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The Petrology of the Sedimentary Rocks (Classic Reprint): A Description of the Sediments and Their Metamorphic Derivatives: A Description of the ... Metamorphic Derivatives (Classic Reprint) - Tapa blanda

Hatch, F. H.

 
9781333608316: The Petrology of the Sedimentary Rocks (Classic Reprint): A Description of the Sediments and Their Metamorphic Derivatives: A Description of the ... Metamorphic Derivatives (Classic Reprint)

Sinopsis

This book describes in great detail the formation of all types of sedimentary rocks, which are derived from sediments. The book delves into the natural processes that turn sediments into rock, including cementation, metasomatism, and other forms of metamorphosis. It also includes a detailed analysis of the many ways various types of sediment are laid down by forces including gravity, wind, running water, ice, marine action, and more. The author separates the study of different types of sediment into three categories: fragmental (formed from the material of pre-existing rocks), chemical (formed from dissolved minerals), and organic (formed from the remains of plants and animals). Each type of sediment is examined, with a particular focus on how the characteristics of the various types of sediment reveal the conditions under which they formed. Whether a particular type of sediment is loose or contained within a solid rock, this book analyzes its processes of formation with an impressive level of detail.

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Reseña del editor

Excerpt from The Petrology of the Sedimentary Rocks: A Description of the Sediments and Their Metamorphic Derivatives

Any of the rocks thus produced are liable to be again broken down should they, either by orogenic elevation or by denudation, be brought into the zone of weathering; and with the deposition OP fresh products of disintegration the cycle of changes starts a'e now. There is no doubt that resistant minerals, such, for example, as zircon, rutile and garnet, have survived many such cycles of change before reaching the positions in which they are now found.

The study of the sediments therefore embraces not only the loose detrital accumulations, but also their derivatives by cementation, metasomatism, and other forms of metamorphism; and the present volume is accordingly divided into two parts, the first of which deals with'the sediments and the second with their metamorphic derivatives.

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