1887

Abstract

The stratigraphic architecture of the Siluro-Devonian succession was studied in Algeria and Libya from outcrop sections, logs and sesimic data. A regional transect between the Libyan basins and the western Algerian basins is proposed, using also a new stratigraphic chart. The role of the sub-basins and arches are highlighted in these paleogeographic reconstructions.

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/content/papers/10.3997/2214-4609.20147375
2007-02-26
2020-03-30
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.20147375
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