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...
Главный автор: | Watts, A |
---|---|
Формат: | Journal article |
Язык: | English |
Опубликовано: |
1982
|
Схожие документы
-
SEISMIC STRATIGRAPHY, SUBSIDENCE HISTORY, AND TECTONIC EVOLUTION OF THE ALBORAN SEA, WESTERN MEDITERRANEAN
по: Watts, A, и др.
Опубликовано: (1991) -
Tectonics, global changes in sea level and their relationship to stratigraphical sequences at the US Atlantic continental margin
по: Watts, A, и др.
Опубликовано: (1984) -
CRUSTAL STRUCTURE, FLEXURE, AND SUBSIDENCE HISTORY OF THE HAWAIIAN-ISLANDS
по: Watts, A, и др.
Опубликовано: (1989) -
Stromatolites in caves of the Dead Sea Fault Escarpment: implications to latest Pleistocene lake levels and tectonic subsidence
по: Lisker, S, и др.
Опубликовано: (2009) -
QUANTITATIVE-ANALYSIS OF NORTH-SEA SUBSIDENCE
по: Thorne, J, и др.
Опубликовано: (1989)