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Geosciences, Volume 15, Issue 9 (September 2025) – 3 articles

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12 pages, 54717 KB  
Communication
Deep-Water Volcaniclastic Layers in the Late Messinian Apennines Foreland Basin Unravel the First Calc-Alkaline Rhyolitic Eruption in the Central Italy Magmatic System
by Michela Principi, Fabio Arzilli, Giulia Bosio, Daniele Morgavi and Claudio N. Di Celma
Geosciences 2025, 15(9), 330; https://doi.org/10.3390/geosciences15090330 (registering DOI) - 23 Aug 2025
Abstract
A package of upper Messinian volcaniclastic layers (UMVLs), exposed in the deep-water foreland basin system of the central Apennines (Italy), is the volcanic product of a rhyolitic eruption dated to 5.5 Ma. These UMVLs are an important marker for stratigraphic correlations along the [...] Read more.
A package of upper Messinian volcaniclastic layers (UMVLs), exposed in the deep-water foreland basin system of the central Apennines (Italy), is the volcanic product of a rhyolitic eruption dated to 5.5 Ma. These UMVLs are an important marker for stratigraphic correlations along the central Apennines foreland basin system, but their source is still debated and poorly understood. Italian Plio-Quaternary volcanism exhibits significant petrological and geochemical variability, causing debate over magma genesis and differentiation. Investigating the magmatic evolution of central Italy is crucial for understanding one of the most complex geodynamic settings on Earth. The first evidence of efficient magma differentiation, producing eruptible calc-alkaline rhyolitic magmas, is the San Vincenzo eruption at 4.41 Ma. Our sedimentological and petrological analyses of UMVL exposures indicate a possible volcanic source in the northeastern Tuscany Magmatic Province. This discovery implies a developed transcrustal magma reservoir system and suggests that efficient magma differentiation capable of producing eruptible calc-alkaline rhyolitic magma occurred about one million years earlier than the San Vincenzo eruption, marking these UMVLs as the first rhyolitic eruption associated with Italian Plio-Quaternary volcanism. Full article
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24 pages, 12181 KB  
Article
Surface and Subsurface Behavior of a Natural Gas Storage Site over Time: The Case of the Cornegliano Gas Field (Po Plain, Northern Italy)
by Stefano Lombardi, Andrea Di Giulio, Giuseppe Gervasi, Chiara Cavalleri, Andrew Johnson, Patrick Egermann, Arnaud Lange and Giovanni Toscani
Geosciences 2025, 15(9), 329; https://doi.org/10.3390/geosciences15090329 - 23 Aug 2025
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Abstract
Foredeep basins often host significant natural gas reservoirs within siliciclastic successions, as exemplified by the Po Plain (Northern Italy), one of Europe’s largest foredeep basins. Here, numerous depleted gas reservoirs have been successfully converted into underground gas storage (UGS) facilities. For safe and [...] Read more.
Foredeep basins often host significant natural gas reservoirs within siliciclastic successions, as exemplified by the Po Plain (Northern Italy), one of Europe’s largest foredeep basins. Here, numerous depleted gas reservoirs have been successfully converted into underground gas storage (UGS) facilities. For safe and efficient storage operations, detailed reservoir characterization and continuous monitoring of surface and subsurface effects are crucial. This study investigates the Cornegliano Laudense reservoir during its first 5–7 years as a UGS facility, employing an integrated monitoring approach that combines traditional methods (InSAR for surface deformation, microseismic monitoring) with innovative techniques (Pulsed Neutron Log-PNL). The results clearly illustrate and quantify the significant increase in storage capacity over a relatively short operational period, primarily driven by the progressive displacement of formation water by injected gas. Despite increased stored gas volumes, monitoring revealed no adverse effects on surface stability or subsurface seismicity. This integrated methodology demonstrates substantial potential for refining predictive models, optimizing storage efficiency, and enhancing sustainable management practices for underground gas storage operations. Full article
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21 pages, 20939 KB  
Article
Identification and Application of Preferred Seepage Channels in Turbidite Lobe Reservoirs of Formation A in Z Oilfield
by Changhai Li
Geosciences 2025, 15(9), 328; https://doi.org/10.3390/geosciences15090328 - 23 Aug 2025
Viewed by 45
Abstract
Turbidite lobe reservoirs represent critical deep-sea hydrocarbon targets, yet preferred seepage channels within them remain poorly characterized. This paper establishes a method for identifying internal preferred seepage channels in turbidite lobe reservoirs using data including seismic, core, thin section, logging, and production performance, [...] Read more.
Turbidite lobe reservoirs represent critical deep-sea hydrocarbon targets, yet preferred seepage channels within them remain poorly characterized. This paper establishes a method for identifying internal preferred seepage channels in turbidite lobe reservoirs using data including seismic, core, thin section, logging, and production performance, combined with neural network technology. A neural network model for predicting reservoir productivity types can be obtained by taking the average logging data of reservoir intervals as input and the reservoir productivity types categorized by meter oil production index calculated by actual production data as the target. By applying the trained neural network model and inputting actual logging attribute model, the reservoir productivity types of single wells are obtained. Using the attribute model of natural gamma ray, acoustic, neutron, density, deep lateral, and shallow lateral logs, which are built by using the actual logging data and Sequential Gaussian Simulation, and supervising with the single well reservoir productivity type, the reservoir productivity type at any position in the reservoir can be predicted. It predicts their spatial distribution characteristics, reveals the genetic mechanism of preferred seepage channels, and discusses the significance of identifying preferred seepage channels for oilfield development. The results show that the reservoir productivity types in the study area can be divided into five categories with progressive improvement in productivity (A, B, C, D, and E) according to the increase in oil production index per meter, among which Type E reservoirs represent typical preferred seepage channels. The attribute model of reservoir productivity types indicates that, horizontally, types E and B are locally developed in the study area, while types D, C, and A are widely distributed. The preferred seepage channels can be divided into two types according to the shape: zonal (length to width > 2:1) and sheet-like (length to width ≤ 2:1). Vertically, types C, D, and E are relatively well-developed in layers III and IV, whereas types A and B are more common in layers I and II. The vertical combination patterns of preferred seepage channels reveal four types, including homogeneous, bottom-dominated, top-dominated, and interbedded patterns. The formation of preferred seepage channels is influenced by both sedimentary and diagenetic processes, and sedimentary is the most important controlling factors. The identification of preferred seepage channels in turbidite lobe reservoirs is of great significance for formulating development policies and tapping remaining oil. Full article
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