FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2004163532> ?p ?o ?g. }

• W2004163532 endingPage "192" @default.
• W2004163532 startingPage "173" @default.
• W2004163532 abstract "Surface ruptures associated with the 1999 Mw=7.6 Chi-Chi earthquake in central western Taiwan have been characterised by mapping along the northern fault-segment. The earthquake occurred on the reactivated Chelungpu fault in the frontal portion of the thin-skinned Taiwan fold-and-thrust belt. The N–S trending Chelungpu fault is a 90-km-long major west-verging thrust, which principally slips within, and parallel to, bedding of the Pliocene Chinshui Shale. In the northern segment of the earthquake fault trace, that we name the Shihkang–Shangchi fault zone, the surface ruptures turn to an E–W strike and produce a series of thrust-and-backthrust pop-ups, about 15 km long, forming several discontinuous subsegments distributed within a broad regional Pliocene syncline. The northern fault segments activated during the Chi-Chi earthquake, in the area where the displacement is largest, not only display anomalous trends and a variety of mechanisms, but also raise a major problem of structural inheritance. Detailed field investigation and kinematic analysis indicate that the surface ruptures in the Shihkang–Shangchi fault zone are the result of dip-slip thrusting, occasionally with a minor strike-slip component. The surface ruptures emerge at the surface from bedding-parallel thrusts on both limbs of the regional south-plunging syncline. In the middle part of the syncline, bedding-parallel thrusts are connected by thrusts that cross-cut beds. The surface ruptures also reactivate a NE–SW trending anticline (Diaoshenshan), with west-vergent thrust on the backlimb and east-vergent backthrust on the forelimb. This anticline is undergoing uplift by breaking through the regional N–S trending syncline. Combining GPS measurements, seismological data, and geological analyses, we propose a kinematic model with a 3-D fault surface for the 1999 earthquake in the area of the northern termination. We highlight the influence of both the local and regional structures (bedding parallel slip, pre-existing faults and folds) on the development of the earthquake rupture, and hence the role of the structural inheritance. We conclude that the south-plunging regional Pliocene syncline in fact acts as a slip/strain guide for the northern termination of the Chelungpu thrust. The Pliocene Chinshui Shale, as a major source of weakness within the syncline, has strongly influenced the pattern of slip surface during the 1999 earthquake rupture. We interpret the large vertical displacement along the northern segment as the fault rupture occurring over a surface whose radius of curvature tightens toward the north around the core of the syncline." @default.
• W2004163532 created "2016-06-24" @default.
• W2004163532 creator A5000914651 @default.
• W2004163532 creator A5010053486 @default.
• W2004163532 creator A5024542860 @default.
• W2004163532 creator A5036497451 @default.
• W2004163532 creator A5061217258 @default.
• W2004163532 creator A5066711510 @default.
• W2004163532 creator A5076011609 @default.
• W2004163532 date "2002-01-01" @default.
• W2004163532 modified "2023-10-14" @default.
• W2004163532 title "Geometry and structure of northern surface ruptures of the 1999 Mw=7.6 Chi-Chi Taiwan earthquake: influence from inherited fold belt structures" @default.
• W2004163532 cites W1965550291 @default.
• W2004163532 cites W1979797863 @default.
• W2004163532 cites W1980698240 @default.
• W2004163532 cites W1997492950 @default.
• W2004163532 cites W2022415851 @default.
• W2004163532 cites W2035727064 @default.
• W2004163532 cites W2036056375 @default.
• W2004163532 cites W2038630183 @default.
• W2004163532 cites W2054730724 @default.
• W2004163532 cites W2075938472 @default.
• W2004163532 cites W2078910455 @default.
• W2004163532 cites W2094603286 @default.
• W2004163532 cites W2094833562 @default.
• W2004163532 cites W2104886142 @default.
• W2004163532 cites W2140709557 @default.
• W2004163532 cites W2148799848 @default.
• W2004163532 cites W2261623958 @default.
• W2004163532 cites W2273630397 @default.
• W2004163532 cites W2296322228 @default.
• W2004163532 cites W2302857091 @default.
