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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…
This textbook describes how past changes in sea-level can be detected through analysis of the sedimentary record. In particular, it concentrates on the theory of sequence stratigraphy, which provides a framework for how entire sedimentary systems evolve through geological time. …