
• W4313461262 cites W2999633267 @default.
• W4313461262 cites W3009054759 @default.
• W4313461262 cites W3017006927 @default.
• W4313461262 cites W3018816405 @default.
• W4313461262 cites W3039374976 @default.
• W4313461262 cites W3044115035 @default.
• W4313461262 cites W3121906292 @default.
• W4313461262 cites W3122879998 @default.
• W4313461262 cites W3171667537 @default.
• W4313461262 cites W3183770145 @default.
• W4313461262 cites W3197091629 @default.
• W4313461262 cites W3197456468 @default.
• W4313461262 cites W3207805732 @default.
• W4313461262 cites W3210146756 @default.
• W4313461262 cites W3214641082 @default.
• W4313461262 cites W3215125831 @default.
• W4313461262 cites W4206033072 @default.
• W4313461262 cites W4210988231 @default.
• W4313461262 cites W4211010522 @default.
• W4313461262 cites W4211030772 @default.
• W4313461262 cites W4221040240 @default.
• W4313461262 cites W4225415800 @default.
• W4313461262 cites W4230724723 @default.
• W4313461262 cites W4240131429 @default.
• W4313461262 cites W4285604272 @default.

• next