Exploitation Chengdu

1 Introduction P-wave impedance (Zp) is a key parameter that links seismic data to rock physical properties such as porosity, permeability and fluid saturation (Brown 1996; Karimi 2015; Bashir et al. 2024). The accuracy of Zp inversion directly affects the reliability of lithology interpretation and reservoir characterization (Russell and Hampson 1991; Hampson et al. 2005; Larsen et al. 2006; Morozov and Ma 2009; Liu et al. 2018; Imran et al. 2020; Bashir et al. 2021, 2024).

F., Y.Dong, J.He, et al. 2026. “Fault-Controlled Thermal Convection Dolomitization and Fluid Evolution Triggered by Emeishan Large Igneous Province.” Basin Research38, no. 3: e70117. Lu, https://doi.org/10.1111/bre.70117. Conflicts of Interest The authors declare no conflicts of interest. Data Availability Statement The data that supports the findings of this study are available in the of this article.

Conflicts of Interest The authors declare no conflicts of interest. Data Availability Statement The data supporting this article have been included as part of the Supporting Information Figure , Tables . Peer Review The peer review history for this article is available at https://www.webofscience.com/api/gateway/wos/peer-review/10.1002/gj.70160. Supporting Information Filename Description gj70160-sup-0001-FigureS1.pdfPDF document, 4.2 MB Figure S1: Results of all Pb contamination.