FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2010718062> ?p ?o ?g. }

• W2010718062 endingPage "330" @default.
• W2010718062 startingPage "315" @default.
• W2010718062 abstract "Because of existing uncertainties as to the influence of errors and non-tectonic movements on releveling estimates of vertical crustal movement, we have taken an empirical approach to investigate some characteristics of the U.S. releveling data base as a whole. Our primary purpose is to establish typical magnitudes of apparent tilt which can serve as a basis for defining anomalous apparent tilts (the term “apparent” is used since differences between levelings can result from errors as well as surface movement). Our analysis is sensitive to apparent tilts with characteristic lengths (i.e. lengths over which tilt is coherent) of 10 to about 70 km, a range which is relevant to many tectonic processes. The apparent tilts developed over a given characteristic length tend to decline as the characteristic length increases. That is the “apparent tilt spectrum” has most “energy” at small spatial wavelengths. For the entire data base the typical magnitudes of apparent tilt for characteristic lengths between 20 and 30 km and between 60 and 70 km are 2.0 and 0.7 μrad respectively. These values are approximately three times larger than the magnitude of apparent tilt expected from random errors. The typical magnitude of apparent tilt averaged over all lengths in the western U.S. (∼- 2.6 μrad) is about 1 μrad higher than that in the east (∼- 1.6 μrad). The largest observed apparent tilts for the entire data base occur along approximately flat routes. For the most part, these large apparent tilts result from real surface movement and are directly associated with sediment compaction due to water withdrawal in flat lying sedimentary areas. While a number of tectonically active areas are characterized by high average apparent tilts, the average magnitude of apparent tilt in releveling data defining the southern California uplift, a feature of much current debate, is not significantly different from that for the entire western U.S. This analysis emphasizes that real surface movements (tectonic and nontectonic) are a significant factor contributing to the high magnitude of apparent tilt relative to random error estimates." @default.
• W2010718062 created "2016-06-24" @default.
• W2010718062 creator A5026396690 @default.
• W2010718062 creator A5069040926 @default.
• W2010718062 creator A5069365402 @default.
• W2010718062 date "1984-08-01" @default.
• W2010718062 modified "2023-09-27" @default.
• W2010718062 title "Tilt from releveling: An overview of the U.S. data base" @default.
• W2010718062 cites W1524236871 @default.
• W2010718062 cites W2020648580 @default.
• W2010718062 cites W2022226656 @default.
• W2010718062 cites W2038095090 @default.
• W2010718062 cites W2040430401 @default.
• W2010718062 cites W2056455274 @default.
• W2010718062 cites W2081619131 @default.
• W2010718062 cites W2124288810 @default.
• W2010718062 cites W2130239837 @default.
• W2010718062 cites W2139776327 @default.
• W2010718062 cites W2157461749 @default.
• W2010718062 cites W2315747755 @default.
• W2010718062 cites W2417546520 @default.
• W2010718062 doi "https://doi.org/10.1016/0040-1951(84)90256-7" @default.
• W2010718062 hasPublicationYear "1984" @default.
• W2010718062 type Work @default.
• W2010718062 sameAs 2010718062 @default.
• W2010718062 citedByCount "9" @default.
• W2010718062 crossrefType "journal-article" @default.
• W2010718062 hasAuthorship W2010718062A5026396690 @default.
• W2010718062 hasAuthorship W2010718062A5069040926 @default.
• W2010718062 hasAuthorship W2010718062A5069365402 @default.
• W2010718062 hasConcept C121332964 @default.
• W2010718062 hasConcept C126691448 @default.
• W2010718062 hasConcept C127313418 @default.
• W2010718062 hasConcept C13280743 @default.
• W2010718062 hasConcept C134306372 @default.
• W2010718062 hasConcept C159985019 @default.
• W2010718062 hasConcept C165205528 @default.
• W2010718062 hasConcept C192562407 @default.
• W2010718062 hasConcept C204323151 @default.
• W2010718062 hasConcept C2524010 @default.
• W2010718062 hasConcept C2779844322 @default.
• W2010718062 hasConcept C33923547 @default.
• W2010718062 hasConcept C42058472 @default.
• W2010718062 hasConcept C44870925 @default.
• W2010718062 hasConcept C77928131 @default.
• W2010718062 hasConceptScore W2010718062C121332964 @default.
• W2010718062 hasConceptScore W2010718062C126691448 @default.
• W2010718062 hasConceptScore W2010718062C127313418 @default.
• W2010718062 hasConceptScore W2010718062C13280743 @default.
• W2010718062 hasConceptScore W2010718062C134306372 @default.
• W2010718062 hasConceptScore W2010718062C159985019 @default.
• W2010718062 hasConceptScore W2010718062C165205528 @default.
• W2010718062 hasConceptScore W2010718062C192562407 @default.
• W2010718062 hasConceptScore W2010718062C204323151 @default.
• W2010718062 hasConceptScore W2010718062C2524010 @default.
• W2010718062 hasConceptScore W2010718062C2779844322 @default.
• W2010718062 hasConceptScore W2010718062C33923547 @default.
• W2010718062 hasConceptScore W2010718062C42058472 @default.
• W2010718062 hasConceptScore W2010718062C44870925 @default.
• W2010718062 hasConceptScore W2010718062C77928131 @default.
• W2010718062 hasIssue "3-4" @default.
• W2010718062 hasLocation W20107180621 @default.
• W2010718062 hasOpenAccess W2010718062 @default.
• W2010718062 hasPrimaryLocation W20107180621 @default.
• W2010718062 hasRelatedWork W1907237374 @default.
• W2010718062 hasRelatedWork W2004013317 @default.
• W2010718062 hasRelatedWork W2022035173 @default.
• W2010718062 hasRelatedWork W2059403730 @default.
• W2010718062 hasRelatedWork W2167517487 @default.
• W2010718062 hasRelatedWork W2188141918 @default.
• W2010718062 hasRelatedWork W2355282060 @default.
• W2010718062 hasRelatedWork W2772196783 @default.
• W2010718062 hasRelatedWork W3113596969 @default.
• W2010718062 hasRelatedWork W3141829427 @default.
• W2010718062 hasVolume "107" @default.
• W2010718062 isParatext "false" @default.
• W2010718062 isRetracted "false" @default.
• W2010718062 magId "2010718062" @default.
• W2010718062 workType "article" @default.