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- W2131485853 abstract "Abstract Trench excavations have provided constraints on the recent paleoseismic history of the northern Horohoro Fault, one of the faults of the Taupo Fault Belt (TFB), a belt of northeast‐striking normal faults that run along the axis of the Taupo Volcanic Zone (TVZ). We excavated two trenches across the northernmost part of the fault where it displaces two Quaternary terraces of different ages. The trench exposures reveal a series of alluvial and volcanic fall deposits, ranging in age from c. 25 to 1.75 ka, that are vertically displaced across the steeply southeast‐dipping fault. The trench data confirm that the fault is active and indicate that it has ruptured at least three times within the last c. 26 000 yr and twice within the last c. 15 700 yr, with an average vertical component of displacement of c. 1.1 m per rupture. The most recent surface rupture occurred between 1750 and 8050 yr ago. Because the fault has ruptured within the last 20 000 yr, we consider it to be part of the modern TFB, the region that accommodates most of the modern extension in the TVZ. The post‐c. 25 ka vertical displacement rate on the northern Horohoro Fault, which runs along the northwest boundary of the TFB, is 0.14–0.2 mm/yr at the trench site, lower than that of many of the faults within the modern TFB. It is unclear if the whole Horohoro Fault or just the northern section is active. If the latter, then the fault may only be accommodating strain associated with a bend or step in the TFB near Rotorua." @default.
- W2131485853 created "2016-06-24" @default.
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- W2131485853 date "2001-09-01" @default.
- W2131485853 modified "2023-10-14" @default.
- W2131485853 title "Paleoseismicity of the northern Horohoro Fault, Taupo Volcanic Zone, New Zealand" @default.
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- W2131485853 doi "https://doi.org/10.1080/00288306.2001.9514946" @default.
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