Mineralogical, Petrophysical and Hydromechanical Properties of Reservoirs and Caprocks, 2nd Edition

A special issue of Minerals (ISSN 2075-163X). This special issue belongs to the section "Clays and Engineered Mineral Materials".

Deadline for manuscript submissions: 31 March 2025 | Viewed by 1772

Special Issue Editors

College of Geosciences and Surveying Engineering, China University of Mining and Technology (Beijing), Beijing, China
Interests: coal and coalbed methane; unconventional natural gas/oil resources; sedimentology
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Guest Editor
School of Engineering, University of Aberdeen, Aberdeen AB24 3FX, UK
Interests: digital rock physics; CO2 geological storage and utilization; multiscale porous material characterization
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Guest Editor
Research Institute of Petroleum Exploration and Development, PetroChina, Beijing 100083, China
Interests: shale oil and gas; coal geology; geochemistry

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Guest Editor
ATC Williams Pty, Ltd., Brisbane, QLD 4051, Australia
Interests: coalbed methane; geofluid flow modelling; environmental risk assessment; geomaterial characterization and reconstruction
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Special Issue Information

Dear Colleagues,

Clays and clay-based materials serve as reservoirs and caprocks for energy resources, storage and waste stream sequestration. The mineralogical, petrophysical and geomechanical characteristics are the information required for understanding unconventional origins, accumulation and evolution in different geological settings. This information also provides a foundation for the accurate modeling of subsurface energy engineering applications. The purpose of this Special Issue is to provide a cutting-edge insight to the multiscale mineralogical, petrophysical and geomechanical properties of shales or mudrocks, during coupled thermal, hydrologic, mechanical, chemical or biological processes in natural or anthrogenic activities.

We seek original research that explores the storage potential and evolution of material properties of shale or mudrocks during hydrogen injection, energy-waste containment and sequestration, gas hydrate formation, and geothermal infiltration. Submitted studies are expected to highlight the potential of shale and other clay-based materials to store and transport these fluids under in situ or in-house laboratory conditions. Work that explores the role of mineral distribution within shales in determining material response to CO2, H2, and other fluids of interest are encouraged.

Dr. Yong Li
Dr. Yingfang Zhou
Dr. Zhenhua Jing
Dr. Junjian Wang
Guest Editors

Manuscript Submission Information

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Keywords

  • reservoir characterization
  • caprock integrity
  • mineralogical control
  • petrophysical properties
  • hydromechanical coupling
  • shale gas
  • gas hydrate
  • hydrogen storage
  • CO2 sequestration

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Related Special Issue

Published Papers (2 papers)

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Research

33 pages, 8053 KiB  
Article
Geochemical and Mineralogical Insights into Organic Matter Preservation in the Gondwana and Post-Gondwana Shale of the Lesser Himalayas, Nepal
by Kumar Khadka, Shuxun Sang, Sijie Han, Junjie He, Upendra Baral, Saunak Bhandari and Debashish Mondal
Minerals 2025, 15(1), 63; https://doi.org/10.3390/min15010063 - 9 Jan 2025
Viewed by 458
Abstract
The depositional environments, weathering and provenance, organic matter enrichment, and preservation in the Gondwana and post-Gondwana units of the Lesser Himalayas, Nepal, are studied through geochemical and mineralogical analyses using petrography, X-ray diffraction, XRF, and ICP-MS. Mineralogical findings indicate that shales comprise 55% [...] Read more.
The depositional environments, weathering and provenance, organic matter enrichment, and preservation in the Gondwana and post-Gondwana units of the Lesser Himalayas, Nepal, are studied through geochemical and mineralogical analyses using petrography, X-ray diffraction, XRF, and ICP-MS. Mineralogical findings indicate that shales comprise 55% to 72% clay, 25% to 55% quartz, and less than 10% carbonate minerals, with a significant presence of illite, suggesting a transition from fluvial to shallow marine environments during post-Gondwana deposition. The thin sections of the post-Gondwana sandstone reveal an increase in quartz, feldspar, and plagioclase content, with rounded to sub-angular quartz grains indicating moderate transportation before lithification, resulting from the Indo-Asian collision. Geochemical data, including major, trace, and rare earth elements (REE), along with bivariate discrimination diagrams, reveal distinct environmental changes; Gondwana sediments exhibit oxic, arid conditions with continental provenance, while post-Gondwana deposits indicate humid environments favorable for organic matter enrichment, primarily sourced from felsic-intermediate igneous rocks. The TOC is less than 1 wt.% in the Gondwana and is 0.75 to 2 wt.% in the post-Gondwana shale, indicating better organic matter preservation. The existing geological structural data and the research findings highlight the pivotal role of Himalayan tectonism in enhancing the thermal maturity and hydrocarbon generation potential of organic-rich post-Gondwana shales, attributed to their substantial organic matter content. Full article
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19 pages, 5654 KiB  
Article
A Rock Physics Modeling Method for Metamorphic Rock Reservoirs in Buried Hill
by Hongjian Hao, Guangzhi Zhang and You Zhou
Minerals 2024, 14(9), 892; https://doi.org/10.3390/min14090892 - 30 Aug 2024
Viewed by 898
Abstract
The buried hills of the Archean metamorphic rocks in the Bozhong Depression of the Bohai Bay Basin are the main gas-bearing strata, with burial depths ranging from 4000 m to 5500 m. However, metamorphic rocks have internal structural characteristics, such as diverse mineral [...] Read more.
The buried hills of the Archean metamorphic rocks in the Bozhong Depression of the Bohai Bay Basin are the main gas-bearing strata, with burial depths ranging from 4000 m to 5500 m. However, metamorphic rocks have internal structural characteristics, such as diverse mineral components, oriented arrangement of mineral particles, complex pore connectivity, variable crystal structures, orthogonal development of multiple sets of fractures, and uneven fluid filling. Compared with conventional reservoirs, they have obvious heterogeneity and anisotropy characteristics. Traditional rock physics modeling methods are no longer suitable for predicting the elastic and anisotropic parameters of metamorphic reservoirs. Therefore, we introduced a vector mixed random medium model to calculate the effect of the oriented arrangement of metamorphic rock minerals on the modulus of the rock matrix and introduced a metamorphic factor to describe the impact of metamorphic recrystallization and alteration metasomatism on the elastic modulus of the rock matrix. Practical applications have shown that the new, improved rock physics modeling method can better estimate the S-wave velocity and anisotropy parameters in wells compared to traditional rock physics modeling methods, providing a reliable basis for predicting fractured reservoirs in metamorphic rock at buried hills. Full article
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