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Open Access

A modeling-inversion methodology for source rocks based on clay-kerogen lamination and pore geometry

Cong Luoa, Jun-Wei Chenga, Jing Baa ( ), José Carcionea,b, Lu-Lu Chena
School of Earth Sciences and Engineering, Hohai University, Nanjing, 211100, Jiangsu, China
National Institute of Oceanography and Applied Geophysics – OGS, Trieste, 34010, Italy

Edited by Meng-Jiao Zhou

Peer review under the responsibility of China University of Petroleum (Beijing).

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Abstract

Source rocks (shales) exhibit different geometric pore types and considerable anisotropy caused by the preferential orientation of the clay and kerogen layers, which is not accounted for in classical rock-physics models. Pore geometry can be effectively studied through the aspect ratio, and in this study, we use the aspect ratio to characterize different pore geometries. Then, we consider a pore connectivity index as well as a lamination index associated with these orientations. An inclusion-based theory (differential effective medium and self-consistent approximation) and the Brown-Korringa equations are used in the modeling approach. The results show that the indices as well as the aspect ratio of the connected pores significantly affect the elastic properties. We propose an inversion method to invert these three parameters simultaneously from experimental vertical P- and S-wave velocities using a global optimization algorithm. The method is applied to well log and seismic data from the Longmaxi shale reservoir in southwest China to verify its predictive ability.

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Petroleum Science
Pages 4462-4491

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Cite this article:
Luo C, Cheng J-W, Ba J, et al. A modeling-inversion methodology for source rocks based on clay-kerogen lamination and pore geometry. Petroleum Science, 2025, 22(11): 4462-4491. https://doi.org/10.1016/j.petsci.2025.06.021

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Received: 21 November 2024
Revised: 18 May 2025
Accepted: 30 June 2025
Published: 05 July 2025
© 2025 The Authors.

This is an open access article under the CC BY license (http://creativecommons.org/licenses/by/4.0/).