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Abstract

Polygonal fracture patterns in clastic environments have been first observed in the early 90’s, thanks to 3D seismic. Incarbonate rocks only few examples, e.g. Abu-Dhabi grainstone reservoirs, are observed using seismic attribute techniques. The lack of fossil analogues and the absence of resolvable displacement results in a debate about their origin: differential compaction under low differential isotropic extensional stress or seismic artifact.

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/content/papers/10.3997/2214-4609-pdb.287.1185885
2012-03-04
2021-12-08
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609-pdb.287.1185885
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