Prospect to Pipeline

Prospect to Pipeline
Author: Wyoming Geological Association. Field Conference
Publisher:
Total Pages: 208
Release: 1997
Genre: Diamond deposits
ISBN:

The Geological Deformation of Sediments

The Geological Deformation of Sediments
Author: A. Maltman
Publisher: Springer Science & Business Media
Total Pages: 368
Release: 2012-12-06
Genre: Science
ISBN: 9401107319

shallow processes and for the pursuit of more Sediments are now known to undergo deforma tion in a wide variety of geological circumstances. quantitative relationships. With these goals in The deforming processes can happen on a vast mind, workers are increasingly drawing on the scale and at all stages before the material be principles and methods of the well-established comes fully lithified. In fact, as exploration of the engineering discipline of soil mechanics. earth continues, the widespread extent and im All this is beginning to attract wider geological portance of sediment deformation is still being interest. Yet to the newcomer, because progress revealed, for example, below the oceans and has been rapid in recent years, the literature is beneath ice sheets. At the same time, it is still already formidable. The information is scattered, being realized just how varied are the resulting so even an expert on sediment deformation in a structures, and how strikingly similar they can be certain setting may be unaware of analogous to those produced by the deformation of deeply problems and successes in other environments. buried rocks. At the same time, although the same basic prin However, there are few precedents to guide the ciples apply in the various geological regimes, a geologist in interpreting structures that formed in subtly different terminology is evolving, which unlithified sediments, or in understanding the can make the subject boundaries hard to cross.

Continental Deformation

Continental Deformation
Author: Paul L. Hancock
Publisher: Pergamon
Total Pages: 444
Release: 1994
Genre: Science
ISBN:

Explains clearly and concisely the essential attributes of new concepts that have arisen during the last twenty years in structural geology and tectonics. Deformational and tectonic processes and relationships on all scales are discussed. Site or time specific assemblages are not emphasised with the exceptions of Archaean tectonics and neotectonics. The new nomenclature that has proliferated as a result of the need to express new ideas is highlighted.