Matches in SemOpenAlex for { <https://semopenalex.org/work/W2389786870> ?p ?o ?g. }
Showing items 1 to 77 of
77
with 100 items per page.
- W2389786870 abstract "The palaeo-ground of the Qijia Culture in the Lajia Ruins was found to be broken by several groups of earthquake fissures.One layer of conglomerated clayey mudflow deposit has blanketed the Lajia Runis and filled with the earthquake fissures.After detailed field observations,samples for OSL dating were taken from the sediment profile.OSL ages of the samples were obtained by using the single-aliquot regenerative-dose method.A chronological framework was established in the XLJ profile based on the OSL ages and in combination with the 14 C ages and stratigraphic correlations,which indicates that the second terrace of the Yellow River was formed at 35.00 ka BP.Then,accumulation of the eolian loess-soil profile started.The red clayey mudflow deposit and the earthquake fissures were formed at 3.95 ka BP in the second terrace in the Guanting Basin.Sedimentary samples were taken from the profile and magnetic susceptibility and particle-size distribution were analyzed in the laboratory.The results show that the Malan loess(L 1-1) was deposited during 35.00~11.50 ka BP.It was accumulated by dust storms and dust falls under a dry-cold environment during the late last glacial without being modified by pedogenesis.The transitional loess(L t) was dated to be 11.50~8.50 ka BP.It was slightly affected by weathering and pedogenesis during the early Holocene because the climate was dry.The palaeosol(S 0),i.e.,Heilusol or Chernozem,was dated to be 8.50~3.10 ka BP.It was strongly affected by weathering and pedogenesis during the mid-Holocene Climatic Optimum.However,a layer of conglomerated red clayey mudflow,which blanketed the Lajia Ruins at 3.95 ka BP,made the palaeosol(S 0) split into two sub-layers(S 0-lower and S 0-upper)." @default.
- W2389786870 created "2016-06-24" @default.
- W2389786870 creator A5050379145 @default.
- W2389786870 date "2013-01-01" @default.
- W2389786870 modified "2023-09-24" @default.
- W2389786870 title "OSL dating of the sediment stratigraphy of the Lajia Ruins in the Guanting Basin in the Upper Yellow River Basin" @default.
- W2389786870 hasPublicationYear "2013" @default.
- W2389786870 type Work @default.
- W2389786870 sameAs 2389786870 @default.
- W2389786870 citedByCount "0" @default.
- W2389786870 crossrefType "journal-article" @default.
- W2389786870 hasAuthorship W2389786870A5050379145 @default.
- W2389786870 hasConcept C105467799 @default.
- W2389786870 hasConcept C109007969 @default.
- W2389786870 hasConcept C112959462 @default.
- W2389786870 hasConcept C114793014 @default.
- W2389786870 hasConcept C127313418 @default.
- W2389786870 hasConcept C140345934 @default.
- W2389786870 hasConcept C151730666 @default.
- W2389786870 hasConcept C159390177 @default.
- W2389786870 hasConcept C159750122 @default.
- W2389786870 hasConcept C17409809 @default.
- W2389786870 hasConcept C180093795 @default.
- W2389786870 hasConcept C184269829 @default.
- W2389786870 hasConcept C185515318 @default.
- W2389786870 hasConcept C186295008 @default.
- W2389786870 hasConcept C206137718 @default.
- W2389786870 hasConcept C2816523 @default.
- W2389786870 hasConcept C40724407 @default.
- W2389786870 hasConcept C6494504 @default.
- W2389786870 hasConcept C76123530 @default.
- W2389786870 hasConceptScore W2389786870C105467799 @default.
- W2389786870 hasConceptScore W2389786870C109007969 @default.
- W2389786870 hasConceptScore W2389786870C112959462 @default.
- W2389786870 hasConceptScore W2389786870C114793014 @default.
- W2389786870 hasConceptScore W2389786870C127313418 @default.
- W2389786870 hasConceptScore W2389786870C140345934 @default.
- W2389786870 hasConceptScore W2389786870C151730666 @default.
- W2389786870 hasConceptScore W2389786870C159390177 @default.
- W2389786870 hasConceptScore W2389786870C159750122 @default.
- W2389786870 hasConceptScore W2389786870C17409809 @default.
- W2389786870 hasConceptScore W2389786870C180093795 @default.
- W2389786870 hasConceptScore W2389786870C184269829 @default.
- W2389786870 hasConceptScore W2389786870C185515318 @default.
- W2389786870 hasConceptScore W2389786870C186295008 @default.
- W2389786870 hasConceptScore W2389786870C206137718 @default.
- W2389786870 hasConceptScore W2389786870C2816523 @default.
- W2389786870 hasConceptScore W2389786870C40724407 @default.
- W2389786870 hasConceptScore W2389786870C6494504 @default.
- W2389786870 hasConceptScore W2389786870C76123530 @default.
- W2389786870 hasLocation W23897868701 @default.
- W2389786870 hasOpenAccess W2389786870 @default.
- W2389786870 hasPrimaryLocation W23897868701 @default.
- W2389786870 hasRelatedWork W1973051377 @default.
- W2389786870 hasRelatedWork W1987493305 @default.
- W2389786870 hasRelatedWork W1993990990 @default.
- W2389786870 hasRelatedWork W2015392340 @default.
- W2389786870 hasRelatedWork W2021864498 @default.
- W2389786870 hasRelatedWork W2046190125 @default.
- W2389786870 hasRelatedWork W2058307246 @default.
- W2389786870 hasRelatedWork W2058689514 @default.
- W2389786870 hasRelatedWork W2078403371 @default.
- W2389786870 hasRelatedWork W2095221530 @default.
- W2389786870 hasRelatedWork W2323838530 @default.
- W2389786870 hasRelatedWork W2767857237 @default.
- W2389786870 hasRelatedWork W2770453784 @default.
- W2389786870 hasRelatedWork W2783651645 @default.
- W2389786870 hasRelatedWork W2802211863 @default.
- W2389786870 hasRelatedWork W2903156079 @default.
- W2389786870 hasRelatedWork W2979092445 @default.
- W2389786870 hasRelatedWork W3011442410 @default.
- W2389786870 hasRelatedWork W3130689337 @default.
- W2389786870 hasRelatedWork W346025193 @default.
- W2389786870 isParatext "false" @default.
- W2389786870 isRetracted "false" @default.
- W2389786870 magId "2389786870" @default.
- W2389786870 workType "article" @default.