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  • 1
    Publication Date: 2021-05-12
    Description: On natural faults that host repeating slip events, the inter‐event loading time is quite large compared to the slip event duration. Since most friction studies focus on steady‐state frictional behavior, the fault loading phase is not typically examined. Here, we employ a method specifically designed to evaluate fault strength evolution during active loading, under shear driving rates as low as 10−10 m/s, on natural fault gouge samples from the Waikukupa Thrust in southern New Zealand. These tests reveal that in the early stages of loading following a slip event, there is a period of increased stability, which fades with accumulated slip. In the framework of rate‐ and state‐dependent friction laws, this temporary stable phase exists as long as slip is less than the critical slip distance and the elapsed time is less than the value of the state variable at steady state. These observations indicate a minimum earthquake recurrence time, which depends on the field value of the critical slip distance and the background slip rate. We compare estimates of minimum earthquake recurrence times with the recurrence times of repeating large earthquakes on the Alpine Fault in southern New Zealand and repeating small‐magnitude earthquakes on the San Andreas Fault system in California. We find that the observed recurrence times are mostly longer than the predicted minimum values, and exceptions in the San Andreas system may be explained by elevated slip rates due to larger earthquakes in this region.
    Description: Deutsche Forschungsgemeinschaft via MARUM Research Centre/Cluster of Excellence (grants FZT15, EXC309, and IK 107/3‐1) and from the European Research Council (ERC) under the European Union's Horizon 2020 research and innovation program (grant agreement 714430) to M. I.
    Description: Published
    Description: e2020JB020015
    Description: 1T. Struttura della Terra
    Description: JCR Journal
    Keywords: Friction ; Fault ; Earthquake physics
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
    Location Call Number Limitation Availability
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  • 2
    Publication Date: 2021-07-21
    Description: Slow slip events (SSEs) are recognized as an important component of plate boundary fault slip, and there is a need for laboratory friction data on natural samples to guide comparisons with natural SSEs. Here, we compile a comprehensive catalog of SSEs observed geodetically at the Hikurangi subduction zone offshore northern New Zealand, and compare it with results of laboratory friction experiments that produce laboratory SSEs under plate tectonic driving rates (5 cm/yr). We use samples from Ocean Drilling Program Site 1124 seaward of the Hikurangi subduction zone to represent the plate boundary that hosts shallow SSEs at Hikurangi. We find that laboratory SSEs exhibit a similar displacement record and range of stress drops as the natural SSEs. Results of velocity step tests, which can be used to evaluate frictional instability based on the critical stiffness criterion, indicate that the slow slip activity at Hikurangi is a form of stably-accelerating slip. Our laboratory SSEs provide an alternative method of quantifying (in)stability by direct measurement of the unloading stiffness during the stress drop. The observed dependence of laboratory SSE parameters on effective normal stress is consistent with critical stiffness theory; however, depth-increasing projections based on laboratory data do not match observations from natural SSEs. These differences are likely related to changing temperature and fault rock composition downdip but also complications related to scaling and/or limited sampling. Scientific drilling recently undertaken at the Hikurangi subduction zone should serve to improve and guide future studies of the role of frictional properties for the occurrence of SSEs.
    Keywords: 551.8 ; Hikurangi ; slow slip ; subduction zone ; friction ; GPS ; fault
    Language: English
    Type: article
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  • 3
    Publication Date: 2024-01-09
    Keywords: 131-808A; 131-808B; 131-808C; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Event label; Illite; Joides Resolution; Leg131; March (1932) model; Ocean Drilling Program; ODP; Philippine Sea; Ratio; Sample code/label
    Type: Dataset
    Format: text/tab-separated-values, 55 data points
    Location Call Number Limitation Availability
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  • 4
    Publication Date: 2024-01-09
    Keywords: 131-808A; 131-808B; 131-808C; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Event label; Intensity; Joides Resolution; Leg131; Method comment; Ocean Drilling Program; ODP; Philippine Sea; Sample code/label
    Type: Dataset
    Format: text/tab-separated-values, 54 data points
    Location Call Number Limitation Availability
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  • 5
    Publication Date: 2024-01-09
    Keywords: 131-808A; 131-808B; 131-808C; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Event label; Fry-technique (Fry 1979); Joides Resolution; Leg131; Ocean Drilling Program; ODP; Philippine Sea; PODI-technique (Unzog 1990); Ratio; Sample code/label; Type; Uniaxial shortening
    Type: Dataset
    Format: text/tab-separated-values, 36 data points
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  • 6
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    PANGAEA
    In:  Supplement to: Behrmann, Jan-Hinrich; Kopf, Achim J (1993): Textures and microfabrics in fine-grained muds and mudstones from Site 808, Nankai accretionary prism. In: Hill, IA; Taira, A; Firth, JV; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 131, 45-56, https://doi.org/10.2973/odp.proc.sr.131.106.1993
    Publication Date: 2024-01-09
    Description: The microfabric of 11 mudrock specimens from ODP Site 808 (Nankai accretionary prism) was quantitatively analyzed using X-ray texture goniometry and optical petrography. The objectives of the study were to learn about rock strain and to detect a component of bulk lateral shortening in the deformation of the mudstones. Strain evaluation is based on the predictions of March theory, and on distortions of initially homogeneous marker particle distributions (the Fry technique). The main results are as follows. The specimens underwent a strain path of progressive flattening, which is closely related to loss of pore space by vertical loading. A component of bulk lateral shortening is detectable in the top 550 mbsf at Site 808, but compared with the amount of uniaxial vertical shortening, its relative magnitude is probably small. Moreover, it cannot be said with confidence whether this is caused by toe contraction of the accretionary wedge or by gravitationally induced downslope movement of the sediment pile. The mudstones examined were deposited in a marine environment with an oxic bottom water column. Micropore collapse is an important fabric building mechanism, but below 400 mbsf its effects are at least partly overridden by recrystallization of smectite. We conclude that mud microfabrics are not very precise deformation gauges, but can be used for rough estimations of strain.
    Keywords: 131-808A; 131-808B; 131-808C; DRILL; Drilling/drill rig; Joides Resolution; Leg131; Ocean Drilling Program; ODP; Philippine Sea
    Type: Dataset
    Format: application/zip, 3 datasets
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