1887
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Abstract

The Strâmbu reservoir is located in ten strata caps of the Helvetian period, transgressively and unconformably overlying the Oligocene, with dips ranging from 400° on the West to 10° on the east.

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/content/papers/10.3997/2214-4609.201406991
1995-05-15
2021-06-14
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201406991
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