1887

Abstract

The Permian–Triassic transition has been surveyed in the Oman Mountains and new detailed sections have been presented (Baud and Bernecker, 2010), from autochthonous shallow-water units (Saih Hatat and Al Jabal al-Akhdar) to slope deposits in the Jabal Sumeini area (Wadi Maqam units), from distal tilted block (Wadi Wasit) to oceanic deep-water deposits (Buday’ah).

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/content/papers/10.3997/2214-4609.20144061
2011-11-28
2024-04-25
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.20144061
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