FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W4283162016> ?p ?o ?g. }

• W4283162016 abstract "Abstract Continental extension is accommodated by the development of kilometer‐scale normal faults, which grow during meter‐scale slip events that occur over millions of years. However, reconstructing the entire lifespan of a fault remains challenging due to a lack of observational data with spatiotemporal scales that span the early stage (<10 6 yrs) of fault growth. Using three‐dimensional numerical simulations of continental extension and novel methods for extracting the locations of faults, we quantitatively examine the key factors controlling the growth of rift‐scale fault networks over 10 4 –10 6 yrs. Early formed faults (<100 kyrs from initiation) exhibit scaling ratios consistent with those characterizing individual earthquake ruptures, before evolving to be geometrically and kinematically similar to more mature structures developed in natural fault networks. Whereas finite fault lengths are rapidly established (<100 kyrs), active deformation is transient, migrating both along‐ and across‐strike. Competing stress interactions determine the distribution of active strain, which oscillates between being distributed and localized. Higher rates of extension (10 mm yr −1 ) lead to more prominent stress redistributions through time, promoting episodic localized slip events. Our findings demonstrate that normal fault growth and the related occurrence of cumulative slip is more complex than that currently inferred from displacement patterns on now‐inactive structures, which only provide a space‐ and time‐averaged picture of fault kinematics and related seismic hazard." @default.
• W4283162016 created "2022-06-21" @default.
• W4283162016 creator A5037066162 @default.
• W4283162016 creator A5038951648 @default.
• W4283162016 creator A5051782784 @default.
• W4283162016 creator A5084726357 @default.
• W4283162016 date "2022-07-01" @default.
• W4283162016 modified "2023-10-05" @default.
• W4283162016 title "Bridging Spatiotemporal Scales of Normal Fault Growth During Continental Extension Using High‐Resolution 3D Numerical Models" @default.
• W4283162016 cites W131420489 @default.
• W4283162016 cites W1506911206 @default.
• W4283162016 cites W1678049551 @default.
• W4283162016 cites W1804188941 @default.
• W4283162016 cites W1874082416 @default.
• W4283162016 cites W1874623802 @default.
• W4283162016 cites W1938551673 @default.
• W4283162016 cites W1976811458 @default.
• W4283162016 cites W1978423887 @default.
• W4283162016 cites W1978619457 @default.
• W4283162016 cites W1983039069 @default.
• W4283162016 cites W1989239363 @default.
• W4283162016 cites W1990772221 @default.
• W4283162016 cites W1991607364 @default.
• W4283162016 cites W1992882250 @default.
• W4283162016 cites W1994323983 @default.
• W4283162016 cites W2002216731 @default.
• W4283162016 cites W2005763377 @default.
• W4283162016 cites W2007996144 @default.
• W4283162016 cites W2022192858 @default.
• W4283162016 cites W2023458663 @default.
• W4283162016 cites W2023781184 @default.
• W4283162016 cites W2026982741 @default.
• W4283162016 cites W2027588046 @default.
• W4283162016 cites W2027650026 @default.
• W4283162016 cites W2028126209 @default.
• W4283162016 cites W2028695951 @default.
• W4283162016 cites W2029675608 @default.
• W4283162016 cites W2034896492 @default.
• W4283162016 cites W2039427030 @default.
• W4283162016 cites W2041191706 @default.
• W4283162016 cites W2041741922 @default.
• W4283162016 cites W2041995828 @default.
• W4283162016 cites W2045009186 @default.
• W4283162016 cites W2045572504 @default.
• W4283162016 cites W2048457371 @default.
• W4283162016 cites W2054321704 @default.
• W4283162016 cites W2055226746 @default.
• W4283162016 cites W2063686424 @default.
• W4283162016 cites W2072129919 @default.
• W4283162016 cites W2076373896 @default.
• W4283162016 cites W2081040260 @default.
• W4283162016 cites W2085189279 @default.
• W4283162016 cites W2093488255 @default.
• W4283162016 cites W2095254973 @default.
• W4283162016 cites W2096141135 @default.
• W4283162016 cites W2098854240 @default.
• W4283162016 cites W2099260306 @default.
• W4283162016 cites W2103423476 @default.
• W4283162016 cites W2114458004 @default.
• W4283162016 cites W2124173286 @default.
• W4283162016 cites W2130040965 @default.
• W4283162016 cites W2132368089 @default.
• W4283162016 cites W2135340540 @default.
• W4283162016 cites W2140163715 @default.
• W4283162016 cites W2141396676 @default.
• W4283162016 cites W2142300912 @default.
• W4283162016 cites W2144594884 @default.
• W4283162016 cites W2152043358 @default.
• W4283162016 cites W2154755364 @default.
• W4283162016 cites W2166134193 @default.
• W4283162016 cites W2167327624 @default.
• W4283162016 cites W2168687360 @default.
• W4283162016 cites W2171212919 @default.
• W4283162016 cites W2279321587 @default.
• W4283162016 cites W2286743874 @default.
• W4283162016 cites W2402196459 @default.
• W4283162016 cites W2518194661 @default.
• W4283162016 cites W2532673054 @default.
• W4283162016 cites W2536347096 @default.
• W4283162016 cites W2552021523 @default.
• W4283162016 cites W2566406820 @default.
• W4283162016 cites W2585229793 @default.
• W4283162016 cites W2587053658 @default.
• W4283162016 cites W2589446435 @default.
• W4283162016 cites W2597795855 @default.
• W4283162016 cites W2618948903 @default.
• W4283162016 cites W2783597319 @default.
• W4283162016 cites W2790674774 @default.
• W4283162016 cites W2802017015 @default.
• W4283162016 cites W2885490588 @default.
• W4283162016 cites W2897057308 @default.
• W4283162016 cites W2940211871 @default.
• W4283162016 cites W2980980383 @default.
• W4283162016 cites W2989695732 @default.
• W4283162016 cites W3006233716 @default.
• W4283162016 cites W3007690964 @default.
• W4283162016 cites W3008872883 @default.
• W4283162016 cites W3027495458 @default.
• W4283162016 cites W3080322780 @default.
• W4283162016 cites W3090800880 @default.

• next