Impacts of Himalayan tectonism on Eocene gas shale and its pore structure within the Lesser Himalayas, Nepal: Insights for shale gas accumulation and preservation

This study investigates the complex relationship between organic matter (OM), tectonic deformation, and pore structure development in Eocene Bhainskati shale within the Lesser Himalayan Foreland Basin, Nepal, to assess its implications for shale gas accumulation and preservation. We hypothesize that tectonic deformation and variations in organic matter have a significant impact on pore size distribution, connectivity, and gas retention, thereby influencing shale gas potential. We characterized pore types and quantified pore size distributions using scanning electron microscopy (SEM), mercury intrusion capillary pressure (MICP) techniques, and low-pressure gas adsorption methods. Our findings indicate a predominance of mesopores (1–10 nm range, with a notable peak at 4 nm), suggesting substantial contributions to surface area from micropores and fine mesopores. Thermal maturity negatively impacts porosity and surface area. At the same time, tectonic activity enhances microfracture development, increasing permeability and gas transport, particularly in the Surkhet area, which exhibits higher pore volume and specific surface area than the Tansen area. Tectonic forces shift the shale from brittle to ductile behavior, altering pore connectivity. Himalayan tectonic forces significantly influence shale structure, pore sizes, gas preservation, and migration, enhancing gas adsorption by increasing surface area but posing challenges due to potential gas escape along faults and folds. Understanding the impact of tectonic activity on shale deformation in similar basins within the Himalayas and the adjacent region is vital for assessing shale gas potential and optimizing exploration strategies in tectonically active Nepal Himalayan regions. This study highlights the dual role of tectonics in both promoting and complicating the formation, accumulation, and preservation of shale gas reservoirs, offering critical insights for future exploration efforts.

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Publication Details

Journal
Petroleum Science
Published
2025-09-23
DOI
https://doi.org/10.1016/j.petsci.2025.09.026
Citations
1
Primary Topic
Hydrocarbon exploration and reservoir analysis
Type
article
Field-Weighted Citation Impact
0.86
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article

Impacts of Himalayan tectonism on Eocene gas shale and its pore structure within the Lesser Himalayas, Nepal: Insights for shale gas accumulation and preservation

Upendra Baral, Shuxun Sang, Ji Lai He, Xiaozhi Zhou et al.
1 citations
Petroleum Science
Hydrocarbon exploration and reservoir analysis
0.86
article

Impacts of Himalayan tectonism on Eocene gas shale and its pore structure within the Lesser Himalayas, Nepal: Insights for shale gas accumulation and preservation

Upendra Baral, Shuxun Sang, Ji Lai He, Xiaozhi Zhou, Kumar Khadka, Saunak Bhandari, Sijie Han, Shiqi Liu, Debashish Mondal
article en
1 citations

Abstract

This study investigates the complex relationship between organic matter (OM), tectonic deformation, and pore structure development in Eocene Bhainskati shale within the Lesser Himalayan Foreland Basin, Nepal, to assess its implications for shale gas accumulation and preservation. We hypothesize that tectonic deformation and variations in organic matter have a significant impact on pore size distribution, connectivity, and gas retention, thereby influencing shale gas potential. We characterized pore types and quantified pore size distributions using scanning electron microscopy (SEM), mercury intrusion capillary pressure (MICP) techniques, and low-pressure gas adsorption methods. Our findings indicate a predominance of mesopores (1–10 nm range, with a notable peak at 4 nm), suggesting substantial contributions to surface area from micropores and fine mesopores. Thermal maturity negatively impacts porosity and surface area. At the same time, tectonic activity enhances microfracture development, increasing permeability and gas transport, particularly in the Surkhet area, which exhibits higher pore volume and specific surface area than the Tansen area. Tectonic forces shift the shale from brittle to ductile behavior, altering pore connectivity. Himalayan tectonic forces significantly influence shale structure, pore sizes, gas preservation, and migration, enhancing gas adsorption by increasing surface area but posing challenges due to potential gas escape along faults and folds. Understanding the impact of tectonic activity on shale deformation in similar basins within the Himalayas and the adjacent region is vital for assessing shale gas potential and optimizing exploration strategies in tectonically active Nepal Himalayan regions. This study highlights the dual role of tectonics in both promoting and complicating the formation, accumulation, and preservation of shale gas reservoirs, offering critical insights for future exploration efforts.

Petroleum ScienceVol. 23(1)
China University of Mining and Technology (CN), Government of Nepal (NP), Mountain Medicine Society of Nepal (NP), Institute of Tibetan Plateau Research (CN)
Openalex Percentile: Top 25%
Hydrocarbon exploration and reservoir analysis
0.86
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