17 research outputs found

    DECAY PARAMETERS OF AFTERSHOCK SEQUENCES GLOBALLY DISTRIBUTED

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    The evaluation of the parameters c and k of the decay law of the aftershocks in an earthquake sequence has been carried out in this study. For this reason 170 seismic sequences globally distributed, during the time period 1964-1986, were performed. All of them modelled well by Omori’s law. We estimated that the mean global values of and parameters , are 0.660+0.181 and - 0.341+0.090, respectively. The values of these parameters are also estimated for different regions of the world, west and east part of circum-Pacific rim, as well as for the Eurasia belt.The parameters c and k calculated for the various regions of the world found to be spread around the global average, although admittedly few exceptions to this generalization are also observed to exist

    An analysis of the three-dimensional kinetics and kinematics of maximal effort punches among amateur boxers.

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    This is an Accepted Manuscript of an article published by Taylor & Francis in International Journal of Performance Analysis in Sport on 27-9-18, available online: https://doi.org/10.1080/24748668.2018.1525651The purpose of this study was to quantify the 3D kinetics and kinematics of six punch types among amateur boxers. Fifteen males (age: 24.9 ± 4.2 years; stature: 1.78 ± 0.1 m; body mass: 75.3 ± 13.4 kg; boxing experience: 6.3 ± 2.8 years) performed maximal effort punches against a suspended punch bag during which upper body kinematics were assessed via a 3D motion capture system, and ground reaction forces (GRF) of the lead and rear legs via two force plates. For all variables except elbowjoint angular velocity, analysis revealed significant (P < 0.05) differences between straight, hook and uppercut punches. The lead hook exhibited the greatest peak fist velocity (11.95 ± 1.84 m/s), the jab the shortest delivery time (405 ± 0.15 ms), the rear uppercut the greatest shoulder-joint angular velocity (1069.8 ± 104.5°/s), and the lead uppercut the greatest elbow angular velocity (651.0 ± 357.5°/s). Peak resultant GRF differed significantly (P < 0.05) between rear and lead legs for the jab punch only. Whilst these findings provide novel descriptive data for coaches and boxers, future research should examine if physical and physiological capabilities relate to the key biomechanical qualities associated with maximal punching performance

    Active fault geometry and kinematics in Parnitha Mountain, Attica, Greece

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    none8The Parnitha mountain range lies between two Quaternary rift systems in central Greece: the Gulf of Corinth Rift and the Gulf of Evia rift. We suggest that the range was formed by footwall uplift on active normal faults striking WNW–ESE and NE–SW. We investigated the scarp appearance, geometry and slip rates of three normal faults bounding this mountain range by field mapping at 1:5000 scale. Active faults studied include the 8.5 km long Fili Fault, the 4.7 km long Maliza Fault and the 4 km long Thrakomakedones Fault. We calculated comparable mean slip rates for all mapped faults (Fili: 0.18 mm/yr, Avlon: 0.2 mm/yr, Thrakomakedones: 0.24 mm/yr); however, we suggest that the WNW–ESE structures are more active during the Late Quaternary because of abundant field evidence of recent movements along slip surfaces (fresh basal stripes and slickenlines). In addition, stress axes analysis shows a N7°E–N25°E (NNE–SSW) oriented, extensional stress field, which is compatible with the focal mechanism of the Athens 1999 earthquake. The fault-slip data from the Parnitha faults show orientations similar to other low-strain areas in central Greece, such as the Gulf of Evia Rift to the north. Our slip rate estimates may explain the low recurrence of large earthquakes in Attica as opposed to high slip rate areas in central Greece such as the neighbouring Gulf of Corinth.noneGanas A.; Pavlides S.; Sboras S.; Valkaniotis S.; Papaioannou S.; Alexandris G.A.; Plessa A.; Papadopoulos G.A.Ganas, A.; Pavlides, S.; Smporas, Sotirios; Valkaniotis, S.; Papaioannou, S.; Alexandris, G. A.; Plessa, A.; Papadopoulos, G. A
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