FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W4367011669> ?p ?o ?g. }

• W4367011669 endingPage "13" @default.
• W4367011669 startingPage "1" @default.
• W4367011669 abstract "The Xianshuihe-Anninghe fault extents SE–S and constitutes the southeastern margin of the Tibetan Plateau. However, the associated Dadu River does not flow following the fault, but makes a 90º turn within a distance of 1 km at Shimian, heading east, and joins the Yangtze River, finally flowing into the East China Sea. Adjacent to the abrupt turn, a low and wide pass near the Daqiao reservoir at Mianning separates the N–S course of the Dadu River from the headwater of the Anning River which then flows south into the Yunnan Province along the Anninghe fault. Therefore, many previous studies assumed southward flow of the paleo-Dadu River from the Shimian to the Anning River. However, evidences for the capture of the integrated N–S paleo-Dadu-Anning River, its timing, and causes are still insufficient. This study explored the paleo-drainage pattern of the Dadu and Anning Rivers based on bulk mineral and geochemical analyses of the large quantities of fluvial/lacustrine sediments along the trunk of the Dadu and Anning Rivers. Similar with sands in the modern Dadu River, the Xigeda sediments also exhibit a granitoid affinity with the bulk major mineral compositions of quartz (>50%), anorthite (about 10%), orthoclase (about 5%), muscovite (about 5%), and clinochlore (about 4%). Correspondingly, bulk major elements show high SiO₂, with all samples >60%, and some of them >70%, low TiO₂ (≤0.75%), P₂O₅ (≤0.55%), FeO* (≤5%), and relatively high CaO (1.02%–8.51%), Na₂O (1.60%–2.52%), and K₂O (2.17%–2.71%), with a uniform REE patterns. Therefore, synthesizing all these results indicate that these lacustrine sediments have similar material sources, which are mainly derived from its course in the Songpan-Ganzi flysch block, implying that the paleo-Dadu originally flowed southward into the Anning River and provided materials to the Xigeda ancient lake. The rearrangement of the paleo-Dadu River appears to be closely related to the locally focused uplift driven by strong activities of the Xianshuihe-Xiaojiang fault system." @default.
• W4367011669 created "2023-04-27" @default.
• W4367011669 creator A5013736647 @default.
• W4367011669 creator A5028655194 @default.
• W4367011669 creator A5045373793 @default.
• W4367011669 creator A5045616519 @default.
• W4367011669 creator A5058811939 @default.
• W4367011669 creator A5074354102 @default.
• W4367011669 date "2023-01-01" @default.
• W4367011669 modified "2023-09-26" @default.
• W4367011669 title "An integrated north–south paleo-Dadu-Anning River: New insights from bulk major and trace element analyses of the Xigeda Formation" @default.
• W4367011669 doi "https://doi.org/10.31035/cg2023027" @default.
• W4367011669 hasPublicationYear "2023" @default.
• W4367011669 type Work @default.
• W4367011669 citedByCount "1" @default.
• W4367011669 countsByYear W43670116692023 @default.
• W4367011669 crossrefType "journal-article" @default.
• W4367011669 hasAuthorship W4367011669A5013736647 @default.
• W4367011669 hasAuthorship W4367011669A5028655194 @default.
• W4367011669 hasAuthorship W4367011669A5045373793 @default.
• W4367011669 hasAuthorship W4367011669A5045616519 @default.
• W4367011669 hasAuthorship W4367011669A5058811939 @default.
• W4367011669 hasAuthorship W4367011669A5074354102 @default.
• W4367011669 hasBestOaLocation W43670116691 @default.
• W4367011669 hasConcept C109007969 @default.
• W4367011669 hasConcept C112959462 @default.
• W4367011669 hasConcept C114793014 @default.
• W4367011669 hasConcept C127313418 @default.
• W4367011669 hasConcept C151730666 @default.
• W4367011669 hasConcept C17409809 @default.
• W4367011669 hasConcept C2776581184 @default.
• W4367011669 hasConcept C2779870107 @default.
• W4367011669 hasConceptScore W4367011669C109007969 @default.
• W4367011669 hasConceptScore W4367011669C112959462 @default.
• W4367011669 hasConceptScore W4367011669C114793014 @default.
• W4367011669 hasConceptScore W4367011669C127313418 @default.
• W4367011669 hasConceptScore W4367011669C151730666 @default.
• W4367011669 hasConceptScore W4367011669C17409809 @default.
• W4367011669 hasConceptScore W4367011669C2776581184 @default.
• W4367011669 hasConceptScore W4367011669C2779870107 @default.
• W4367011669 hasIssue "0" @default.
• W4367011669 hasLocation W43670116691 @default.
• W4367011669 hasOpenAccess W4367011669 @default.
• W4367011669 hasPrimaryLocation W43670116691 @default.
• W4367011669 hasRelatedWork W1678589637 @default.
• W4367011669 hasRelatedWork W2014234281 @default.
• W4367011669 hasRelatedWork W2047380333 @default.
• W4367011669 hasRelatedWork W2080731282 @default.
• W4367011669 hasRelatedWork W2110423347 @default.
• W4367011669 hasRelatedWork W2113927977 @default.
• W4367011669 hasRelatedWork W2181546618 @default.
• W4367011669 hasRelatedWork W3031552867 @default.
• W4367011669 hasRelatedWork W3037686908 @default.
• W4367011669 hasRelatedWork W4385658230 @default.
• W4367011669 hasVolume "6" @default.
• W4367011669 isParatext "false" @default.
• W4367011669 isRetracted "false" @default.
• W4367011669 workType "article" @default.