Treatise on geochemistry
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Treatise on geophysics
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"This proceedings book investigates the possibilities for creating new models of the continental lithosphere structure by integrating methods from geothermodynamics and deep geoelectrics. It particularly focuses on the use of powerful controlled sources of electromagnetic field …
This proceedings book investigates the possibilities for creating new models of the continental lithosphere structure by integrating methods from geothermodynamics and deep geoelectrics. It particularly focuses on the use of powerful controlled sources of electromagnetic field t…
This proceedings book investigates the possibilities for creating new models of the continental lithosphere structure by integrating methods from geothermodynamics and deep geoelectrics. It particularly focuses on the use of powerful controlled sources of electromagnetic field t…
"This book is a handbook for geologists and geophyicists who manipulate thermal data, particularly for petroleum exploration. In theory and with practical examples, the book discusses the sources of heat within the crust, describes how to maximize the accuracy of temperature dat…
"Crustal Heat Flow: A Guide to Measurement and Modelling is a handbook for geologists and geophysicists who manipulate thermal data, particularly for petroleum exploration." "This text will be attractive to a broad range of earth scientists. Many geologists will be interested in…
Crustal Heat Flow: A Guide to Measurement and Modeling is a handbook for geologists and geophysicists who manipulate thermal data, particularly for petroleum exploration. In theory and with practical examples the book discusses the sources of heat within the crust, describes how…
Cratons are the ancient, typically Archean in age, stable interior of continental plates. They are thicker and more stable than the surrounding lithosphere due to their lithospheric mantle composition of depleted peridotite and limited interaction with convecting mantle. The inh…
Glacial isostatic adjustment (GIA) is the ongoing response of the viscoelastic solid Earth, oceans and the gravitational field to the previous burden of the ice loads. The Earth’s surface was once covered with massive ice sheets, and melting of these ice sheets is still reshapin…