FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W4308743463> ?p ?o ?g. }

• W4308743463 endingPage "117888" @default.
• W4308743463 startingPage "117888" @default.
• W4308743463 abstract "The Integrated Ocean Drilling Program conducted Expedition 343 and 343T, named the Japan Trench Fast Drilling Project (JFAST), to drill through the plate boundary fault that ruptured during the 2011 Mw 9.0 Tohoku earthquake in the area with the largest fault slip displacement near the Japan trench. Analyses of breakouts observed from borehole C0019B produced postearthquake stress states above the plate boundary fault between the subducting Pacific plate and overriding North American plate. To supplement the lack of stress data below the rupture zone of the earthquake, we conducted core-based three-dimensional stress measurements by the anelastic strain recovery (ASR) method using four whole-round core samples of sediments, of which three samples were located above, but one sample was located below the plate boundary fault in borehole C0019E. As a result of the stress measurements, the postearthquake three-dimensional stress magnitudes at ∼802 and ∼828 meters below seafloor (mbsf) across the plate boundary fault at ∼820 mbsf reveal a normal faulting stress regime. The differences between the three-dimensional intermediate principal stress and the minimum principal stress at the two depths are less than 1 MPa, suggesting a complete release of horizontal tectonic stresses that accumulated before the earthquake. In addition, the maximum horizontal stress SHmax azimuth N115°E at ∼828 mbsf below the plate boundary fault from ASR measurements shows consistency with the SHmax azimuth N139 ± 23°E (mean ± standard deviation) at ∼550–810 mbsf from breakout analyses above the fault. Taken together with the similar stress magnitudes at ∼802 and ∼828 mbsf, we interpret that the postearthquake stress states are almost the same in the sediments above and below the plate boundary fault. In other words, the stress state in terms of both orientation and magnitude is continuous across the fault. At a shallower depth of ∼177 mbsf in the slope sediments, the ASR stress data reveal a “stress state at rest”, which is likely free from tectonic effects of plate subduction, suggesting that the stress state was reset by the great coseismic displacement of ∼50 m slipped during the Tohoku earthquake." @default.
• W4308743463 created "2022-11-15" @default.
• W4308743463 creator A5013060805 @default.
• W4308743463 creator A5041412971 @default.
• W4308743463 creator A5076295270 @default.
• W4308743463 date "2023-01-01" @default.
• W4308743463 modified "2023-10-02" @default.
• W4308743463 title "Three-dimensional stress state above and below the plate boundary fault after the 2011 Mw 9.0 Tohoku earthquake" @default.
• W4308743463 cites W1525521307 @default.
• W4308743463 cites W1551655887 @default.
• W4308743463 cites W1689232968 @default.
• W4308743463 cites W1968704068 @default.
• W4308743463 cites W1981523453 @default.
• W4308743463 cites W1998819856 @default.
• W4308743463 cites W2022314603 @default.
• W4308743463 cites W2022774905 @default.
• W4308743463 cites W2024078373 @default.
• W4308743463 cites W2034089522 @default.
• W4308743463 cites W2035446128 @default.
• W4308743463 cites W2035612331 @default.
• W4308743463 cites W2040044650 @default.
• W4308743463 cites W2044727153 @default.
• W4308743463 cites W2044872654 @default.
• W4308743463 cites W2050445830 @default.
• W4308743463 cites W2051102191 @default.
• W4308743463 cites W2052242710 @default.
• W4308743463 cites W2059477612 @default.
• W4308743463 cites W2067242983 @default.
• W4308743463 cites W2075201372 @default.
• W4308743463 cites W2079749210 @default.
• W4308743463 cites W2083949913 @default.
• W4308743463 cites W2088025384 @default.
• W4308743463 cites W2120532388 @default.
• W4308743463 cites W2122111506 @default.
• W4308743463 cites W2124153265 @default.
• W4308743463 cites W2127848990 @default.
• W4308743463 cites W2129289899 @default.
• W4308743463 cites W2129396440 @default.
• W4308743463 cites W2156127212 @default.
• W4308743463 cites W2161284747 @default.
• W4308743463 cites W2729504164 @default.
• W4308743463 cites W2741410973 @default.
• W4308743463 cites W2754972977 @default.
• W4308743463 cites W2971636029 @default.
• W4308743463 cites W2984172238 @default.
• W4308743463 cites W3023274567 @default.
• W4308743463 cites W3038038034 @default.
• W4308743463 cites W4283512606 @default.
• W4308743463 doi "https://doi.org/10.1016/j.epsl.2022.117888" @default.
• W4308743463 hasPublicationYear "2023" @default.
• W4308743463 type Work @default.
• W4308743463 citedByCount "1" @default.
• W4308743463 countsByYear W43087434632023 @default.
• W4308743463 crossrefType "journal-article" @default.
• W4308743463 hasAuthorship W4308743463A5013060805 @default.
• W4308743463 hasAuthorship W4308743463A5041412971 @default.
• W4308743463 hasAuthorship W4308743463A5076295270 @default.
• W4308743463 hasBestOaLocation W43087434631 @default.
• W4308743463 hasConcept C117485682 @default.
• W4308743463 hasConcept C119477230 @default.
• W4308743463 hasConcept C127313418 @default.
• W4308743463 hasConcept C150560799 @default.
• W4308743463 hasConcept C155310634 @default.
• W4308743463 hasConcept C165205528 @default.
• W4308743463 hasConcept C175551986 @default.
• W4308743463 hasConcept C178790620 @default.
• W4308743463 hasConcept C185592680 @default.
• W4308743463 hasConcept C187320778 @default.
• W4308743463 hasConcept C2779227376 @default.
• W4308743463 hasConcept C77928131 @default.
• W4308743463 hasConcept C8058405 @default.
• W4308743463 hasConceptScore W4308743463C117485682 @default.
• W4308743463 hasConceptScore W4308743463C119477230 @default.
• W4308743463 hasConceptScore W4308743463C127313418 @default.
• W4308743463 hasConceptScore W4308743463C150560799 @default.
• W4308743463 hasConceptScore W4308743463C155310634 @default.
• W4308743463 hasConceptScore W4308743463C165205528 @default.
• W4308743463 hasConceptScore W4308743463C175551986 @default.
• W4308743463 hasConceptScore W4308743463C178790620 @default.
• W4308743463 hasConceptScore W4308743463C185592680 @default.
• W4308743463 hasConceptScore W4308743463C187320778 @default.
• W4308743463 hasConceptScore W4308743463C2779227376 @default.
• W4308743463 hasConceptScore W4308743463C77928131 @default.
• W4308743463 hasConceptScore W4308743463C8058405 @default.
• W4308743463 hasLocation W43087434631 @default.
• W4308743463 hasLocation W43087434632 @default.
• W4308743463 hasOpenAccess W4308743463 @default.
• W4308743463 hasPrimaryLocation W43087434631 @default.
• W4308743463 hasRelatedWork W2004477205 @default.
• W4308743463 hasRelatedWork W2057447701 @default.
• W4308743463 hasRelatedWork W2061727365 @default.
• W4308743463 hasRelatedWork W2152907035 @default.
• W4308743463 hasRelatedWork W2604251004 @default.
• W4308743463 hasRelatedWork W2904330901 @default.
• W4308743463 hasRelatedWork W3112513249 @default.
• W4308743463 hasRelatedWork W3141829427 @default.
• W4308743463 hasRelatedWork W4220794936 @default.
• W4308743463 hasRelatedWork W4379469054 @default.

• next