Author reply: ‘Response to: Pleural abnormalities in the Framingham Heart Study: prevalence and CT image features’ by Araki <i>et al</i>

Araki, Toshimitsu; Hunninghake, Gary M.; Christiani, David C.; Hatabu, Hiroto

doi:10.1136/oemed-2017-104823

Cited by 2 publications

(6 citation statements)

References 7 publications

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“…Seafloor measurement techniques are beneficial to better capture offshore slow slip. Direct-path acoustic ranging, ocean bottom pressure sensors, coupled GNSS -acoustic systems, and pore-pressure measurements in boreholes have all proven capable of observing slow slip on offshore faults (Bürgmann and Chadwell, 2014, and references cited therein; Wallace et al, 2016, Araki et al, 2017.…”

Section: Geodetic Observationsmentioning

confidence: 99%

“…3a). Araki et al (2017) used observations of seafloor borehole pressure to document SSEs in this shallow zone, often accompanied by clusters of low-frequency earthquakes. These near-trench slip transients recur every 8 to 15 months and accommodate roughly half of the total plate convergence rate.…”

Section: Geodetic Observationsmentioning

confidence: 99%

“…These near-trench slip transients recur every 8 to 15 months and accommodate roughly half of the total plate convergence rate. Two of these SSEs were dynamically triggered by the 2011 Tohoku-oki and 2016 Kumamoto earthquakes, suggesting the shallow megathrust is mechanically weak (Araki et al, 2017). In 2014, Wallace et al (2016) captured a large shallow SSE on the Hikurangi subduction thrust in New Zealand using a temporary array of ocean bottom pressure sensors and permanent land-based GNSS stations (Fig.…”

Section: Geodetic Observationsmentioning

confidence: 99%

“…Static and dynamic stresses from a mainshock rupture can also lead to triggered postseismic SSEs relieving stress that had already built up during the preceding inter-SSE period (Fig. 3c, Taira et al, 2014, Araki et al, 2017, Wallace et al, 2017. Together with other postseismic relaxation mechanisms, slow slip of either type can enhance static stress changes at large distances from a mainshock and trigger subsequent events (e.g., Hearn et al, 2002, Freed, 2005.…”

Section: Slow Slip the Earthquake Cycle And Earthquake Hazardmentioning

confidence: 99%

“…3, Fig. 5, Wallace et al, 2016, Araki et al, 2017, these most hazardous plate-boundary fault systems justifiably are toppriority targets for future research (McGuire et al, 2017). Recent studies of precursory earthquake swarm activity and reduced seismic velocities in the Gofar transform fault (see Fig.…”

Section: New Frontiers Of Slow-slip Researchmentioning

confidence: 99%

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The geophysics, geology and mechanics of slow fault slip

Bürgmann

2018

Earth and Planetary Science Letters

336

308

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Modern geodetic and seismologic observations describe the behavior of fault slip over a vast range of spatial and temporal scales. Slip at sub-seismogenic speeds is evident from top to bottom of lithospheric faults and plays an important role throughout the earthquake cycle. Where earthquakes and tremor accompany slow slip, they help illuminate the spatiotemporal evolution of fault slip. Geophysical subsurface imaging and geologic field studies provide information about suitable environments of slow slip. In particular, exhumed fault and shear zones from various depths reveal the importance of multiple deformation processes and fault-zone structures. Most geologic examples feature frictionally weak and velocity-strengthening materials, well-developed mineral fabrics, and abundant veining indicative of near-lithostatic fluid pressure. To produce transient slow slip events and tremor, in addition to the presence of high-pressure fluids a heterogeneous fault-zone structure, composition, and/or metamorphic assemblage may be needed. Laboratory and computational models suggest that velocityweakening slip patches smaller than a critical dimension needed for earthquake nucleation will also fail in slow slip events. Changes in fluid pressure or slip ratecan cause a fault to transition between stable and unstable fault slip behavior. Future interdisciplinary investigations of slow fault slip, directly integrating geophysical, geological and modeling investigations, will further improve our understanding of the dynamics of slow slip and aid in providing more accurate earthquake hazard characterizations.

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Section: Geodetic Observationsmentioning

confidence: 99%

Section: Geodetic Observationsmentioning

confidence: 99%

Section: Geodetic Observationsmentioning

confidence: 99%

Section: Slow Slip the Earthquake Cycle And Earthquake Hazardmentioning

confidence: 99%

Section: New Frontiers Of Slow-slip Researchmentioning

confidence: 99%

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The geophysics, geology and mechanics of slow fault slip

Bürgmann

2018

Earth and Planetary Science Letters

336

308

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Computed Tomography- (CT-) Based Virtual Surgery Planning for Spinal Intervertebral Foraminal Assisted Clinical Treatment

Wang

Tang

et al. 2021

Journal of Healthcare Engineering

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With the development of minimally invasive spine concepts and the introduction of new minimally invasive instruments, minimally invasive spine technology, represented by foraminoscopy, has flourished, and percutaneous foraminoscopy has become one of the most reliable minimally invasive procedures for the treatment of lumbar disc herniation. Percutaneous foraminoscopy is a safe and effective minimally invasive spinal endoscopic surgical technique. It fully protects the paravertebral muscles and soft tissues as well as the posterior column structure of the spine, provides precise treatment of the target nucleus pulposus tissue, with the advantages of less surgical trauma, fewer postoperative complications, and rapid postoperative recovery, and is widely promoted and used in clinical practice. In this paper, we can view the location, morphology, structure, alignment, and adjacency relationships by performing coronary, CT, and diagonal reconstruction along the attachment of the yellow ligaments and performing 3D reconstruction or processing techniques after performing CT scans. This allows clinicians to observe the laminoplasty and the stenosis of the vertebral canal in a more intuitive and overall manner. It has clinical significance for the display of the sublaminar spine as well as the physician’s judgment of the disease and the choice of surgery.

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Author reply: ‘Response to: Pleural abnormalities in the Framingham Heart Study: prevalence and CT image features’ by Araki et al

Cited by 2 publications

References 7 publications

The geophysics, geology and mechanics of slow fault slip

The geophysics, geology and mechanics of slow fault slip

Computed Tomography- (CT-) Based Virtual Surgery Planning for Spinal Intervertebral Foraminal Assisted Clinical Treatment

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