Study on Organic Identification of Black Shale in Bokor Formation, Kampot Province, Cambodia

Ratha Heng; Sopheap Pech; Sreymean Sio; Chandoeun Eng; Chanmoly Or

doi:doi:10.11648/j.ogce.20221004.11

| Peer-Reviewed

Study on Organic Identification of Black Shale in Bokor Formation, Kampot Province, Cambodia

Ratha Heng, Sopheap Pech, Sreymean Sio, Chandoeun Eng, Chanmoly Or

Published in International Journal of Oil, Gas and Coal Engineering (Volume 10, Issue 4)

Received: 1 August 2022 Accepted: 24 August 2022 Published: 16 September 2022

Views: Downloads:

Download PDF

Share This Article

Twitter
Linked In
Facebook

Abstract

Organic petrology is the key study to identify the favorable geological condition of black shale as a hydrocarbon source rock. The study aims to identify the organic matter types in the black shale of Bokor Formation, Kampot province. Three outcrop cross-sections (Phnom Khley, Phnom Chakrey, and Phnom Monprey), which extend from the West to the East of Kampot province, were investigated for stratigraphic sequences, sedimentary structures/textures, fossil contents through fieldwork observation. Rock sampling was conducted to performed polish pellet for organic petrology. The result demonstrated that the western part consisted of repeated sequences of thin laminated shale layers interbedded with massive sandstone layers. In the eastern part, the shale layers are continually deposited as a thick bedding with fossils of syringopora, crinoid, and foraminifera, which indicates a low energy flow environment during sediment deposition. Organic petrologic analysis in shale samples revealed that alginate and bituminite were dominantly found shale samples in the Phnom Khley section, whereas macrinite and vitrinite were observed in Phnom Monprey and Phnom Chakrey, respectively. The presence of alginate, bituminite, and macrinite, suggest a potential for hydrocarbon source rock. The maceral types, such as alginite, bituminite, micrinite, and vitrinite, indicate deposition in periodically oxygenated bottom water and a sulfidic marine water environment. Based on the existing macerals and cubic pyrite that presented in the collected samples, those source rocks are suggested as thermally mature petroleum source rock.

Published in	International Journal of Oil, Gas and Coal Engineering (Volume 10, Issue 4)
DOI	10.11648/j.ogce.20221004.11
Page(s)	90-96
Creative Commons	This is an Open Access article, distributed under the terms of the Creative Commons Attribution 4.0 International License (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted use, distribution and reproduction in any medium or format, provided the original work is properly cited.
Copyright	Copyright © The Author(s), 2022. Published by Science Publishing Group

