Non-volcanic continental margins may form up to 300f all present-day passive margins, and remnants of them are preserved in mountain belts. The papers in this volume demonstrate the benefits of integrating offshore and onshore studies, and illustrate the range of information obt…
Intraplate strike-slip deformation belts are common tectonic features, particularly at convergent plate boundaries, where they are produced by both oblique convergence and continental indentation. This volume contains 13 papers from an international field of contributors. Studie…
![The nature and origin of compression in passive margins ; [Joint Petroleum Group/Tectonic Studies Group International Conference "Compressional Deformation within Passive Margins: Nature, Causes and Effects" which was held at the Geological Society, Londin in Oktober 2005]](https://covers.openlibrary.org/b/isbn/1862392617-M.jpg?default=false)
by International Conference Compressional Deformation within Passive Margins: Nature, Causes and Effects, London, Joint Petroleum Group/Tectonic Studies Group International Conference "Compressional Deformation Within Passive Margins: Nature, Causes and Effects", London