• W2004163532 cites W2496336242 @default.
• W2004163532 doi "https://doi.org/10.1016/s0191-8141(01)00056-6" @default.
• W2004163532 hasPublicationYear "2002" @default.
• W2004163532 type Work @default.
• W2004163532 sameAs 2004163532 @default.
• W2004163532 citedByCount "136" @default.
• W2004163532 countsByYear W20041635322012 @default.
• W2004163532 countsByYear W20041635322013 @default.
• W2004163532 countsByYear W20041635322014 @default.
• W2004163532 countsByYear W20041635322015 @default.
• W2004163532 countsByYear W20041635322016 @default.
• W2004163532 countsByYear W20041635322017 @default.
• W2004163532 countsByYear W20041635322018 @default.
• W2004163532 countsByYear W20041635322019 @default.
• W2004163532 countsByYear W20041635322020 @default.
• W2004163532 countsByYear W20041635322021 @default.
• W2004163532 countsByYear W20041635322022 @default.
• W2004163532 countsByYear W20041635322023 @default.
• W2004163532 crossrefType "journal-article" @default.
• W2004163532 hasAuthorship W2004163532A5000914651 @default.
• W2004163532 hasAuthorship W2004163532A5010053486 @default.
• W2004163532 hasAuthorship W2004163532A5024542860 @default.
• W2004163532 hasAuthorship W2004163532A5036497451 @default.
• W2004163532 hasAuthorship W2004163532A5061217258 @default.
• W2004163532 hasAuthorship W2004163532A5066711510 @default.
• W2004163532 hasAuthorship W2004163532A5076011609 @default.
• W2004163532 hasBestOaLocation W20041635324 @default.
• W2004163532 hasConcept C110041135 @default.
• W2004163532 hasConcept C116637073 @default.
• W2004163532 hasConcept C121332964 @default.
• W2004163532 hasConcept C127313418 @default.
• W2004163532 hasConcept C127413603 @default.
• W2004163532 hasConcept C144027150 @default.
• W2004163532 hasConcept C149465734 @default.
• W2004163532 hasConcept C165205528 @default.
• W2004163532 hasConcept C175551986 @default.
• W2004163532 hasConcept C195268267 @default.
• W2004163532 hasConcept C2776545315 @default.
• W2004163532 hasConcept C2777232088 @default.
• W2004163532 hasConcept C2993396000 @default.
• W2004163532 hasConcept C52678131 @default.
• W2004163532 hasConcept C53942344 @default.
• W2004163532 hasConcept C7251660 @default.
• W2004163532 hasConcept C77928131 @default.
• W2004163532 hasConcept C78519656 @default.
• W2004163532 hasConcept C79420006 @default.
• W2004163532 hasConcept C86803240 @default.
• W2004163532 hasConcept C97355855 @default.
• W2004163532 hasConceptScore W2004163532C110041135 @default.
• W2004163532 hasConceptScore W2004163532C116637073 @default.
• W2004163532 hasConceptScore W2004163532C121332964 @default.
• W2004163532 hasConceptScore W2004163532C127313418 @default.
• W2004163532 hasConceptScore W2004163532C127413603 @default.
• W2004163532 hasConceptScore W2004163532C144027150 @default.
• W2004163532 hasConceptScore W2004163532C149465734 @default.
• W2004163532 hasConceptScore W2004163532C165205528 @default.
• W2004163532 hasConceptScore W2004163532C175551986 @default.
• W2004163532 hasConceptScore W2004163532C195268267 @default.
• W2004163532 hasConceptScore W2004163532C2776545315 @default.
• W2004163532 hasConceptScore W2004163532C2777232088 @default.
• W2004163532 hasConceptScore W2004163532C2993396000 @default.
• W2004163532 hasConceptScore W2004163532C52678131 @default.
• W2004163532 hasConceptScore W2004163532C53942344 @default.
• W2004163532 hasConceptScore W2004163532C7251660 @default.
• W2004163532 hasConceptScore W2004163532C77928131 @default.
• W2004163532 hasConceptScore W2004163532C78519656 @default.

• next