Keywords

Organic Identification, Black Shake, Bokor Formation, Cambodia

References

[1]	Asl, S. a. (2016). Microfacies Patterns and Depositional Environments of the Sarvak Formation in the Abadan Plain, Southwest of Zagros, Iran.. Open Journal of Geology, 6, 201-209. doi: doi.org/10.4236/ojg.2016.63018.
[2]	Er, C., Li, Y., Zhao, J., Wang, R., & Wei, Z. (2016). Characteristics of lacustrine organic-rich shale: A case study of the Chang 7 member, Triassic Yanchang Formation, Ordos Basin, China. Journal of Natural Gas Geoscience, 1-13. doi: dx.doi.org/10.1016/j.jnggs.2016.04.001.
[3]	Fishman, N. S., Hackley, P. C., Lowers, H. A., Hill, R. J., Egenhoff, S. O., Eberl, D. D., & Blum, A. E. (2012). The nature of porosity in organic-rich mudstones of the Upper Jurassic Kimmeridge Clay Formation, North Sea, offshore United Kingdom. International Journal of Coal Geology, 32-50. doi: dx.doi.org/10.1016/j.coal.2012.07.012.
[4]	FYHN, M. B., LARS, S. A., LARS, O. B., PAUL, H. N., PHAN, F. G., LUONG, T. D., & FREI, T. H. (2010). Palaeocene early Eocene inversion of the Phuquoc Kampot Som Basin: SE Asian deformation associated with the suturing of Luconia. Journal of the Geological Society, 167, 281–295. doi: 10.1144/0016-76492009-039.
[5]	Hongdong Wang, M. L. (2019). Intelligent Identification of Maceral Components of Coal Based on Image Segmentation and Classification. applied sciences, 9. doi: doi: 10.3390/app9163245.
[6]	Hower, J. C., O'Keefe, J. M., Eble, C. F., Volk, T. J., Richardson, A. R., Satterwhite, A. B., &... & Kostova, I. J. (2011). Notes on the origin of inertinite macerals in coals: Funginite associations with cutinite and suberinite. International Journal of Coal Geology, 85 (1), 186-190.
[7]	I. Coronado, S. R. (2014). Carboniferous auloporids from the Iberian Peninsula: palaeocology, diversity, and spatio-temporal distribution. Journal of Iberian Geology, 1, 40. doi: doi.org/10.5209/rev_JIGE.2014.v40.n1.44088.
[8]	Jahan, S., & Uddin, A. (2022). Organic petrography and depositional environments of the upper Eocene Kopili Shale, Bengal Basin, Bangladesh. Journal of Asian Earth Sciences, 17. doi: doi.org/10.1016/j.jaesx.2022.100092.
[9]	Jahan, S., Ashraf, U., C, P. J., & E, S. C. (2017). Petroleum source-rock evaluation of upper Eocene Kopili Shale, Bengal Basin, Bangladesh. International Journal of Coal Geology, 71-79. doi: doi.org/10.1016/j.coal.2017.02.002.
[10]	Killops, S., & Killops, V. (2005). Introduction to Organic Geochemistry. Victoria, Australia: Blackwell Science.
[11]	Liu, B., Schieber, J., & Mastalerz, M. (2017). Combined SEM and reflected light petrography of organic matter in the New Albany Shale (Devonian-Mississippian) in the Illinois Basin: A perspective on organic pore development with thermal maturation. International Journal of Coal Geology, 57-72. doi: doi.org/10.1016/j.coal.2017.11.002.
[12]	Mao, C., Yasuhiro, Y., & Matsuoka., T. (2014). A preliminary assessment of geological CO₂ storage in Cambodia. International Journal of Greenhouse Gas Control., 19–33. doi: dx.doi.org/10.1016/j.ijggc.2014.08.016.
[13]	PICKETT, J. W. (2016). Settlement strategy in Symplectophyllum (Cnidaria, Rugosa). GEOLOGICA BELGICA, 19. doi: doi.org/10.20341/gb.2015.015.
[14]	Potter, P., Maynard, J., & Depetris, P. (2005). Mud and mudstones: Introduction and overview. Berlin-Heidelberg-New York: Springer.
[15]	Ratha, H., Chanmoly, O., Chandoeun, E., & Pech, S. (2022). Depositional Environment of Black Shale in Bokor Formation, Kampot Province, Cambodia. Smart Technology for Sustainable Economic Growth (p. 4). Phnom Penh: Reasearch and Innovation Center.
[16]	Vysotsky, V. R. (1994). The Petroleum Geology of Cambodia. J. Pet, 195–210. doi: 10.1144/0016-76492009-03x.

Cite This Article

Plain Text BibTeX RIS

APA Style

Ratha Heng, Sopheap Pech, Sreymean Sio, Chandoeun Eng, Chanmoly Or. (2022). Study on Organic Identification of Black Shale in Bokor Formation, Kampot Province, Cambodia. International Journal of Oil, Gas and Coal Engineering, 10(4), 90-96. https://doi.org/10.11648/j.ogce.20221004.11

Copy | Download

ACS Style

Ratha Heng; Sopheap Pech; Sreymean Sio; Chandoeun Eng; Chanmoly Or. Study on Organic Identification of Black Shale in Bokor Formation, Kampot Province, Cambodia. Int. J. Oil Gas Coal Eng. 2022, 10(4), 90-96. doi: 10.11648/j.ogce.20221004.11

Copy | Download

AMA Style

Ratha Heng, Sopheap Pech, Sreymean Sio, Chandoeun Eng, Chanmoly Or. Study on Organic Identification of Black Shale in Bokor Formation, Kampot Province, Cambodia. Int J Oil Gas Coal Eng. 2022;10(4):90-96. doi: 10.11648/j.ogce.20221004.11

Copy | Download

@article{10.11648/j.ogce.20221004.11,
  author = {Ratha Heng and Sopheap Pech and Sreymean Sio and Chandoeun Eng and Chanmoly Or},
  title = {Study on Organic Identification of Black Shale in Bokor Formation, Kampot Province, Cambodia},
  journal = {International Journal of Oil, Gas and Coal Engineering},
  volume = {10},
  number = {4},
  pages = {90-96},
  doi = {10.11648/j.ogce.20221004.11},
  url = {https://doi.org/10.11648/j.ogce.20221004.11},
  eprint = {https://article.sciencepublishinggroup.com/pdf/10.11648.j.ogce.20221004.11},
  abstract = {Organic petrology is the key study to identify the favorable geological condition of black shale as a hydrocarbon source rock. The study aims to identify the organic matter types in the black shale of Bokor Formation, Kampot province. Three outcrop cross-sections (Phnom Khley, Phnom Chakrey, and Phnom Monprey), which extend from the West to the East of Kampot province, were investigated for stratigraphic sequences, sedimentary structures/textures, fossil contents through fieldwork observation. Rock sampling was conducted to performed polish pellet for organic petrology. The result demonstrated that the western part consisted of repeated sequences of thin laminated shale layers interbedded with massive sandstone layers. In the eastern part, the shale layers are continually deposited as a thick bedding with fossils of syringopora, crinoid, and foraminifera, which indicates a low energy flow environment during sediment deposition. Organic petrologic analysis in shale samples revealed that alginate and bituminite were dominantly found shale samples in the Phnom Khley section, whereas macrinite and vitrinite were observed in Phnom Monprey and Phnom Chakrey, respectively. The presence of alginate, bituminite, and macrinite, suggest a potential for hydrocarbon source rock. The maceral types, such as alginite, bituminite, micrinite, and vitrinite, indicate deposition in periodically oxygenated bottom water and a sulfidic marine water environment. Based on the existing macerals and cubic pyrite that presented in the collected samples, those source rocks are suggested as thermally mature petroleum source rock.},
 year = {2022}
}

