‘Biaxial serial excision’ or ‘polyaxial serial excision’
However, I wish to differ on the terminology used for the technique ‘biaxial’, described by the author, as it gives an erroneous impression. Biaxial implies two axes as shown in Figure 1 a and b where, the skin laxity in two axes is taken advantage of, in order to close the skin edges. The author’s technique described as “edges of the ellipse (excision planned) are extended outwards into multiple W’S and V’s” can be analyzed as in Figure 2a and b where the multiple W’s or V’s can be joined to form multiple ellipses. One can now see that the axes of excision of these different ellipses are multiple and the technique takes advantage of skin laxity along multiple different axes. Therefore, geometrically speaking, the technique should be called‘Polyaxial serial excision› and not Biaxial serial excision’ as claimed by the author.
Integrating a Profile of Frontal Face With Its Mirror Image for Facial Reconstruction
Introduction and Objectives: Face recognition plays an important role in the field of biometrics, bioinformatics, and forensic identification. Human faces appear bilaterally symmetric. However, asymmetry is a norm in the human body and careful morphological and metric examination of the human face gives an exact idea of the asymmetry present in the face of an individual. Most of the studies on asymmetry of human face have been carried out with regard to evaluation of expressions in psychology, anthropology, and biometrics. In this preliminary study, an idea of the human face symmetry has been used for complete facial reconstruction. Sometimes, in the CCTV cameras and other surveillance systems, the complete face is not visible, but only a half of the frontal face is detectable. In all such cases, the mirror image of the face can be used to reconstruct the complete face of the person in question for representation-based face recognition. In previous studies related to forensic identification and in the discipline of computer science, mirror images have only been used to overcome and deal with the problem of nonsufficient training sample and have not been used for the reconstruction of the full facial profile. Methodology: In this article, we present a computerized methodology to generate the mirror image from one frontal half of the face (either left or right) and merging the both (input image and generated mirror image) halves to create the full face. The program was designed using METLAB computer program. This procedure is very simple, less time–consuming, and computationally efficient. Results and Conclusion: The results have been presented with regard to generate a complete face in those cases where only one frontal profile, that is, left or right sides of the face is available for examination. The scenario is commonly seen in those cases also where shadow almost hides one half of the face. The proposed methodology would also be useful for improving other facial reconstruction and recognition methods in forensic identification and in other medical fields such as plastic surgery, where creating full face still poses a technical challenge to a plastic surgeon. Some challenges, limitations, and future perspectives of the method have also been discussed in the article.
Igneous Rock Associations 23. The Bushveld Complex, South Africa: New Insights and Paradigms
SUMMARYThe Bushveld Complex has continued to serve as the basis for study into the fundamental nature of petrological processes for layered intrusion formation and for oxide and sulphide hosted Platinum Group Element (PGE)–Cu–Ni ore deposits. These studies have included discoveries in terms of the physical extent of Bushveld magmatism, both laterally and internally. Lateral variations in the mafic to ultramafic Rustenburg Layered Suite of the Northern Lobe of the complex have also revealed petrologically distinctive Upper Critical Zone equivalent rocks (the so-called Flatreef) with enhanced contamination and mineralization traits that reflect a transition between Eastern and Western Lobe equivalent stratigraphy and Platreef-style complexity. Traditional magma mixing models have been re-examined in light of radiogenic isotopic evidence for crustal involvement early in the chromite precipitation or formation process, combined with evidence for associated heterogeneous fluid contents, cryptic layering profiles, and textural evidence. A wide variety of alternative ore-genesis models have been proposed as a consequence. The fundamental mechanics of magma chamber processes and the existence of the magma chamber as an entity have been called into question through various lines of evidence which have promoted the concept of progressive emplacement of the complex as a stack of not-necessarily-quite-sequentially intruded sills (with or without significant quantities of transported phenocrysts), emplaced into variably crystallized and compacted crystal-liquid mush mixtures, modified by compaction-driven late magmatic fluid (silicate and aqueous) activity. Alternatively, petrological and geochemical observations have been used to discount these interpretations in favour of more conventional cooling and gravity-driven accumulation of silicate and ore minerals in a large, liquid-dominated system.RÉSUMÉLe complexe de Bushveld a demeuré à la base d’études sur la nature fondamentale des processus pétrologiques de formation d’intrusions litées et des gîtes des éléments du groupe platine (ÉGP)-Cu-Ni hébergés dans les oxydes et les sulfures. Ces études ont comporté des découvertes sur l’étendue physique, à la fois latérale et interne, du magmatisme de Bushveld. Les variations latérales de la suite stratifiée et mafique à ultramafique Rustenburg du lobe nord du complexe ont également révélé des roches équivalentes pétrologiquement distinctes de la zone critique supérieure (le communément désigné Flatreef) avec des traits de contamination et de minéralisation accrus qui reflètent une transition entre la stratigraphie équivalente des lobes est et ouest et la complexité de type Platreef. Les modèles traditionnels de mélanges magmatiques ont été réexaminés à la lumière de preuves isotopiques radiogéniques indiquant une implication de la croûte au début du processus de précipitation ou de formation de la chromite, combinées à des preuves de contenu fluide hétérogène associé, de profils de litage cryptique et de preuves texturales. Ainsi, une grande variété de modèles alternatifs de genèse de minerai a été proposée. La mécanique fondamentale des processus de la chambre magmatique et l'existence de la chambre magmatique en tant qu'entité ont été remises en question au moyen de divers éléments de preuve qui ont mis en avant le concept de mise en place progressive du complexe sous forme d'un empilement non-nécessairement séquentiel de sills injectés (avec ou sans quantités significatives de phénocristaux transportés) mis en place dans des mélanges de bouillie cristaux/liquide à cristallisation et compaction variable, modifiés par une activité tardive de fluide magmatique (silicaté et aqueux) induite par la compaction. Alternativement, des observations pétrologiques et géochimiques ont été utilisées pour écarter ces interprétations en faveur d'un processus plus conventionnel de refroidissement et d’accumulation de minérais silicatés et minéralisés induite par la gravité dans un vaste système à dominance liquide.