Titlebook: Geological Structures and Moving Plates; R. G. Park Book 1988 Springer Science+Business Media Dordrecht 1988 orogenic belt.orogeny.structu

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鍍金

遠(yuǎn)地點(diǎn)

https://doi.org/10.1007/978-3-642-52602-2ements involving precise levelling and other techniques have shown that most parts of the crust are undergoing slow uplift or depression. The frequency and distribution of intraplate earthquakes is also an indication of widespread tectonic activity, albeit to a notably lesser degree than at plate boundaries.

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高腳酒杯

The lithosphere: some important properties,eanic crust is only about 7 km thick and could not remain undistorted when subjected to the horizontal stresses associated with plate tectonic processes. Plates must be therefore be considerably thicker than the crust and include part of the upper mantle as well.

高腳酒杯

Plate movement and plate boundaries, to plate boundaries, where crustal deformation is therefore concentrated. The determination, both qualitatively and quantitatively, of the relative motion between two adjoining plates at their common boundary is therefore essential in understanding the deformation that takes place there.

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