大理石流动的实验研究

F. Adams, J. T. Nicolson
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引用次数: 30

摘要

条件下,岩石,它们受到某些地区的地壳,成为最复杂的弯曲和扭曲的方式是一个最早的地质学家,这是公认的事实,它需要但一眼任何扭曲的准确的部分地区的地壳已准备在最近几年显示,通常会有转移或“流”的材料从一个地方到另一个折叠。然而,这种扭曲以及伴随而来的“流动”是如何发生的,这是一个讨论很多、意见分歧很大的问题。一些权威人士认为这是一个纯粹的机械过程,而另一些人则认为溶液和再沉积在所有这些运动中起着必要的作用。这个问题似乎可以通过实验调查来阐明。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
An experimental investigation into the flow of marble
That rocks, under the conditions to which they are subjected in certain parts of the earth’s crust, become bent and twisted in the most complicated manner is a fact which was recognised by the earliest geologists, and it needs but a glance at any of the accurate sections of contorted regions of the earth’s crust which have been prepared in more recent years to show that there is often a transfer or “flow" of material from one place to another in the folds. The manner in which this contortion, with its concomitant “flowing,” has taken place is, however, a matter concerning which there has been much discussion, and a wide divergence of opinion. Some authorities have considered it to be a purely mechanical process, while others have looked upon solution and redeposition as playing a necessary role in all such movements, The problem is one on which it would appear that much light might be thrown by experimental investigation.
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