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Abstract Background It is challenging to determine the orthogonality of radiographs in daily clinical practice. The purpose of this study was to show the usefulness of an additional foot ring which might determine the orthogonality of postoperative radiographs for the parameter measurement of hexapod external fixator. Methods We retrospectively analyzed 81 consecutive trauma patients with tibial shaft fractures treated by the hexapod external fixator at our institution from September 2014 to July 2019. Starting in March 2016, the postoperative radiographs for parameter measurement were obtained under the control of an additional foot ring. The final data consisted of 47 patients in traditional radiographs (Group I) and 34 patients under the control of foot ring during the radiographic process (Group II). The demographic data, original postoperative deformities, residual deformities after final correction, number of repeated radiographs after the first postoperative radiographs, time to the satisfactory reduction achieved, and external fixation time in all patients were documented and analyzed. The Johner–Wruhs criteria were used for the final clinical outcomes evaluation at the last clinical visit. Results Satisfactory reduction and bone union were achieved in all patients. There were no statistical significances between the two groups in the demographic data, original postoperative deformities, residual deformities after final correction, external fixation time, and the final clinical outcomes (P > 0.05). The mean number of repeated radiographs after the first radiographs (1.4 times) and mean time to the satisfactory reduction achieved (3.3 days) in patients with an additional foot ring used were all less than those without foot ring (2.4 times, 5.3 days) (P

Resumen: Las deformidades torsionales de las extremidades inferiores corresponden a una de las causas de visita más frecuente al ortopedista infantil. En la mayoría de los casos, estas consultas son innecesarias, pues se trata de condiciones normales del esqueleto en desarrollo, que suelen corregir espontáneamente. El médico no especialista debe estar familiarizado con los cambios fisiológicos que ocurren en las extremidades inferiores del niño, de manera de identificar aquellos casos severos o aquellos que producen alteraciones funcionales.Estas deformidades, pueden ocurrir en cualquier nivel, desde la pelvis a los pies, por lo que un examen físico sistemático permitirá identificar la causa y proponer un tratamiento de acuerdo a los hallazgos. El único tratamiento eficaz, cuando la situación lo requiere, es la cirugía ortopédica. El uso de plantillas, calzado ortopédico y órtesis no cumplen ninguna función en el manejo de estas alteraciones. Summary: Torsional deformities of lower limbs are one of the most frequent causes to visit a pediatric orthopedic surgeon. In most cases, these are unnecessary, as they represent a normal stage of the developing skeleton, which usually correct spontaneously. The nonspecialist physician must be familiar with the physiological changes that occur in children's lower limb, in order to identify those cases that are severe, or cause functional disabilities.These deformities can occur at any level, from the pelvis to the feet, so a systematic physical examination will allow the cause to be identified and treated to be proposed according on to the findings. The only effective treatment, when the situation requires it, is orthopedic surgery. The use of insoles, orthopedic footwear, and orthoses have no role in the management of these alterations.

Background: It is challenging to determine the orthogonality of radiographs in daily clinical practice. The purpose of this study was to show the usefulness of an additional foot ring which might determine the orthogonality of postoperative radiographs for the parameter measurement of hexapod external fixator. Methods: We retrospectively analyzed 81 consecutive trauma patients with tibial shaft fractures treated by the hexapod external fixator at our institution from September 2014 to July 2019. Starting in March 2016, the postoperative radiographs for parameter measurement were obtained under the control of an additional foot ring. The final data consisted of 47 patients in traditional radiographs (Group I) and 34 patients under the control of foot ring during the radiographic process (Group II). The demographic data, original postoperative deformities, residual deformities after final correction, number of repeated radiographs after the first postoperative radiographs, time to the satisfactory reduction achieved, and external fixation time in all patients were documented and analyzed. The Johner–Wruhs criteria were used for the final clinical outcomes evaluation at the last clinical visit. Results: Satisfactory reduction and bone union were achieved in all patients. There were no statistical significances between the two groups in the demographic data, original postoperative deformities, residual deformities after final correction, external fixation time, and the final clinical outcomes (P > 0.05). The mean number of repeated radiographs after the first radiographs (1.4 times) and mean time to the satisfactory reduction achieved (3.3 days) in patients with an additional foot ring used were all less than those without foot ring (2.4 times, 5.3 days) (P < 0.05). Conclusions: The additional foot ring is a practical device to ensure the orthogonality of postoperative radiographs for the hexapod external fixator parameter measurement. Radiation exposure, duration of deformity correction, and cost for patients might be reduced due to the less repeated radiographs with the wrong position. [ABSTRACT FROM AUTHOR]

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Shear fault-bend folds, a common feature of fault bend folds in foreland fold-and-thrust belts, originate in the early deformation stage. Building upon Suppe's geometric model of 'shear fault-bend folding,' we present refined calculation formulas for total shortening, incremental shortening, and the shear coefficient specific to these folds, as well as ideas to verify model parameters. The practicality and versatility of our refined approach are confirmed through case studies of the Pakuashan anticline in Taiwan and the Tugulu anticline in North Tian Shan. This improved incremental shortening calculation formula, conserves the bed length and eliminates errors of the widely used shortening calculation formula, is crucial for understanding deformation processes and assessing seismic risks shear fault bend folding. To obtain more precise incremental shortening calculations, it should further refine the geometric and kinematic models of shear fault bend folding in the future. • We derive the equations for the relationship between parameters of shear fault bend folds (FBF). • A new method is developed for constraining the incremental shortening of shear FBF. • The change of each parameter during the shear fault bend folding are described while maintaining simplicity. [ABSTRACT FROM AUTHOR]

