Experimental modeling of rifting at craton margins

Lithospheric-scale centrifuge models are used to investigate the process of continental rifting at the margins of cratonic areas. Models reproduce extension between a resistant cratonic lithosphere and an adjacent, weaker mobile belt and investigate the influence of the strength contrast between craton and belt and the presence or absence of an intervening weak zone (such as a suture) on the extensional deformation. Model results suggest that regardless of craton and belt strength contrast, the presence of the weak zone strongly localizes deformation, leading to the development of narrow, deep rift valleys corresponding at depth to marked lithospheric thinning. Depending on the pre-rift rheology (in particular depending on the presence of a significant decrease of the brittle-ductile transition depth in the belt domain), the resulting basin can be largely asymmetric, with a major border fault system on the craton side. When the weak zone is absent, deformation is typically more distributed and lithospheric thinning more homogeneous. In these conditions the strength contrast between craton and belt strongly controls deformation: when the contrast is minimal, no major faults form at the craton-belt boundary, and a roughly symmetric deformation affects a wide region inside the strong mobile belt after the initial stages of extension. Conversely, for high strength contrasts, more asymmetric deformation is localized on a major fault system at the craton margin at the beginning of extension; with progressive extension, minor faulting propagates inside the weak belt, widening the deformed zone. Comparison with different natural examples suggests that these results may be important and have relevance for the development of continental rifts at the margins of cratonic areas

A metrological characterization of the Kinect V2 time-of-flight camera

A metrological characterization process for time-of-flight (TOF) cameras is proposed in this paper and applied to the Microsoft Kinect V2. Based on the Guide to the Expression of Uncertainty in Measurement (GUM), the uncertainty of a three-dimensional (3D) scene reconstruction is analysed. In particular, the random and the systematic components of the uncertainty are evaluated for the single sensor pixel and for the complete depth camera. The manufacturer declares an uncertainty in the measurement of the central pixel of the sensor of about few millimetres (Kinect for Windows Features, 2015), which is considerably better than the first version of the Microsoft Kinect (Chow et al., 2012 [1]). This work points out that performances are highly influenced by measuring conditions and environmental parameters of the scene; actually the 3D point reconstruction uncertainty can vary from 1.5 to tens of millimetres

Images and videos of analogue centrifuge models exploring marginal flexure during rifting in Afar, East Africa

This data set includes images and videos depicting the evolution of deformation and topography of 17 analogue experiments c passive margin development, to better understand the ongoing tectonics along the western margin of Afar, East Africa. The tectonic background that forms the basis for the experimental design is found in Zwaan et al. 2019 and 2020a-b, and references therein. The experiments, in an enhanced gravity field in a large-capacity centrifuge, examined the influence of brittle layer thickness, strength contrast, syn-rift sedimentation and oblique extension on a brittle-viscous system with a strong and weak viscous domain. All experiments were performed at the Tectonic Modelling Laboratory of of the Istituto di Geoscience e Georisorse - Consiglio Nazionale delle Ricerche (CNR-IGG) and of the Earth Sciences Department of the University of Florence (CNR/UF). The brittle layer (sand) thickness ranged between 6 and 20 mm, the underlying viscous layer, split in a competent and weak domain (both viscous mixtures), was always 10 mm thick. Asymmetric extension was applied by removing a 1.5 mm thick spacer at the side of the model at every time step, allowing the analogue materials to spread when enhanced gravity was applied during a centrifuge run. Differential stretching of the viscous material creates flexure and faulting in the overlying brittle layer. Total extension amounted to 10.5 mm over 7 intervals for Series 1 models that aimed at understanding generic passive margin development in a generic orthogonal extension setting, whereas up to 16.5 mm of extension was applied for the additional Series 2 models aiming at reproducing the tectonic phases in Afar. In models involving sedimentation, sand was filled in at time steps 2, 4 and 6 (i.e. after 3, 6 and 9 mm of extension). Detailed descriptions of the experiments, monitoring techniques and tectonic interpretation of the model results are presented in Zwaan et al. (2020c) to which these data are supplementary

analogue modelling of the influence of ice shelf collapse on the flow of ice sheets grounded below sea level

