By A. P. Bos, Rein Ferwerda
Not like what's usually proposal, the paintings "De spiritu" is fullyyt Aristotelian. It presents an integral a part of Aristotle's philosophy of dwelling nature. during this paintings he's the 1st Greek to argue that the main basic important precept.
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Additional info for Aristotle, On the life-bearing spirit (De spiritu): a discussion with Plato and his predecessors on pneuma as the instrumental body of the soul
9 km s−1 became the first arrivals, termed the Pn phase. These data were interpreted by the standard techniques of refraction seismology, with Pn representing seismic waves that had been critically refracted at a velocity discontinuity at a depth of some 54 km. This discontinuity was subsequently named the Mohorovicˇic´ discontinuity, or Moho, and it marks the boundary between the crust and mantle. Subsequent work has demonstrated that the Moho is universally present beneath continents and marks an abrupt increase in seismic velocity to about 8 km s−1.
The seismic effects are more pronounced for S waves than for P waves. The low seismic velocities could arise from a number of different mechanisms, including an anomalously high temperature, a phase change, a compositional change, the presence of open cracks or fissures, and partial melting. All but the latter appear to be unlikely, and it is generally accepted that the lower seismic velocities arise because of the presence of molten material. 12, Fig. 36). Only a very small amount of melt is required to lower the seismic velocity of the mantle to the observed values and to provide the observed attenuation properties.
There have been many different mechanisms proposed for ophiolite obduction, none of which can satisfactorily explain all cases. It must thus be recognized that there may be several operative mechanisms and that, although certainly formed by some type of accretionary process, ophiolite sequences may differ significantly, notably in terms of their detailed geochemistry, from lithosphere created at mid-ocean ridge crests in the major ocean basins. Although many ophiolites are highly altered and tectonized, because of the way in which they are uplifted and emplaced in the upper crust, there are definite indications that there is more than one type of ophiolite.
Aristotle, On the life-bearing spirit (De spiritu): a discussion with Plato and his predecessors on pneuma as the instrumental body of the soul by A. P. Bos, Rein Ferwerda