1887

Abstract

Analysis of industry 3D seismic reflection data on the Ebro continental margin was analized to better understand the evolution of the sedimentary dynamics of the Ebro margin shelf from late Pliocene to present, considering the Gelasian-Calabrian boundary transition from a climate dominated by 41 ka Earth precession cycles to 100 ka obliquity of the Earth’s orbit dominated cycles.

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/content/papers/10.3997/2214-4609-pdb.330.20
2012-07-29
2020-11-24
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609-pdb.330.20
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