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Pronounced lateral variations in Europes intraplate strength occur, as a result of thermal perturbation in the underlying mantle and inherited inhomogeneity in lithospheric structures, as a result of Europes polyphase pre-Quaternary evolution. This book presents the results from quantitative subsidence analysis studies.

NEOTECTONICS AND QUATERNARY FAULT-REACTIVATION IN EUROPE'S INTRAPLATE LITHOSPHERE

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NEOTECTONICS AND QUATERNARY FAULT-REACTIVATION IN EUROPE'S INTRAPLATE LITHOSPHERE

ELSEVIER SCIENCE & TECHNOLOGY

 

SERIES:  
YEAR: 2005
SIZE: 280 x 210
BINDING: Hardback
ISBN: 9780080446875
TYPE: Professional and Vocational

 

 

 

Product Description for NEOTECTONICS AND QUATERNARY FAULT-REACTIVATION IN EUROPE'S INTRAPLATE LITHOSPHERE

 

Pronounced lateral variations in Europe's intraplate strength occur, as a result of thermal perturbation in the underlying mantle and inherited inhomogeneity in lithospheric structures, as a result of Europe's polyphase pre-Quaternary evolution. This book presents the results from quantitative subsidence analysis studies.

 

 

 

 


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