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dc.contributor.authorLiu, Z
dc.contributor.authorHan, L
dc.contributor.authorBoulton, Sarah
dc.contributor.authorWu, T
dc.contributor.authorGuo, J
dc.date.accessioned2019-11-22T09:49:14Z
dc.date.issued2020-02-15
dc.identifier.issn0169-555X
dc.identifier.issn1872-695X
dc.identifier.other106974
dc.identifier.urihttp://hdl.handle.net/10026.1/15175
dc.description.abstract

River morphology has been widely used to record and track the transient landscape response to active faulting. Here we evaluate the landscape response to active faulting in the Qianhe Graben of southwest Ordos, China. In this region, it has been difficult to determine the activity of mapped faults because of the presence of thick Quaternary Loess; however, by analysing the presence and distribution of slope-break knickpoints in river longitudinal profiles, the ongoing tectonic uplift of the Qianhe Graben can be investigated. The alignment of vertical-step knickpoints gives a new insight into the location of an active fault on the southern margin of Qianhe Graben. Additionally, slope-break knickpoints, typical of fault controlled landscape change, were identified from 24 river longitudinal profiles that drain across normal faults along both graben margins. Along strike from north to south, the knickpoints varied systematically with relief, and the height of the knickpoints also decrease to the southeast. Indicating that the rate of motion on the faults, likely is greater in the northwest and decays southeastwards. The horizontal knickpoint retreat rates range from 0.3 to 27.3 mm/yr, constraining the landscape response time with fault initiation at 1.2–1.4 Myr. In comparison with other studies, the knickpoint recession triggered by base-level fall as a result of faulting is relatively lower than when the base-level fall is the result of sea-level fall potentially the result of different mechanism of retreat. Finally, the potential for earthquakes along the Taoyuan-Guichuansi Fault (TGF) before and after fault linkage was assessed, indicating the potential for earthquakes of Mw of 6.3–6.7 and 6.8–7.0, respectively. These observations not only suggest the knickpoints are recording fault evolution in Qianhe Graben, but also provide information on seismic hazard in this populous region.

dc.format.extent106974-106974
dc.languageen
dc.language.isoen
dc.publisherElsevier
dc.subjectQianhe Graben
dc.subjectKnickpoint
dc.subjectActive faulting
dc.subjectTransient landform response
dc.titleQuantifying the transient landscape response to active faulting using fluvial geomorphic analysis in the Qianhe Graben on the southwest margin of Ordos, China
dc.typejournal-article
dc.typeJournal Article
plymouth.author-urlhttps://www.webofscience.com/api/gateway?GWVersion=2&SrcApp=PARTNER_APP&SrcAuth=LinksAMR&KeyUT=WOS:000514254300018&DestLinkType=FullRecord&DestApp=ALL_WOS&UsrCustomerID=11bb513d99f797142bcfeffcc58ea008
plymouth.volume351
plymouth.publication-statusPublished
plymouth.journalGeomorphology
dc.identifier.doi10.1016/j.geomorph.2019.106974
plymouth.organisational-group/Plymouth
plymouth.organisational-group/Plymouth/Faculty of Science and Engineering
plymouth.organisational-group/Plymouth/Faculty of Science and Engineering/School of Geography, Earth and Environmental Sciences
plymouth.organisational-group/Plymouth/REF 2021 Researchers by UoA
plymouth.organisational-group/Plymouth/REF 2021 Researchers by UoA/UoA07 Earth Systems and Environmental Sciences
plymouth.organisational-group/Plymouth/Users by role
plymouth.organisational-group/Plymouth/Users by role/Academics
dcterms.dateAccepted2019-11-21
dc.rights.embargodate2020-11-21
dc.identifier.eissn1872-695X
dc.rights.embargoperiodNot known
rioxxterms.versionAccepted Manuscript
rioxxterms.versionofrecord10.1016/j.geomorph.2019.106974
rioxxterms.licenseref.urihttp://www.rioxx.net/licenses/all-rights-reserved
rioxxterms.licenseref.startdate2020-02-15
rioxxterms.typeJournal Article/Review


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