1887

Abstract

The development of the Central Luconia carbonate build-ups were strongly influenced by the interplay between eustatic sealevel<br>and basinal tectonics. The Alpha field addressed here is one of the seismically best imaged isolated carbonate platforms<br>in Central Luconia and dendritic features, interpreted as karst, were found to be very prominent throughout the field. Karst is a<br>diagenetic facies, an overprint in sub-aerially exposed carbonate bodies produced and controlled by dissolution and migration<br>of calcium carbonate in meteoric waters.

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/content/papers/10.3997/2214-4609-pdb.280.iptc14539_noPW
2012-02-07
2021-10-20
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609-pdb.280.iptc14539_noPW
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