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Ridge preservation following dental extractions is fundamental, preserving the ridge profile for subsequent implant placement and providing a sustained function and esthetics.
In a patient with microstomia, hinge axis approximation, diagnostic casts simulating postextraction alveolar ridge profile, and facial simulation of prosthetic treatment outcome were completed in a 3D, virtual environment.
The aim of this clinical, radiological, and histological study was to evaluate the potential of the use of poly(lactide-co-glycolide) acid (PLGA -coated alloPLGA -coatedpalloplastic preserve the ridge profile while supporting the formation of new BCPe in intact socket defect after tooth extraction.
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The ridge-parallel profile of Kodaira et al. (2010) and the cross-ridge profile of Takahashi et al. (2009) intersect between Chichi-jima and Muko-jima, where the ridge-parallel profile shows a crust of about 10 km thickness, and the cross-ridge profile shows a crust of about 18 km thickness.
The conditions leading to different ridging profiles, e.g., corrugated and ribbed surface profiles, are discussed.
Moreover, although Tokuyama et al. (1986) proposed that the backarc spreading of the Kita-Daito Basin was caused by subduction at the southern edge of the Daito Ridge, our seismic profiles do not contain any distinctive features indicative of subduction.
The prognostic ability of our index based on the 88-gene expression profile in ridge regression Cox hazard model was shown to be independent of other clinical factors in predicting cancer prognosis across two distinct datasets.
To understand the slowest spreading rate, we recall that U0 controls two fundamental properties of a mid-ocean ridge system: the thermal profile of the adjacent lithosphere and the magnitude of asthenospheric strain rates.
According to the characteristics of double row ridge cultivation technique, the profiling elastic press roller (PEPR) was designed.
With the goal of better understanding where weathering is occurring, a toposequence of five soil/regolith profiles from ridge crest to valley bottom in the Mt Lofty Range of South Australia was investigated using whole soil geochemistry, soil exchange pool and soil pore water hydrochemistry; stream water and groundwater hydrochemistry were analysed as well.
To traverse the mountain and control speed, riders lean to engage low-profile ridges on the board's underside.
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