In this work we use analogue modelling to analyse the effect of sudden ice shelf breakup on the flow of ice draining an ice sheet grounded below sea level. Experimental results confirm that the removal of the buttressing effect exerted by the ice shelf results in significant acceleration of inland glaciers: the models show indeed a pronounced increase in ice velocity close to the grounding line. However, this effect does not significantly propagate upstream towards the internal portions of the ice sheet and rapidly decays with time. Therefore, the ice sheet is almost unaffected by flow perturbations induced by the disintegration of the ice shelf

Fault architecture in the Main Ethiopian Rift and comparison with experimental models: Implications for rift evolution and Nubia-Somalia kinematics

The Main Ethiopian Rift (MER) offers a complete record of the time–space evolution of a continental rift. We have characterized the brittle deformation in different rift sectors through the statistical analysis of a new database of faults obtained from the integration between satellite images and digital elevation models, and implemented with field controls. This analysis has been compared with the results of lithospheric-scale analogue models reproducing the kinematical conditions of orthogonal and oblique rifting. Integration of these approaches suggests substantial differences in fault architecture in the different rift sectors that in turn reflect an along-axis variation of the rift development and southward decrease in rift evolution. The northernmost MER sector is in a mature stage of incipient continental rupture, with deformation localised within the rift floor along discrete tectono-magmatic segments and almost inactive boundary faults. The central MER sector records a transitional stage in which migration of deformation from boundary faults to faults internal to the rift valley is in an incipient phase. The southernmost MER sector is instead in an early continental stage, with the largest part of deformation being accommodated by boundary faults and almost absent internal faults. The MER thus records along its axis the typical evolution of continental rifting, from fault-dominated rift morphology in the early stages of extension toward magma-dominated extension during break-up. The extrapolation of modelling results suggests that a variable rift obliquity contributes to the observed along-axis variations in rift architecture and evolutionary stage, being oblique rifting conditions controlling the MER evolution since its birth in the Late Miocene in relation to a constant post ca. 11 Ma ~ N100°E Nubia–Somalia motion.Published479-4923.2. Tettonica attiva3.3. Geodinamica e struttura dell'interno della TerraJCR Journalreserve

The Use of Empirical Methods for Testing Granular Materials in Analogue Modelling

The behaviour of a granular material is mainly dependent on its frictional properties, angle of internal friction, and cohesion, which, together with material density, are the key factors to be considered during the scaling procedure of analogue models. The frictional properties of a granular material are usually investigated by means of technical instruments such as a Hubbert-type apparatus and ring shear testers, which allow for investigating the response of the tested material to a wide range of applied stresses. Here we explore the possibility to determine material properties by means of different empirical methods applied to mixtures of quartz and K-feldspar sand. Empirical methods exhibit the great advantage of measuring the properties of a certain analogue material under the experimental conditions, which are strongly sensitive to the handling techniques. Finally, the results obtained from the empirical methods have been compared with ring shear tests carried out on the same materials, which show a satisfactory agreement with those determined empirically

The Social Transmission of Attractiveness Stereotypes: An Investigation of Parental Expectations of Children\u27s Behavior

Eighty-six children from the Utah State University Child Development Laboratories and Hillcrest Elementary School and their parents participated in the study. The study focused on the use of attractiveness stereotyping used by children across four age groups. The study also analyzed the social transmission of attractiveness stereotypes from parents to their children. The study included two parts: 1) a play-preference measure, and 2) a social attribution measure. The stimuli were sketches of twelve children, six toys and six girls. The sketches of children included attractive, unattractive, mesomorphic, endomorphic, handicapped and nonhandicapped children. In the study we found that parents and children use attractiveness stereotypes. Further, parents and children utilized a beauty-is-good assumption when evaluating the children\u27s personalities and social tendencies from the sketches. Finally, we found that parents in this study expected their children to use a similar physical attractiveness hypothesis in their Social judgement