Version 1
: Received: 20 April 2021 / Approved: 21 April 2021 / Online: 21 April 2021 (16:50:54 CEST)
How to cite:
Puttiwongrak, A.; Nufus, S.; Bunprasert, C.; Giao, P.H.; Vann, S.; Suteerasak, T.; Sasaki, N. Compaction Model for Shale in Differences of Geological Ages Using A 3D Empirical Relationship in Northeastern Thailand. Preprints2021, 2021040589. https://doi.org/10.20944/preprints202104.0589.v1
Puttiwongrak, A.; Nufus, S.; Bunprasert, C.; Giao, P.H.; Vann, S.; Suteerasak, T.; Sasaki, N. Compaction Model for Shale in Differences of Geological Ages Using A 3D Empirical Relationship in Northeastern Thailand. Preprints 2021, 2021040589. https://doi.org/10.20944/preprints202104.0589.v1
Puttiwongrak, A.; Nufus, S.; Bunprasert, C.; Giao, P.H.; Vann, S.; Suteerasak, T.; Sasaki, N. Compaction Model for Shale in Differences of Geological Ages Using A 3D Empirical Relationship in Northeastern Thailand. Preprints2021, 2021040589. https://doi.org/10.20944/preprints202104.0589.v1
APA Style
Puttiwongrak, A., Nufus, S., Bunprasert, C., Giao, P.H., Vann, S., Suteerasak, T., & Sasaki, N. (2021). Compaction Model for Shale in Differences of Geological Ages Using A 3D Empirical Relationship in Northeastern Thailand. Preprints. https://doi.org/10.20944/preprints202104.0589.v1
Chicago/Turabian Style
Puttiwongrak, A., Thongchai Suteerasak and Nophea Sasaki. 2021 "Compaction Model for Shale in Differences of Geological Ages Using A 3D Empirical Relationship in Northeastern Thailand" Preprints. https://doi.org/10.20944/preprints202104.0589.v1
Abstract
Shales are well known for their strong anisotrophic properties. The classical Athy’s model on the exponential porosity reduction with the depth commonly uses based on localities only. Shale compaction curve affects the results of the basin modeling as it is important input data, thus the standard compaction curve of shales needs to be established. This study provided a new data and complies available data of Thailand shales to propose the new empirical relationship among porosity, burial depth, and geological age. The numerical data of the geological time were estimated by the application from the relationship of velocity and depth in each geological ages. The variation of the Thailand shale data due to the different geological ages was found in this study. Finally, the standard curve of shale compaction proposed by Puttiwongrak et al. [9] was examined and confirmed by this research findings.
Keywords
Shale compaction; Geological age; Thailand shale; Compaction model; Standard curve
Subject
Environmental and Earth Sciences, Atmospheric Science and Meteorology
Copyright:
This is an open access article distributed under the Creative Commons Attribution License which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited.
