TECTONIC SUBSIDENCE, FLEXURE AND GLOBAL CHANGES OF SEA-LEVEL

Tectonic models for the evolution of passive continental margins predict that following rifting, sediments should progressively onlap basement at the edge of a margin as the lithosphere cools and increases its flexural rigidity with age. The pattern of modelled onlap is strikingly similar to that us...

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Bibliografiske detaljer
Hovedforfatter: Watts, A
Format: Journal article
Sprog:English
Udgivet: 1982

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