Titlebook: Microtectonics; C. W. Passchier,R. A. J. Trouw Textbook 19981st edition Springer-Verlag Berlin Heidelberg 1998 Deformation.Foliation.Mikro

Desert

paroxysm

Deformation Mechanisms,n rate. Grain-scale microstructures that are thought to be formed in response to these processes are highlighted, and it is shown how such microstructures can be used to identify deformation processes that have been operating. Structures visible within grains are known as ..

道學(xué)氣

Special Techniques,m is to allow the reader to assess whether other techniques can help him to solve his problem and, if so, what material has to be prepared. We do not treat microprobe analysis or field techniques since they are sufficiently covered in other textbooks.

ANA

Exercises,s are given at the end of the section. The subjects of the problems follow the sequence of treatment in the book. The reader may not always agree with our interpretations, but the main purpose of this chapter is to provide some examples of how information can be obtained from thin sections and which arguments can be used for their interpretation.

執(zhí)

Feigned

A Framework of Microtectonic Studies,ral geologists learned to profit from the wealth of data that can be obtained from the geometry of structures studied in thin section, and metamorphic petrologists have appreciated the relation of structural evolution on the thin section scale and metamorphic processes.

多嘴多舌

過(guò)多

etidronate

Flow and Deformation,regard to forces causing the motion. This approach is useful in geology, where usually very little information can be obtained concerning forces responsible for deformation. In order to keep the discussion simple, the treatment is centred on flow and deformation in two dimensions.