Pore pressure study in the Irpinia area (Southern Apennines, Italy)

TL;DR

This study investigates subsurface pore pressure regimes in the Irpinia region of Italy, revealing spatial variations and identifying zones of overpressure linked to geological formations and seismic activity.

Contribution

It provides a detailed methodology for analyzing pore pressures using well data and correlates pressure regimes with geological features and gas occurrences in a tectonically active area.

Findings

Carbonate successions are mainly hydrostatic.

Shale-rich successions show moderate overpressure.

Highest overpressures occur in evaporitic deposits and Pliocene shales.

Abstract

Subsurface pore pressure studies are crucial for understanding the geomechanical behaviours of the geological formations and for preventing the failure conditions of the rocks. Although the interplay between pore pressure changes and rock deformation is nowadays widely treated in the literature, the magnitude and the distribution of the fluid pressure regimes at depth is not completely clear, especially in those areas, such as the fold and thrust belts, characterised by a complex tectonostratigraphic setting. The proposed study deals with the subsurface fluid dynamics of the Irpinia region, located in the Southern Apennines (Italy) and marked by intense tectonic activity and seismicity. In that area, the most recent and notable Italian earthquake occurred in November 1980 (6.9 Mw) and caused significant damage and loss of life. Irpinia area is also a site of deep gas rising to the surface and exhibits clear correlations between crustal deformation and groundwater circulation. The pressure analysis herein proposed has been performed using direct and indirect pressure measurements collected from 13 hydrocarbon exploration wells available in open source. It provides a detailed description of the methodology used to identify where overpressures develop within the sediments of both autochthonous and allochthonous layers. It also investigates the relationship between pore pressures, gas occurrences found at well sites, and the possible sources of overpressures. The results show that the carbonate successions of the South-Apennines and Apulian Platforms are characterized by predominantly hydrostatic pressure regimes, while the shale-rich successions of the Lagonegrese pelagic basin and the Miocene-Pliocene foredeep basin locally demonstrate moderate overpressured gradients. Finally, the highest overpressures are observed in the evaporitic deposits and Pliocene shales.