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Abstract

The Lekhwair/Habshan/Salil (or LHS) system is a carbonate succession that prograded by 300 km toward the northeast across the eastern part of the Arabian Plate (Rayda Basin) from Berriasian to Early Barremian. The system is organized as a series of large prograding clinoforms with amplitudes ranging from 200 to 350 m.

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/content/papers/10.3997/2214-4609.20142797
2012-12-09
2020-10-28
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.20142797
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