1887

Abstract

Caipe Field was discovered in 1967 by drilling of the well C-1X. During the completion<br>operations the zones corresponding to Gobernador Formation of the Eocene were<br>tested successfully, nevertheless the "O" Member of the Escandalosa Formation of the<br>Cenomanian – Turonian, mainly composed by a mix of carbonates and siliciclastic rocks, was<br>not evaluated due to little economic interest at that time.

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/content/papers/10.3997/2214-4609-pdb.111.12
2006-09-24
2021-06-15
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609-pdb.111.12
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