FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W1992029791> ?p ?o ?g. }

• W1992029791 endingPage "15377" @default.
• W1992029791 startingPage "15365" @default.
• W1992029791 abstract "We use the locations and source mechanisms of oceanic intraplate earthquakes to test the hypothesis that the strength of oceanic fracture zones is less than that of normal oceanic lithosphere. If fracture zones are weaker than the surrounding lithosphere, they should be sites of concentrated intraplate seismicity, and the lithospheric stress field should be perturbed in their vicinity. The 77 earthquakes selected for the study have well‐determined focal mechanisms and epicenters in regions where fracture zones are well mapped. We have searched for dependence of faulting style, fault orientation, or principal stress direction on the distance from the nearest fracture zone. If fracture zones were generally weaker than the surrounding lithosphere, one of the principal horizontal stresses would be oriented nearly perpendicular to the fracture zone; we find no evidence that principal stresses near fracture zones are oriented preferentially in this manner. There is a slight tendency for earthquakes to occur near fracture zones, and patterns of fault orientation and sense of slip support the view that differential cooling and horizontal contraction on fracture zones may contribute seismogenic stress. These patterns are not demonstrable at high significance, however. If oceanic transform fault zones are weak relative to the surrounding lithosphere, these results suggest that the strength of the fracture zones increases within a few million years after cessation of transform motion to levels comparable with that of normal oceanic lithosphere." @default.
• W1992029791 created "2016-06-24" @default.
• W1992029791 creator A5026410195 @default.
• W1992029791 creator A5042187705 @default.
• W1992029791 date "1992-10-10" @default.
• W1992029791 modified "2023-10-14" @default.
• W1992029791 title "On the strength of oceanic fracture zones and their influence on the intraplate stress field" @default.
• W1992029791 cites W1637028626 @default.
• W1992029791 cites W1968036908 @default.
• W1992029791 cites W1968824256 @default.
• W1992029791 cites W1973287273 @default.
• W1992029791 cites W1983105885 @default.
• W1992029791 cites W1983992782 @default.
• W1992029791 cites W1992357382 @default.
• W1992029791 cites W1999221527 @default.
• W1992029791 cites W2000210417 @default.
• W1992029791 cites W2001132662 @default.
• W1992029791 cites W2004758340 @default.
• W1992029791 cites W2007738582 @default.
• W1992029791 cites W2010739316 @default.
• W1992029791 cites W2014390311 @default.
• W1992029791 cites W2018618010 @default.
• W1992029791 cites W2019910035 @default.
• W1992029791 cites W2022016919 @default.
• W1992029791 cites W2032260697 @default.
• W1992029791 cites W2033072383 @default.
• W1992029791 cites W2034322653 @default.
• W1992029791 cites W2040105500 @default.
• W1992029791 cites W2043425848 @default.
• W1992029791 cites W2047516202 @default.
• W1992029791 cites W2047712588 @default.
• W1992029791 cites W2048360618 @default.
• W1992029791 cites W2049126610 @default.
• W1992029791 cites W2051364810 @default.
• W1992029791 cites W2053668411 @default.
• W1992029791 cites W2055236946 @default.
• W1992029791 cites W2058953789 @default.
• W1992029791 cites W2059798979 @default.
• W1992029791 cites W2061341025 @default.
• W1992029791 cites W2061829935 @default.
• W1992029791 cites W2068654805 @default.
• W1992029791 cites W2074329878 @default.
• W1992029791 cites W2075956357 @default.
• W1992029791 cites W2079460275 @default.
• W1992029791 cites W2082672358 @default.
• W1992029791 cites W2094231314 @default.
• W1992029791 cites W2102234201 @default.
• W1992029791 cites W2105310668 @default.
• W1992029791 cites W2105511586 @default.
• W1992029791 cites W2107169990 @default.
• W1992029791 cites W2107309024 @default.
• W1992029791 cites W2115878345 @default.
• W1992029791 cites W2119111392 @default.
• W1992029791 cites W2128110973 @default.
• W1992029791 cites W2133071671 @default.
• W1992029791 cites W2137300802 @default.
• W1992029791 cites W2140826376 @default.
• W1992029791 cites W2151597277 @default.
• W1992029791 cites W2155624949 @default.
• W1992029791 cites W2292278295 @default.
• W1992029791 doi "https://doi.org/10.1029/92jb01076" @default.
• W1992029791 hasPublicationYear "1992" @default.
• W1992029791 type Work @default.
• W1992029791 sameAs 1992029791 @default.
• W1992029791 citedByCount "14" @default.
• W1992029791 countsByYear W19920297912014 @default.
• W1992029791 countsByYear W19920297912018 @default.
• W1992029791 crossrefType "journal-article" @default.
• W1992029791 hasAuthorship W1992029791A5026410195 @default.
• W1992029791 hasAuthorship W1992029791A5042187705 @default.
• W1992029791 hasConcept C106973953 @default.
• W1992029791 hasConcept C111368507 @default.
• W1992029791 hasConcept C121332964 @default.
• W1992029791 hasConcept C127313418 @default.
• W1992029791 hasConcept C135628077 @default.
• W1992029791 hasConcept C165205528 @default.
• W1992029791 hasConcept C16942324 @default.
• W1992029791 hasConcept C175551986 @default.
• W1992029791 hasConcept C187320778 @default.
• W1992029791 hasConcept C204366326 @default.
• W1992029791 hasConcept C2778414698 @default.
• W1992029791 hasConcept C2778677506 @default.
• W1992029791 hasConcept C2780012869 @default.
• W1992029791 hasConcept C43369102 @default.
• W1992029791 hasConcept C77928131 @default.
• W1992029791 hasConcept C84786313 @default.
• W1992029791 hasConcept C97355855 @default.
• W1992029791 hasConceptScore W1992029791C106973953 @default.
• W1992029791 hasConceptScore W1992029791C111368507 @default.
• W1992029791 hasConceptScore W1992029791C121332964 @default.
• W1992029791 hasConceptScore W1992029791C127313418 @default.
• W1992029791 hasConceptScore W1992029791C135628077 @default.
• W1992029791 hasConceptScore W1992029791C165205528 @default.
• W1992029791 hasConceptScore W1992029791C16942324 @default.
• W1992029791 hasConceptScore W1992029791C175551986 @default.
• W1992029791 hasConceptScore W1992029791C187320778 @default.
• W1992029791 hasConceptScore W1992029791C204366326 @default.
• W1992029791 hasConceptScore W1992029791C2778414698 @default.

• next