Geothermics - Heat Flow in the Lithosphere

by Vincenzo Pasquale
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$66.40
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Vincenzo Pasquale Geothermics - Heat Flow in the Lithosphere
Vincenzo Pasquale - Geothermics - Heat Flow in the Lithosphere

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Description

After a brief review of global tectonics and the structure of the crust and upper mantle, the basic relations of conductive heat transport and the rock thermal properties are introduced as well as the various methods for measuring thermal conductivity and heat generation due to the decay of radioactive elements. The authors analyze geothermal flow and the thermal state of the lithosphere and deep interior and discuss the fundamental problems related to the formation, upwelling mechanisms, solidification and cooling of magmas. The text presents analytical methods that allow us to gain information on heat and groundwater flow from the analyses of temperature–depth data. It also provides ample data and examples to facilitate understanding of the different topics. This book is useful to researchers and graduate students interested in pure and applied geothermics.

Contributors

Author:
Vincenzo Pasquale
Massimo Verdoya
Paolo Chiozzi

Further information

Illustrations Note:
55 SW-Abb., 15 Tabellen
Remarks:

Offers a clear overview of the thermal structure of the Earth


Gives an insight into the formation processes and upwelling mechanisms of magma


Presents an interdisciplinary approach to the analysis of magma solidification, which involve phase change, and cooling of both intrusive igneous bodies and lava covers


Introduces the methods for measuring the thermal properties and the radiogenic heat of rocks


Presents analytical methods for the quantitative inference of the groundwater flow from analyses of subsurface temperature data

Media Type:
Softcover
Publisher:
Springer International Publishing
Language:
English
Number of Pages:
119

Master Data

Product Type:
Paperback book
Release date:
October 29, 2013
Package Dimensions:
0.231 x 0.152 x 0.01 m; 0.166 kg
GTIN:
09783319025100
DUIN:
HD61V4UAIMF
$66.40
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