Copy | Download

TY  - JOUR
T1  - Study on Organic Identification of Black Shale in Bokor Formation, Kampot Province, Cambodia
AU  - Ratha Heng
AU  - Sopheap Pech
AU  - Sreymean Sio
AU  - Chandoeun Eng
AU  - Chanmoly Or
Y1  - 2022/09/16
PY  - 2022
N1  - https://doi.org/10.11648/j.ogce.20221004.11
DO  - 10.11648/j.ogce.20221004.11
T2  - International Journal of Oil, Gas and Coal Engineering
JF  - International Journal of Oil, Gas and Coal Engineering
JO  - International Journal of Oil, Gas and Coal Engineering
SP  - 90
EP  - 96
PB  - Science Publishing Group
SN  - 2376-7677
UR  - https://doi.org/10.11648/j.ogce.20221004.11
AB  - Organic petrology is the key study to identify the favorable geological condition of black shale as a hydrocarbon source rock. The study aims to identify the organic matter types in the black shale of Bokor Formation, Kampot province. Three outcrop cross-sections (Phnom Khley, Phnom Chakrey, and Phnom Monprey), which extend from the West to the East of Kampot province, were investigated for stratigraphic sequences, sedimentary structures/textures, fossil contents through fieldwork observation. Rock sampling was conducted to performed polish pellet for organic petrology. The result demonstrated that the western part consisted of repeated sequences of thin laminated shale layers interbedded with massive sandstone layers. In the eastern part, the shale layers are continually deposited as a thick bedding with fossils of syringopora, crinoid, and foraminifera, which indicates a low energy flow environment during sediment deposition. Organic petrologic analysis in shale samples revealed that alginate and bituminite were dominantly found shale samples in the Phnom Khley section, whereas macrinite and vitrinite were observed in Phnom Monprey and Phnom Chakrey, respectively. The presence of alginate, bituminite, and macrinite, suggest a potential for hydrocarbon source rock. The maceral types, such as alginite, bituminite, micrinite, and vitrinite, indicate deposition in periodically oxygenated bottom water and a sulfidic marine water environment. Based on the existing macerals and cubic pyrite that presented in the collected samples, those source rocks are suggested as thermally mature petroleum source rock.
VL  - 10
IS  - 4
ER  -

Copy | Download

Author Information

Ratha Heng

Research and Innovation Center, Institute of Technology of Cambodia, Phnom Penh, Cambodia
Sopheap Pech

Research and Innovation Center, Institute of Technology of Cambodia, Phnom Penh, Cambodia
Sreymean Sio

Research and Innovation Center, Institute of Technology of Cambodia, Phnom Penh, Cambodia
Chandoeun Eng

Faculty of Geo-resources and Geotechnical Engineering, Institute of Technology of Cambodia, Phnom Penh, Cambodia
Chanmoly Or

Research and Innovation Center, Institute of Technology of Cambodia, Phnom Penh, Cambodia

Download PDF

Sections

Plain Text BibTeX RIS

APA Style

Ratha Heng, Sopheap Pech, Sreymean Sio, Chandoeun Eng, Chanmoly Or. (2022). Study on Organic Identification of Black Shale in Bokor Formation, Kampot Province, Cambodia. International Journal of Oil, Gas and Coal Engineering, 10(4), 90-96. https://doi.org/10.11648/j.ogce.20221004.11

Copy | Download

ACS Style

Ratha Heng; Sopheap Pech; Sreymean Sio; Chandoeun Eng; Chanmoly Or. Study on Organic Identification of Black Shale in Bokor Formation, Kampot Province, Cambodia. Int. J. Oil Gas Coal Eng. 2022, 10(4), 90-96. doi: 10.11648/j.ogce.20221004.11

