FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2021121970> ?p ?o ?g. }

• W2021121970 endingPage "422" @default.
• W2021121970 startingPage "411" @default.
• W2021121970 abstract "Breakouts observed in a vertical borehole (C0002A) drilled through two major tectonic sedimentary formations consisting of forearc basin (upper) and accretionary prism (lower) sediments in the Nankai accretionary wedge, Japan, exhibit distinctive geometric features in respective formations. Breakouts in the lower accretionary prism sediments are markedly wider than those in the forearc basin sediments, and breakout azimuths in the two units are horizontally rotated relative to one another. Breakout azimuths are widely used as a proxy for the determination of principal stress directions. However, strength anisotropies related to the presence of bedding planes may affect both breakout azimuths and widths, which can result in misleading in situ stress interpretations. While thinly bedded mudstones are the dominant lithology in both the forearc basin and accretionary prism sediments, bedding planes in the accretionary prism sediments are relatively steeper than those in the forearc basin sediments, with possible implications for breakout geometry and interpretations of principal stress directions. To investigate the effects of bedding planes on breakout geometry (azimuth and width), we conducted borehole wall failure analyses using a weak-plane failure model that incorporates material strength anisotropies. The model results show that breakout widths and orientations are strongly affected by steeply dipping (>40°) bedding planes in cases where dip directions are unaligned with the principal stress orientation. Our theoretical results suggest that variations in breakout azimuths in the C0002A site may be associated with bedding plane related strength anisotropy, and not associated with the rotation of stress field. That is, stress orientation is consistent throughout the borehole (down to the bottom-hole depth of 1495 m below sea floor). In addition, disregarding the effects of bedding planes tends to yield an overestimation of in situ stress magnitude." @default.
• W2021121970 created "2016-06-24" @default.
• W2021121970 creator A5027217124 @default.
• W2021121970 creator A5027635571 @default.
• W2021121970 creator A5060147373 @default.
• W2021121970 creator A5075886726 @default.
• W2021121970 date "2013-12-01" @default.
• W2021121970 modified "2023-10-18" @default.
• W2021121970 title "Effect of anisotropic borehole wall failures when estimating in situ stresses: A case study in the Nankai accretionary wedge" @default.
• W2021121970 cites W1537905573 @default.
• W2021121970 cites W1625840933 @default.
• W2021121970 cites W1982874765 @default.
• W2021121970 cites W1985085998 @default.
• W2021121970 cites W1993061931 @default.
• W2021121970 cites W1997271048 @default.
• W2021121970 cites W2001334743 @default.
• W2021121970 cites W2006027570 @default.
• W2021121970 cites W2018363314 @default.
• W2021121970 cites W2019877689 @default.
• W2021121970 cites W2027181922 @default.
• W2021121970 cites W2035630376 @default.
• W2021121970 cites W2035931273 @default.
• W2021121970 cites W2041307537 @default.
• W2021121970 cites W2041643909 @default.
• W2021121970 cites W2042599657 @default.
• W2021121970 cites W2046965708 @default.
• W2021121970 cites W2050355706 @default.
• W2021121970 cites W2054300000 @default.
• W2021121970 cites W2058871289 @default.
• W2021121970 cites W2060354120 @default.
• W2021121970 cites W2069080412 @default.
• W2021121970 cites W2074899401 @default.
• W2021121970 cites W2076673261 @default.
• W2021121970 cites W2077291550 @default.
• W2021121970 cites W2080602806 @default.
• W2021121970 cites W2083678379 @default.
• W2021121970 cites W2102114010 @default.
• W2021121970 cites W2106545196 @default.
• W2021121970 cites W2113163803 @default.
• W2021121970 cites W2120899807 @default.
• W2021121970 cites W2125792403 @default.
• W2021121970 cites W2147880216 @default.
• W2021121970 cites W2151289207 @default.
• W2021121970 cites W2155856691 @default.
• W2021121970 cites W4247457893 @default.
• W2021121970 doi "https://doi.org/10.1016/j.marpetgeo.2013.09.004" @default.
• W2021121970 hasPublicationYear "2013" @default.
• W2021121970 type Work @default.
• W2021121970 sameAs 2021121970 @default.
• W2021121970 citedByCount "31" @default.
• W2021121970 countsByYear W20211219702015 @default.
• W2021121970 countsByYear W20211219702016 @default.
• W2021121970 countsByYear W20211219702017 @default.
• W2021121970 countsByYear W20211219702018 @default.
• W2021121970 countsByYear W20211219702019 @default.
• W2021121970 countsByYear W20211219702020 @default.
• W2021121970 countsByYear W20211219702021 @default.
• W2021121970 countsByYear W20211219702022 @default.
• W2021121970 countsByYear W20211219702023 @default.
• W2021121970 crossrefType "journal-article" @default.
• W2021121970 hasAuthorship W2021121970A5027217124 @default.
• W2021121970 hasAuthorship W2021121970A5027635571 @default.
• W2021121970 hasAuthorship W2021121970A5060147373 @default.
• W2021121970 hasAuthorship W2021121970A5075886726 @default.
• W2021121970 hasConcept C10138342 @default.
• W2021121970 hasConcept C121332964 @default.
• W2021121970 hasConcept C127313418 @default.
• W2021121970 hasConcept C144027150 @default.
• W2021121970 hasConcept C150560799 @default.
• W2021121970 hasConcept C155954305 @default.
• W2021121970 hasConcept C162324750 @default.
• W2021121970 hasConcept C165205528 @default.
• W2021121970 hasConcept C17409809 @default.
• W2021121970 hasConcept C187320778 @default.
• W2021121970 hasConcept C2524010 @default.
• W2021121970 hasConcept C2777232088 @default.
• W2021121970 hasConcept C2778091849 @default.
• W2021121970 hasConcept C33923547 @default.
• W2021121970 hasConcept C44140439 @default.
• W2021121970 hasConcept C47422493 @default.
• W2021121970 hasConcept C58097730 @default.
• W2021121970 hasConcept C5900021 @default.
• W2021121970 hasConcept C62520636 @default.
• W2021121970 hasConcept C6494504 @default.
• W2021121970 hasConcept C77928131 @default.
• W2021121970 hasConcept C85725439 @default.
• W2021121970 hasConcept C86803240 @default.
• W2021121970 hasConcept C94436079 @default.
• W2021121970 hasConceptScore W2021121970C10138342 @default.
• W2021121970 hasConceptScore W2021121970C121332964 @default.
• W2021121970 hasConceptScore W2021121970C127313418 @default.
• W2021121970 hasConceptScore W2021121970C144027150 @default.
• W2021121970 hasConceptScore W2021121970C150560799 @default.
• W2021121970 hasConceptScore W2021121970C155954305 @default.
• W2021121970 hasConceptScore W2021121970C162324750 @default.
• W2021121970 hasConceptScore W2021121970C165205528 @default.
• W2021121970 hasConceptScore W2021121970C17409809 @default.
• W2021121970 hasConceptScore W2021121970C187320778 @default.

• next