FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2002140130> ?p ?o ?g. }

• W2002140130 endingPage "274" @default.
• W2002140130 startingPage "263" @default.
• W2002140130 abstract "Landslides influence local slope morphology, affect sediment flux from hillslopes to rivers, and mass wasting in response to tectonics and climate forcing. However, the links between giant, non-catastrophic landslides known as Deep-Seated Gravitational Slope Deformations (DSGSDs) and the long-term evolution of orogenic landscapes are almost unknown. We explore these links in the European Alps using the first orogen-scale inventory of DSGSDs (>900 over an area >105 km2) and a dataset of published apatite fission-track ages (>1000) that provides an estimate of the long-term exhumation patterns of the orogen. We show that DSGSDs are more widespread than previously considered, and exhibit an orogen-scale distribution not explained by well-known local lithological and structural controls. We test the hypothesis that this orogen-scale distribution correlates to the long-term evolution of the Alps by subdividing the study area into 37 square sub-areas (50×50 km), classified according to combinations of long-term exhumation and mean annual rainfall. On each sub-area we perform a morphometric analysis of topography (hypsometry, relief, slope). Excluding local and regional controls due to rock type and structure, DSGSDs tend to cluster in areas with intermediate exhumation rates (fission-track age between 10 and 40 Ma), where large-scale topography is less dissected and incision is localised along major valleys. Here DSGSD abundance correlates positively with the degree of valley incision and related relief. Instead, DSGSDs lack in areas which underwent either low exhumation rates, resulting in insufficient relief production, or high exhumation rates associated to rapid uplift or higher erosional dissection of topography. Negative correlation between DSGSD abundance and mean annual rainfall suggests that effective hydrological surface processes contribute, on the long-term timescale, to the development of large-scale topography unfavourable to DSGSDs, especially in areas of high exhumation rates. Where DSGSDs are abundant, long-lasting slope deformations effectively adjust post-glacial relief by reducing slope inclination values, and are thus expected to significantly contribute to the long-term denudation of active orogens." @default.
• W2002140130 created "2016-06-24" @default.
• W2002140130 creator A5000469045 @default.
• W2002140130 creator A5025868395 @default.
• W2002140130 creator A5047247987 @default.
• W2002140130 creator A5060919376 @default.
• W2002140130 date "2013-03-01" @default.
• W2002140130 modified "2023-10-01" @default.
• W2002140130 title "Giant non-catastrophic landslides and the long-term exhumation of the European Alps" @default.
• W2002140130 cites W1823541180 @default.
• W2002140130 cites W1882234879 @default.
• W2002140130 cites W1929828296 @default.
• W2002140130 cites W1938715807 @default.
• W2002140130 cites W1964122498 @default.
• W2002140130 cites W1964921771 @default.
• W2002140130 cites W1965730105 @default.
• W2002140130 cites W1969942680 @default.
• W2002140130 cites W1969970441 @default.
• W2002140130 cites W1971670210 @default.
• W2002140130 cites W1974230799 @default.
• W2002140130 cites W1977050438 @default.
• W2002140130 cites W1980889991 @default.
• W2002140130 cites W1984123163 @default.
• W2002140130 cites W1985565675 @default.
• W2002140130 cites W1986920683 @default.
• W2002140130 cites W1991436475 @default.
• W2002140130 cites W1993422708 @default.
• W2002140130 cites W2006266078 @default.
• W2002140130 cites W2010786242 @default.
• W2002140130 cites W2012333595 @default.
• W2002140130 cites W2012426996 @default.
• W2002140130 cites W2019367177 @default.
• W2002140130 cites W2024920324 @default.
• W2002140130 cites W2025007742 @default.
• W2002140130 cites W2029130717 @default.
• W2002140130 cites W2030870608 @default.
• W2002140130 cites W2033345860 @default.
• W2002140130 cites W2033928239 @default.
• W2002140130 cites W2036327876 @default.
• W2002140130 cites W2041843560 @default.
• W2002140130 cites W2043184651 @default.
• W2002140130 cites W2043911906 @default.
• W2002140130 cites W2048535129 @default.
• W2002140130 cites W2055161902 @default.
• W2002140130 cites W2059054619 @default.
• W2002140130 cites W2064504230 @default.
• W2002140130 cites W2064505321 @default.
• W2002140130 cites W2064972007 @default.
• W2002140130 cites W2068393938 @default.
• W2002140130 cites W2070868689 @default.
• W2002140130 cites W2071585772 @default.
• W2002140130 cites W2074331670 @default.
• W2002140130 cites W2074489750 @default.
• W2002140130 cites W2075402055 @default.
• W2002140130 cites W2075426128 @default.
• W2002140130 cites W2076744895 @default.
• W2002140130 cites W2082733182 @default.
• W2002140130 cites W2082784698 @default.
• W2002140130 cites W2084138021 @default.
• W2002140130 cites W2084364546 @default.
• W2002140130 cites W2084744129 @default.
• W2002140130 cites W2091472939 @default.
• W2002140130 cites W2091501510 @default.
• W2002140130 cites W2094346571 @default.
• W2002140130 cites W2098496988 @default.
• W2002140130 cites W2104300819 @default.
• W2002140130 cites W2111173422 @default.
• W2002140130 cites W2111403581 @default.
• W2002140130 cites W2116123160 @default.
• W2002140130 cites W2128610717 @default.
• W2002140130 cites W2131621559 @default.
• W2002140130 cites W2132394621 @default.
• W2002140130 cites W2139409798 @default.
• W2002140130 cites W2162607354 @default.
• W2002140130 cites W2166132752 @default.
• W2002140130 cites W2171415071 @default.
• W2002140130 cites W4210964572 @default.
• W2002140130 cites W4254850455 @default.
• W2002140130 cites W52407342 @default.
• W2002140130 cites W636473100 @default.
• W2002140130 doi "https://doi.org/10.1016/j.epsl.2013.01.030" @default.
• W2002140130 hasPublicationYear "2013" @default.
• W2002140130 type Work @default.
• W2002140130 sameAs 2002140130 @default.
• W2002140130 citedByCount "82" @default.
• W2002140130 countsByYear W20021401302013 @default.
• W2002140130 countsByYear W20021401302014 @default.
• W2002140130 countsByYear W20021401302015 @default.
• W2002140130 countsByYear W20021401302016 @default.
• W2002140130 countsByYear W20021401302017 @default.
• W2002140130 countsByYear W20021401302018 @default.
• W2002140130 countsByYear W20021401302019 @default.
• W2002140130 countsByYear W20021401302020 @default.
• W2002140130 countsByYear W20021401302021 @default.
• W2002140130 countsByYear W20021401302022 @default.
• W2002140130 countsByYear W20021401302023 @default.
• W2002140130 crossrefType "journal-article" @default.
• W2002140130 hasAuthorship W2002140130A5000469045 @default.

• next