1887

Abstract

The Gryphon Field comprises Eocene aged high-density turbidite sands, which were remobilised and forcibly injected into the overlying claystones as injection features. Reservoir sands in each well were classified either as ‘in-situ’ or ‘injected’ using in

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/content/papers/10.3997/2214-4609.201400295
2009-06-08
2024-04-20
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201400295
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