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Bleeding is commonly used to quantify the degree of subsidence for CLSM and was measured in this study according to ASTM C 232.
Clift et al. (2015) estimated the amount of subsidence that would be anticipated based on the degree of subsidence that occurred prior to the onset of seafloor spreading, which would normally be considered the syn-rift period (>30 Ma).
However, if the degree of subsidence is much higher than would be predicted then thermal models may be in error because the mantle lithosphere may not be as extended as the lower crust, resulting in thermal models that over-predict heatflow.
However, in accordance with the previous studies on the ABG-I, our results with the ABG-II stem showed a median degree of subsidence of 0.17 mm (at 2 years) in patients with normal BMD.
The radiographs taken immediately after the index operation were compared with those at follow-up examination in order to classify the restoration of the proximal part of the femur and the degree of subsidence.
We found a slightly higher degree of subsidence, retroversion, and posterior translation of the Charnley flanged 40 femoral component than was found in a previous study from our institution (Hallan et al. 2006).
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The degree of subsidence-related damage in different mining regions varies due to the geological and hydrogeological differences.
In this scenario high degrees of subsidence could be explained if the lower crust was extended more than the upper crust as a result of the passive margin being located in the upper plate of a simple shear system.
Studies of extension in this system, based on industrial seismic reflection profiles, suggested that the high degrees of subsidence seen, especially in the oceanward parts of the rifted margins around this basin could be explained in terms of depth-dependent extension (Davis and Kusznir 2004; Clift and Lin 2001).
Recently, this basin was analyzed to determine the degree of excess subsidence, as well as the timing of when this particular subsidence anomaly formed.
The most salient finding of this study was an increased uptake of 18 F-fluoride at the endplates of the upper and lower vertebral bodies of the fusion region, which was significantly associated with the degree of cage subsidence on CT, regardless of the length of follow-up.
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