Copy | Download

AMA Style

Ratha Heng, Sopheap Pech, Sreymean Sio, Chandoeun Eng, Chanmoly Or. Study on Organic Identification of Black Shale in Bokor Formation, Kampot Province, Cambodia. Int J Oil Gas Coal Eng. 2022;10(4):90-96. doi: 10.11648/j.ogce.20221004.11

Copy | Download

@article{10.11648/j.ogce.20221004.11,
  author = {Ratha Heng and Sopheap Pech and Sreymean Sio and Chandoeun Eng and Chanmoly Or},
  title = {Study on Organic Identification of Black Shale in Bokor Formation, Kampot Province, Cambodia},
  journal = {International Journal of Oil, Gas and Coal Engineering},
  volume = {10},
  number = {4},
  pages = {90-96},
  doi = {10.11648/j.ogce.20221004.11},
  url = {https://doi.org/10.11648/j.ogce.20221004.11},
  eprint = {https://article.sciencepublishinggroup.com/pdf/10.11648.j.ogce.20221004.11},
  abstract = {Organic petrology is the key study to identify the favorable geological condition of black shale as a hydrocarbon source rock. The study aims to identify the organic matter types in the black shale of Bokor Formation, Kampot province. Three outcrop cross-sections (Phnom Khley, Phnom Chakrey, and Phnom Monprey), which extend from the West to the East of Kampot province, were investigated for stratigraphic sequences, sedimentary structures/textures, fossil contents through fieldwork observation. Rock sampling was conducted to performed polish pellet for organic petrology. The result demonstrated that the western part consisted of repeated sequences of thin laminated shale layers interbedded with massive sandstone layers. In the eastern part, the shale layers are continually deposited as a thick bedding with fossils of syringopora, crinoid, and foraminifera, which indicates a low energy flow environment during sediment deposition. Organic petrologic analysis in shale samples revealed that alginate and bituminite were dominantly found shale samples in the Phnom Khley section, whereas macrinite and vitrinite were observed in Phnom Monprey and Phnom Chakrey, respectively. The presence of alginate, bituminite, and macrinite, suggest a potential for hydrocarbon source rock. The maceral types, such as alginite, bituminite, micrinite, and vitrinite, indicate deposition in periodically oxygenated bottom water and a sulfidic marine water environment. Based on the existing macerals and cubic pyrite that presented in the collected samples, those source rocks are suggested as thermally mature petroleum source rock.},
 year = {2022}
}

Copy | Download

TY  - JOUR
T1  - Study on Organic Identification of Black Shale in Bokor Formation, Kampot Province, Cambodia
AU  - Ratha Heng
AU  - Sopheap Pech
AU  - Sreymean Sio
AU  - Chandoeun Eng
AU  - Chanmoly Or
Y1  - 2022/09/16
PY  - 2022
N1  - https://doi.org/10.11648/j.ogce.20221004.11
DO  - 10.11648/j.ogce.20221004.11
T2  - International Journal of Oil, Gas and Coal Engineering
JF  - International Journal of Oil, Gas and Coal Engineering
JO  - International Journal of Oil, Gas and Coal Engineering
SP  - 90
EP  - 96
PB  - Science Publishing Group
SN  - 2376-7677
UR  - https://doi.org/10.11648/j.ogce.20221004.11
AB  - Organic petrology is the key study to identify the favorable geological condition of black shale as a hydrocarbon source rock. The study aims to identify the organic matter types in the black shale of Bokor Formation, Kampot province. Three outcrop cross-sections (Phnom Khley, Phnom Chakrey, and Phnom Monprey), which extend from the West to the East of Kampot province, were investigated for stratigraphic sequences, sedimentary structures/textures, fossil contents through fieldwork observation. Rock sampling was conducted to performed polish pellet for organic petrology. The result demonstrated that the western part consisted of repeated sequences of thin laminated shale layers interbedded with massive sandstone layers. In the eastern part, the shale layers are continually deposited as a thick bedding with fossils of syringopora, crinoid, and foraminifera, which indicates a low energy flow environment during sediment deposition. Organic petrologic analysis in shale samples revealed that alginate and bituminite were dominantly found shale samples in the Phnom Khley section, whereas macrinite and vitrinite were observed in Phnom Monprey and Phnom Chakrey, respectively. The presence of alginate, bituminite, and macrinite, suggest a potential for hydrocarbon source rock. The maceral types, such as alginite, bituminite, micrinite, and vitrinite, indicate deposition in periodically oxygenated bottom water and a sulfidic marine water environment. Based on the existing macerals and cubic pyrite that presented in the collected samples, those source rocks are suggested as thermally mature petroleum source rock.
VL  - 10
IS  - 4
ER  -

Copy | Download