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Alan Pitts

Researcher at University of Camerino

Publications -  13
Citations -  111

Alan Pitts is an academic researcher from University of Camerino. The author has contributed to research in topics: Geology & Structural basin. The author has an hindex of 4, co-authored 9 publications receiving 79 citations.

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Analysis of Fracture Roughness Control on Permeability Using SfM and Fluid Flow Simulations: Implications for Carbonate Reservoir Characterization

TL;DR: In this paper, a complete protocol for fracture surface mapping, roughness evaluation, fracture modeling, fluid flow simulation, and permeability estimation of individual fracture (open or sheared joint/pressure solution seam).
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The August 24th 2016 Accumoli earthquake: surface faulting and Deep-Seated Gravitational Slope Deformation (DSGSD) in the Monte Vettore area

TL;DR: In this paper, the authors bring data on superficial effects and some preliminary considerations about the interaction and possible relationship between surface faulting and the occurrence of Deep-Seated Gravitational Slope Deformation (DSGSD) along the southern and western slope of Monte Vettore.
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Integrating traditional field methods with emerging digital techniques for enhanced outcrop analysis of deep water channel-fill deposits

TL;DR: In this paper, the Gorgoglione Flysch Formation in Southern Italy has been measured and described in detailed stratigraphic sections, providing data for both sedimentological analysis and correlation of the stratigraphy.
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Pore-scale dual-porosity and dual-permeability modeling in an exposed multi-facies porous carbonate reservoir

TL;DR: In this paper, a dual-porosity/permeability (DP/P) model for porous carbonate reservoirs is proposed to evaluate the contribution of macrofracture segments to porosity and connectivity of the pore network.
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Backset lamination produced by supercritical backwash flows at the beachface-shoreface transition of a storm-dominated gravelly beach (middle Pleistocene, central Italy)

TL;DR: In this article, a detailed analysis of mid-Pleistocene beachface-shoreface strata containing sedimentary structures interpreted to have been formed by storm-generated backwash flows during the transition in flow regime from supercritical to subcritical is presented.