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• W2330734504 abstract "Research Article| May 01, 2013 Timing of late Holocene paleoearthquakes on the Hurunui segment of the Hope fault: Implications for plate boundary strain release through South Island, New Zealand Robert M. Langridge; Robert M. Langridge † 1Department of Active Landscapes, GNS Science, P.O. Box 30-368, Lower Hutt, New Zealand †E-mail: r.langridge@gns.cri.nz Search for other works by this author on: GSW Google Scholar Peter C. Almond; Peter C. Almond 2Department of Soil Science, Lincoln University, P.O. Box 84, Lincoln 7647, Canterbury, New Zealand Search for other works by this author on: GSW Google Scholar Richard P. Duncan Richard P. Duncan 3Bio-Protection Research Centre, Lincoln University, P.O. Box 84, Lincoln 7647, Canterbury, New Zealand Search for other works by this author on: GSW Google Scholar Author and Article Information Robert M. Langridge † 1Department of Active Landscapes, GNS Science, P.O. Box 30-368, Lower Hutt, New Zealand Peter C. Almond 2Department of Soil Science, Lincoln University, P.O. Box 84, Lincoln 7647, Canterbury, New Zealand Richard P. Duncan 3Bio-Protection Research Centre, Lincoln University, P.O. Box 84, Lincoln 7647, Canterbury, New Zealand †E-mail: r.langridge@gns.cri.nz Publisher: Geological Society of America Received: 22 Jan 2012 Revision Received: 31 Jul 2012 Accepted: 22 Aug 2012 First Online: 08 Mar 2017 Online ISSN: 1943-2674 Print ISSN: 0016-7606 © 2013 Geological Society of America GSA Bulletin (2013) 125 (5-6): 756–775. https://doi.org/10.1130/B30674.1 Article history Received: 22 Jan 2012 Revision Received: 31 Jul 2012 Accepted: 22 Aug 2012 First Online: 08 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn Email Permissions Search Site Citation Robert M. Langridge, Peter C. Almond, Richard P. Duncan; Timing of late Holocene paleoearthquakes on the Hurunui segment of the Hope fault: Implications for plate boundary strain release through South Island, New Zealand. GSA Bulletin 2013;; 125 (5-6): 756–775. doi: https://doi.org/10.1130/B30674.1 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 SocietyGSA Bulletin Search Advanced Search Abstract The Hurunui segment of the dextral-slip Hope fault extends for ∼42 km between the Hope and Hurunui River catchments and westward to Harper Pass at the Main Divide of South Island. We conducted paleoseismic, soil, and landscape dating studies in the upper Hurunui valley to determine the timing of past earthquake ruptures along this geometric fault segment. On a late Holocene alluvial surface at Matagouri Flat, a young channel system is displaced dextrally by ∼4.5 ± 0.6 m, which is attributed to the most recent faulting event. A trench and soil pits excavated nearby yield evidence for the timing of the last two surface-faulting events. These events, dated from a combination of radiocarbon dates, relative soil, tree, and historical constraints, modified within an OxCal analysis, occurred at ca. A.D. 1655–1835 and 1425–1625. The occurrence of two rupture events during the last ∼600 yr is consistent with previous estimates stating a short recurrence interval for the Hurunui segment. The most recent faulting event in our trenches predates the historic 1888 North Canterbury (Amuri) earthquake, which ruptured the Hope River segment to the east. A comparison of the record from the Hurunui segment with paleoseismic records from other segments along the Hope fault zone indicates evidence for two or three rupture events within the last 700–900 yr. Within the age resolution of the current dates, the data suggest that along-strike rupture occurred along the majority of the Hope fault zone between 120 and 360 yr ago (i.e., A.D. 1650–1888), and may all postdate the most recent rupture of the Alpine fault in ca. A.D. 1717. In addition, the timings of penultimate faulting events along the Hurunui, Hope River, and Conway segments and the Hanmer fault all fall in the range ∼400–700 yr ago. These preliminary observations indicate that rupture of segments of the Hope fault, and indeed the Alpine fault, could occur as clusters that are years to decades apart. Rupture of the major plate boundary faults in the northern South Island may therefore occur in sequences that are enhanced, or even retarded, by stress triggering and fault interactions. You do not have access to this content, please speak to your institutional administrator if you feel you should have access." @default.
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• W2330734504 title "Timing of late Holocene paleoearthquakes on the Hurunui segment of the Hope fault: Implications for plate boundary strain release through South Island, New Zealand" @default.
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