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Abstract

Albian-Turonian carbonates in NE Arabia show a progressive retreat of their shelf margins towards palaeohighs. This retreat is controlled by localised tectonic collapse of the pre-existing platforms and re-location of platform margins onto structurally high areas.

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/content/papers/10.3997/2214-4609.20145345
2010-01-24
2021-01-23
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.20145345
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