FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2884865185> ?p ?o ?g. }

• W2884865185 endingPage "2348" @default.
• W2884865185 startingPage "2341" @default.
• W2884865185 abstract "Abstract. An accurate chronology is the essential first step for a sound understanding of ice core records. However, dating ice cores drilled from the high-elevation glaciers is challenging and often problematic, leading to great uncertainties. The Guliya ice core, drilled to the bedrock (308.6 m in length) along the western Kunlun Mountains on the north-western Tibetan Plateau (TP) and widely used as a benchmark for palaeoclimate research, is believed to reach >500 ka (thousand years) at its bottom. Meanwhile other Tibetan ice cores (i.e. Dasuopu and East Rongbuk in the Himalayas, Puruogangri in the central TP and Dunde in the north-eastern TP) are mostly of Holocene origin. In this study, we drilled four ice cores into bedrock (216.6, 208.6, 135.8 and 133.8 m in length, respectively) from the Chongce ice cap ∼30 km to the Guliya ice core drilling site. We took measurements of 14C, 210Pb, tritium and β activity for the ice cores, and used these values in a two-parameter flow model to establish the ice core depth–age relationship. We suggested that the Chongce ice cores might be of Holocene origin, consistent with the other Tibetan ice cores except Guliya. The remarkable discrepancy between the Guliya and all the other Tibetan ice core chronology implies that more effort is necessary to explore multiple dating techniques to confirm the age ranges of the TP glaciers, including those from Chongce and Guliya." @default.
• W2884865185 created "2018-08-03" @default.
• W2884865185 creator A5009158797 @default.
• W2884865185 creator A5022509108 @default.
• W2884865185 creator A5027348502 @default.
• W2884865185 creator A5066590225 @default.
• W2884865185 creator A5071641429 @default.
• W2884865185 creator A5071897789 @default.
• W2884865185 creator A5073607488 @default.
• W2884865185 creator A5087169565 @default.
• W2884865185 date "2018-07-16" @default.
• W2884865185 modified "2023-10-14" @default.
• W2884865185 title "Age ranges of the Tibetan ice cores with emphasis on the Chongce ice cores, western Kunlun Mountains" @default.
• W2884865185 cites W1644167798 @default.
• W2884865185 cites W1774412088 @default.
• W2884865185 cites W1967851076 @default.
• W2884865185 cites W1980743935 @default.
• W2884865185 cites W2001629141 @default.
• W2884865185 cites W2009877158 @default.
• W2884865185 cites W2037047850 @default.
• W2884865185 cites W2044337251 @default.
• W2884865185 cites W2049491558 @default.
• W2884865185 cites W2095942571 @default.
• W2884865185 cites W2096484028 @default.
• W2884865185 cites W2108848995 @default.
• W2884865185 cites W2119986263 @default.
• W2884865185 cites W2124965732 @default.
• W2884865185 cites W2126815914 @default.
• W2884865185 cites W2137286731 @default.
• W2884865185 cites W2140309430 @default.
• W2884865185 cites W2146673202 @default.
• W2884865185 cites W2158503926 @default.
• W2884865185 cites W2168566790 @default.
• W2884865185 cites W2172010105 @default.
• W2884865185 cites W2472665633 @default.
• W2884865185 cites W2512727626 @default.
• W2884865185 cites W2526971270 @default.
• W2884865185 cites W2565939490 @default.
• W2884865185 cites W2613577641 @default.
• W2884865185 cites W2792366294 @default.
• W2884865185 cites W4249751050 @default.
• W2884865185 doi "https://doi.org/10.5194/tc-12-2341-2018" @default.
• W2884865185 hasPublicationYear "2018" @default.
• W2884865185 type Work @default.
• W2884865185 sameAs 2884865185 @default.
• W2884865185 citedByCount "32" @default.
• W2884865185 countsByYear W28848651852019 @default.
• W2884865185 countsByYear W28848651852020 @default.
• W2884865185 countsByYear W28848651852021 @default.
• W2884865185 countsByYear W28848651852022 @default.
• W2884865185 countsByYear W28848651852023 @default.
• W2884865185 crossrefType "journal-article" @default.
• W2884865185 hasAuthorship W2884865185A5009158797 @default.
• W2884865185 hasAuthorship W2884865185A5022509108 @default.
• W2884865185 hasAuthorship W2884865185A5027348502 @default.
• W2884865185 hasAuthorship W2884865185A5066590225 @default.
• W2884865185 hasAuthorship W2884865185A5071641429 @default.
• W2884865185 hasAuthorship W2884865185A5071897789 @default.
• W2884865185 hasAuthorship W2884865185A5073607488 @default.
• W2884865185 hasAuthorship W2884865185A5087169565 @default.
• W2884865185 hasBestOaLocation W28848651851 @default.
• W2884865185 hasConcept C100834320 @default.
• W2884865185 hasConcept C100970517 @default.
• W2884865185 hasConcept C127313418 @default.
• W2884865185 hasConcept C134306372 @default.
• W2884865185 hasConcept C136894858 @default.
• W2884865185 hasConcept C137527640 @default.
• W2884865185 hasConcept C140345934 @default.
• W2884865185 hasConcept C151730666 @default.
• W2884865185 hasConcept C160464908 @default.
• W2884865185 hasConcept C181536285 @default.
• W2884865185 hasConcept C197435368 @default.
• W2884865185 hasConcept C205325660 @default.
• W2884865185 hasConcept C205649164 @default.
• W2884865185 hasConcept C2780030769 @default.
• W2884865185 hasConcept C33923547 @default.
• W2884865185 hasConcept C49204034 @default.
• W2884865185 hasConcept C81820708 @default.
• W2884865185 hasConceptScore W2884865185C100834320 @default.
• W2884865185 hasConceptScore W2884865185C100970517 @default.
• W2884865185 hasConceptScore W2884865185C127313418 @default.
• W2884865185 hasConceptScore W2884865185C134306372 @default.
• W2884865185 hasConceptScore W2884865185C136894858 @default.
• W2884865185 hasConceptScore W2884865185C137527640 @default.
• W2884865185 hasConceptScore W2884865185C140345934 @default.
• W2884865185 hasConceptScore W2884865185C151730666 @default.
• W2884865185 hasConceptScore W2884865185C160464908 @default.
• W2884865185 hasConceptScore W2884865185C181536285 @default.
• W2884865185 hasConceptScore W2884865185C197435368 @default.
• W2884865185 hasConceptScore W2884865185C205325660 @default.
• W2884865185 hasConceptScore W2884865185C205649164 @default.
• W2884865185 hasConceptScore W2884865185C2780030769 @default.
• W2884865185 hasConceptScore W2884865185C33923547 @default.
• W2884865185 hasConceptScore W2884865185C49204034 @default.
• W2884865185 hasConceptScore W2884865185C81820708 @default.
• W2884865185 hasIssue "7" @default.
• W2884865185 hasLocation W28848651851 @default.
• W2884865185 hasLocation W28848651852 @default.

• next