The Plate Tectonics Concept The years following the south military personnel War saw a quantum throttle in the methods of question and analysis in the various terra firma sciences. Based on these discoveries, the very scientists who had earlier doubted Continental drifting, straight off conceded that horizontal continental movement was a possibility and that in that location was a vigorous layer below the crust in the upper mantlepiece - the asthenosphere - that could play a part in this. The evidences of palaeo magnetism and sea-floor spreading confident(p) many scientists of the reality of continental drifting and ushered in the headquarters tectonics theory. Palaeomagnetism: In the 1950s, a group of British scientists showed that when a shake up was formed, be it a polycrystalline rock band from hot magma or a sedimentary or metamorphic rock, the ferrous content of the rock of all time got preserved in it by irritateting magnetised in a burster that was in accordance with the then existent charismatic field. This set magnetism was referred to as leftover magnetism or palaeomagnetism. The come in of magnitude and inclination of an orbit of the palaeomagnetism in a rock could be metrical with the help of magnetometers. The intensity of magnetism in a rock depends on the composition of the lava or magma from which the rock solidifies and on the carriage of the geomagnetic field that time.

Based on these facts, scientists could use the orientation and inclination of a rocks palaeomagnetic axis to determine the side of past magnetic poles. sizeable samples of rock were collected and their rem! nant magnetism measured along with the orientation of the ferrous particles. In Japan, Italy and France, the palaeomagnetic poles were reconstructed on the flat coat of Cenozoic lava flows. It was found that there had been considerable wandering in the position of the poles, which suggested two possibilities. 1. The poles had remained constant and the continents had drifted , or the poles and continents had moved congeneric to each other. 2. The...If you want to get a full essay, order it on our website:
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