FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2895840141> ?p ?o ?g. }

• W2895840141 endingPage "978" @default.
• W2895840141 startingPage "975" @default.
• W2895840141 abstract "Research Article| October 08, 2018 Erosion of the Southern Alps of New Zealand during the last deglaciation Ruohong Jiao; Ruohong Jiao 1Institute of Earth Surface Dynamics, University of Lausanne, 1015 Lausanne, Switzerland2Department of Geological and Environmental Sciences, Ben-Gurion University of the Negev, Beer-Sheva 8410501, Israel3Helmholtz Centre Potsdam, GFZ German Research Centre for Geosciences, Telegrafenberg, 14473 Potsdam, Germany Search for other works by this author on: GSW Google Scholar Frédéric Herman; Frédéric Herman 1Institute of Earth Surface Dynamics, University of Lausanne, 1015 Lausanne, Switzerland Search for other works by this author on: GSW Google Scholar Olivier Beyssac; Olivier Beyssac 4Institut de Minéralogie, de Physique des Matériaux, et de Cosmochimie, UMR CNRS 7590, Sorbonne Universités–Université Pierre et Marie Curie, 75005 Paris, France Search for other works by this author on: GSW Google Scholar Thierry Adatte; Thierry Adatte 5Institute of Earth Sciences, University of Lausanne, 1015 Lausanne, Switzerland Search for other works by this author on: GSW Google Scholar Simon C. Cox; Simon C. Cox 6GNS Science, Private Bag 1930, Dunedin 9054, New Zealand Search for other works by this author on: GSW Google Scholar Faye E. Nelson; Faye E. Nelson 7Department of Marine Science, University of Otago, P.O. Box 56, Dunedin 9054, New Zealand Search for other works by this author on: GSW Google Scholar Helen L. Neil Helen L. Neil 8National Institute of Water and Atmospheric Research, Private Bag 14901, Wellington 6021, New Zealand Search for other works by this author on: GSW Google Scholar Author and Article Information Ruohong Jiao 1Institute of Earth Surface Dynamics, University of Lausanne, 1015 Lausanne, Switzerland2Department of Geological and Environmental Sciences, Ben-Gurion University of the Negev, Beer-Sheva 8410501, Israel3Helmholtz Centre Potsdam, GFZ German Research Centre for Geosciences, Telegrafenberg, 14473 Potsdam, Germany Frédéric Herman 1Institute of Earth Surface Dynamics, University of Lausanne, 1015 Lausanne, Switzerland Olivier Beyssac 4Institut de Minéralogie, de Physique des Matériaux, et de Cosmochimie, UMR CNRS 7590, Sorbonne Universités–Université Pierre et Marie Curie, 75005 Paris, France Thierry Adatte 5Institute of Earth Sciences, University of Lausanne, 1015 Lausanne, Switzerland Simon C. Cox 6GNS Science, Private Bag 1930, Dunedin 9054, New Zealand Faye E. Nelson 7Department of Marine Science, University of Otago, P.O. Box 56, Dunedin 9054, New Zealand Helen L. Neil 8National Institute of Water and Atmospheric Research, Private Bag 14901, Wellington 6021, New Zealand Publisher: Geological Society of America Received: 17 May 2018 Revision Received: 02 Aug 2018 Accepted: 06 Sep 2018 First Online: 08 Oct 2018 Online Issn: 1943-2682 Print Issn: 0091-7613 © 2018 Geological Society of America Geology (2018) 46 (11): 975–978. https://doi.org/10.1130/G45160.1 Article history Received: 17 May 2018 Revision Received: 02 Aug 2018 Accepted: 06 Sep 2018 First Online: 08 Oct 2018 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation Ruohong Jiao, Frédéric Herman, Olivier Beyssac, Thierry Adatte, Simon C. Cox, Faye E. Nelson, Helen L. Neil; Erosion of the Southern Alps of New Zealand during the last deglaciation. Geology 2018;; 46 (11): 975–978. doi: https://doi.org/10.1130/G45160.1 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyGeology Search Advanced Search Abstract During the Quaternary, periodic glaciations transformed mountain landscapes. However, characterizing the way in which mountain erosion changes between glacier- and river-dominated conditions has been elusive. Here, using samples from an offshore sedimentary core, we estimated the spatial distribution of erosion in the southern part of the Southern Alps of New Zealand during a full transition from the Last Glacial Maximum (LGM), ca. 20 ka, to the last millennium. Raman spectroscopy analyses of carbonaceous material revealed a marked change in the sediment provenance, which we interpreted to reflect the evolving erosion pattern of the mountain range. Over the Holocene, since at least ca. 9 ka, erosion was focused on the chlorite zone schist within the upper reaches of the valleys (>15–20 km distance from the mountain front), possibly dominated by large-magnitude landslides. During the last glaciation, the proportion of sediments from the biotite schist and higher-grade metamorphic rocks in the lower-lying areas closer to the mountain front (<15–20 km) was relatively higher, probably as a result of glacier carving. Our results suggest that glacier retreat during the last deglaciation caused an upstream localization of the high erosion rates, which is consistent with the snowline records in the Southern Alps and regional and global climate histories. You do not have access to this content, please speak to your institutional administrator if you feel you should have access." @default.
• W2895840141 created "2018-10-26" @default.
• W2895840141 creator A5024159600 @default.