The Annot syncline is one of the synclinal remnants of the Tertiary Alpine foreland basin, which was mainly structured during the Paleocene and filled during the Eocene-Oligocene by a marine transgressive succession. The upper unit consists in the Annot Sandstone formation deposited in a fan delta-fed turbidite setting. New detailed structural data from the Annot depocentre indicate a progressive limb rotation during deposition of the Annot Sandstone. These data are used to build a 3D model of the syncline in Gocad software that documents turbidite depocentre evolution. Trishear modelling constrains the role and interaction of regional thrusts and fault propagation folds in depocentre development. [ABSTRACT FROM AUTHOR]

The Huoerguosi anticline, located in the north Tianshan Mountains piedmont fold-and thrust belt, is a trending east-west fault-related fold. In the cross section along the Jingou River, its south limb is composed of the pre-growth strata of the Anjihaihe (E2-3a), the Shawan ((E3-N1)s), the Taxihe (N1f) and the lower part of the Dushanzi (N2,d)Formations, trending east-west and dipping to south 55°, and the growth strata of the upper part of the Dushanzi (N2d) and Xiyu ((N2-Q1)x) Formations, dips of which decrease from 55° at the base of the growth strata to 47° at the bottom of the Xiyu ((N2-Q1)x) Formation to ∼0° at the top of the Xiyu ((N2-Q1)x) Formation. The strata at the north limb of the anticline are vertical or over-turned, and are cut by the breakthrough thrusts to result in the drag fold. In the depth, the anticline is symmetric, and its core comprises the Cretaceous and the Jurassic coal-bearing beds. In the seismic profile, the seismic reflectors of pre-growth strata at the south limb of the anticline dip to south constantly, and ones of the growth strata fan southward, whose dips decrease upward. The geometry of the south limb growth strata outcropped along the Jingou River valley and the deep structure of the anticline shown in the seismic profile indicate that the Huoerguosi anticline is a detachment fold anticline growing by limb rotation. Based on the growth model and magneto stratigraphic age, during the growing process of the Huoerguosi anticline, the average shortening rate absorbed by the south limb is ∼0.46 mm/a, and the average uplifting rate of the anticline is ∼0.86 mm/a which exceeds the average deposition rate, which is in accordance with the fact that the top of the anticline is intensely eroded. Considering symmetric geometry of the Huoerguosi anticline and ignoring the breakthrough thrusts, the shortening of the whole anticline should be more than ∼0.92 mm/a, doubling the shortening rate determined from the growth at the south limb. [ABSTRACT FROM AUTHOR]

Abstract: Fault-bend folding is a common folding mechanism in thrust and fold belts worldwide. The widely used kink-band geometric model of fault-bend folding necessitates complex ramp segmentations to reproduce the rounded shape of many natural thrust related anticlines. Curvilinear hinge sectors provide a geometric and kinematic alternative solution to kink bands for modelling curved-hinge folds. We developed an analytical solution for modelling fault-bend folding using circular hinge sectors. The velocity field of this kinematic solution is different from that associated with the classical, kink-style model. Our solution predicts the development of curvilinear anticlines above staircase fault geometries, the occurrence of limb rotation and, consequently, the development of rotational syngrowth wedges on both the forelimb and the crest. Conversely to the kink-style kinematics, curvilinear hinge sectors imply a dependence of deformation intensity from the fold shape and stratigraphic position of the folded layer. Application to natural thrust-related anticlines validates the effectiveness of curvilinear fault-bend folding. [Copyright &y& Elsevier]

The Surin Mastgarh anticline (SMA) marks the active deformation front in the northwest Sub-Himalaya near Jammu. The southern limb of the SMA is not truncated by an emergent thrust, unlike other frontal folds along the Himalayan front. We investigate the structural data, deformation pattern, and seismic potential of the SMA using field surveys and re-interpretation of seismic profile. Strath profiles along the Chenab and the Munavar Tawi river valleys indicate active growth of the SMA by layer parallel shortening, and limb rotation accompanied by flexural slip, suggesting an early phase of its development. Lateral migration of the southern limb suggesting limb lengthening and bending at the hinge are the dominant mechanisms of fold amplification with strain localization at the fold core above the floor thrust tip. Bending moment faulting at the hinge led to the formation of crestal grabens or lakes in the southeastern section of the SMA. Our results suggest the existence of a weak, less viscous layer beneath a brittle sedimentary detachment. The SMA initiated as a detachment fold and sequentially deformed by passive roof thrusting. Therefore, the seismotectonic model of the Jammu Sub-Himalaya is different from that of the central and eastern Himalaya. • The Surin Mastgarh Anticline is a detachment fold. • The Surin Mastgarh Anticline grows with a fixed hinge and limb lengthening. • The Surin Mastgarh Anticline is associated with flexural-slip and bending moment fault. [ABSTRACT FROM AUTHOR]

The human body's structure is remarkable in that it is basically uniform across the populations. Apart from a few dissimilarities in skin color and external features, at the visceral and microscopic levels, man is unusually identical. Minor ethnic variations, both acquired or congenital and atavistic traits apart, human morphology is universal. In this brief communication I present and discuss an observation made on the position of the free upper limb in the erect adult. It is seen that body weight influences forelimb position. In the stout, stocky and overweight, the upper limb is at rest, held medially rotated (axially); the degree of axial rotation being directly related to the increase in body weight. [ABSTRACT FROM AUTHOR]