1887

Abstract

Inversion tectonics of pre-existing extensional basins produces characteristic hydrocarbon traps. The positive reactivation along N-S oblique extensional paleo-lineaments in both the Central-Southern Apennines of Italy and in the Adriatic foreland occurs and shows different structural geometries with respect to NW-SE extensional paleo-lineaments, in which short-cut thrusts were developed.

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/content/papers/10.3997/2214-4609.20148899
2012-06-04
2020-05-27
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.20148899
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