• W2895840141 creator A5033878600 @default.
• W2895840141 creator A5038246107 @default.
• W2895840141 creator A5041029530 @default.
• W2895840141 creator A5052768032 @default.
• W2895840141 creator A5058061052 @default.
• W2895840141 creator A5075110863 @default.
• W2895840141 date "2018-10-08" @default.
• W2895840141 modified "2023-10-14" @default.
• W2895840141 title "Erosion of the Southern Alps of New Zealand during the last deglaciation" @default.
• W2895840141 cites W1489510501 @default.
• W2895840141 cites W1532026954 @default.
• W2895840141 cites W182155117 @default.
• W2895840141 cites W1919802293 @default.
• W2895840141 cites W1936621377 @default.
• W2895840141 cites W1960465926 @default.
• W2895840141 cites W1971492950 @default.
• W2895840141 cites W1987470663 @default.
• W2895840141 cites W1991359619 @default.
• W2895840141 cites W2033340258 @default.
• W2895840141 cites W2039380582 @default.
• W2895840141 cites W2049830390 @default.
• W2895840141 cites W2053982496 @default.
• W2895840141 cites W2059054619 @default.
• W2895840141 cites W2076744895 @default.
• W2895840141 cites W2092805274 @default.
• W2895840141 cites W2096717450 @default.
• W2895840141 cites W2129419016 @default.
• W2895840141 cites W2136551514 @default.
• W2895840141 cites W2143340696 @default.
• W2895840141 cites W2145428023 @default.
• W2895840141 cites W2147357873 @default.
• W2895840141 cites W2160085328 @default.
• W2895840141 cites W2161480748 @default.
• W2895840141 cites W2163958438 @default.
• W2895840141 cites W2164790200 @default.
• W2895840141 cites W2165064016 @default.
• W2895840141 cites W2235929395 @default.
• W2895840141 cites W2319342235 @default.
• W2895840141 cites W2585560985 @default.
• W2895840141 doi "https://doi.org/10.1130/g45160.1" @default.
• W2895840141 hasPublicationYear "2018" @default.
• W2895840141 type Work @default.
• W2895840141 sameAs 2895840141 @default.
• W2895840141 citedByCount "7" @default.
• W2895840141 countsByYear W28958401412020 @default.
• W2895840141 countsByYear W28958401412021 @default.
• W2895840141 countsByYear W28958401412022 @default.
• W2895840141 countsByYear W28958401412023 @default.
• W2895840141 crossrefType "journal-article" @default.
• W2895840141 hasAuthorship W2895840141A5024159600 @default.
• W2895840141 hasAuthorship W2895840141A5033878600 @default.
• W2895840141 hasAuthorship W2895840141A5038246107 @default.
• W2895840141 hasAuthorship W2895840141A5041029530 @default.
• W2895840141 hasAuthorship W2895840141A5052768032 @default.
• W2895840141 hasAuthorship W2895840141A5058061052 @default.
• W2895840141 hasAuthorship W2895840141A5075110863 @default.
• W2895840141 hasBestOaLocation W28958401412 @default.
• W2895840141 hasConcept C105639569 @default.
• W2895840141 hasConcept C127313418 @default.
• W2895840141 hasConcept C140345934 @default.
• W2895840141 hasConcept C144133560 @default.
• W2895840141 hasConcept C161191863 @default.
• W2895840141 hasConcept C166957645 @default.
• W2895840141 hasConcept C180705331 @default.
• W2895840141 hasConcept C2910001868 @default.
• W2895840141 hasConcept C2993243194 @default.
• W2895840141 hasConcept C41008148 @default.
• W2895840141 hasConcept C52119013 @default.
• W2895840141 hasConcept C95457728 @default.
• W2895840141 hasConceptScore W2895840141C105639569 @default.
• W2895840141 hasConceptScore W2895840141C127313418 @default.
• W2895840141 hasConceptScore W2895840141C140345934 @default.
• W2895840141 hasConceptScore W2895840141C144133560 @default.
• W2895840141 hasConceptScore W2895840141C161191863 @default.
• W2895840141 hasConceptScore W2895840141C166957645 @default.
• W2895840141 hasConceptScore W2895840141C180705331 @default.
• W2895840141 hasConceptScore W2895840141C2910001868 @default.
• W2895840141 hasConceptScore W2895840141C2993243194 @default.
• W2895840141 hasConceptScore W2895840141C41008148 @default.
• W2895840141 hasConceptScore W2895840141C52119013 @default.
• W2895840141 hasConceptScore W2895840141C95457728 @default.
• W2895840141 hasIssue "11" @default.
• W2895840141 hasLocation W28958401411 @default.
• W2895840141 hasLocation W28958401412 @default.
• W2895840141 hasLocation W28958401413 @default.
• W2895840141 hasLocation W28958401414 @default.
• W2895840141 hasLocation W28958401415 @default.
• W2895840141 hasOpenAccess W2895840141 @default.
• W2895840141 hasPrimaryLocation W28958401411 @default.
• W2895840141 hasRelatedWork W1963873591 @default.
• W2895840141 hasRelatedWork W1974179861 @default.
• W2895840141 hasRelatedWork W2003683093 @default.
• W2895840141 hasRelatedWork W2005657131 @default.
• W2895840141 hasRelatedWork W2055019155 @default.
• W2895840141 hasRelatedWork W2083990288 @default.

• next