Earth Sciences

| Peer-Reviewed |

Present-Day Two-Dimension Maturity History Modelling of Source Rocks from the Central Region of the Andaman Sea Back Arc Depression

Received: 01 September 2019    Accepted: 05 October 2019    Published: 17 October 2019
Views:       Downloads:

Share This Article

Abstract

Basin modelling is an essential research tool that aids geologists improve the description and analysis of subsurface activity. The central region of the Andaman Sea back arc basin is a potential oil and gas prospect. Herein, two-dimension present-day maturity models are constructed from four seismic sections of the study area using Basin Mod software (Platte River Associates, Inc. of USA). Designated study areas are the South to North Moattama Basin, western Moattama to the Mergui Shelf, Western to Eastern Moattama basin centres through Eastern Moattama basin centre to the Eastern section of Mergui basin and Eastern Andaman Sea Basin to Western Mergui Basin. The two-dimension (2D) maturity models are generated from known data burial and geothermal data. Vitrinite Reflectance (Ro%) which is the main variable in determining source rock (s) maturity showed that the source units were within the oil (0.5% ≤ Ro ≤ 1%) and gas (1.3% ≤ Ro ≤ 4.5%) and had commenced generation of some quantities of hydrocarbons. Data analyzed revealed that most portions of the Oligocene and Lower Miocene shales source units in all study areas buried below 2000 m are matured to generate oil and / or gas. The outcome of modelling also indicated that source units from the Moattama Basin center and the Mergui Basin were mostly matured to produce some form of hydrocarbons, principally gas or dry gas. However, no oil expulsion into limestone reservoirs was observed; only gas or dry gas.

DOI 10.11648/j.earth.20190805.12
Published in Earth Sciences (Volume 8, Issue 5, October 2019)

This article belongs to the Special Issue Geoscience and Energy

Page(s) 268-276
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), 2024. Published by Science Publishing Group

Keywords

Maturity History Model, Andaman Sea, Vitrinite Reflectance, Back Arc Depression, Basin Modelling, Seismic Profile, Oil and Gas Windows

References
[1] Rivas, S., Grimmer, J. O. W., Alaminos, A., Navarro, J., 2016. Basin Modelling at the Songkhla Basin (Gulf of Thailand) or: How Many Source Rocks Do I Have? AAPG/SEG International Conference and Exhibition, Barcelona, Spain.
[2] Olaru, R., Krézsek, C., Rainer, T. M., Ungureanu, C., Turi, V., Ionescu, G., Tari, G., 2018. 3D Basin Modelling of Oligocene –Miocene Maikop Source Rocks Offshore Romania and in the Western Black Sea. Journal of Petroleum Geology, Vol. 41 (3), pp 351-366.
[3] Christine Yallup, C., Scotchman, J., 2018. Basin Modelling Offshore Guyana: Predicting Source Rock Risk. Exploration Insights, Halliburton Landmark.
[4] Quaye, J. A., Xu, S., 2013. One Dimensional Evolution History Modelling Of Source Rocks in the Central. Int. J. Eng. Sci. Res. Technol. 2, 8.
[5] Polachan, S., Racey, A., 1994. Stratigraphy of the Mergui Basin, Andaman Sea: Implications for Petroleum Exploration. J. Pet. Geol. 17, 373–406. https://doi.org/10.1111/j.1747-5457.1994.tb00147.x
[6] Fagelnour, M., Gamil, I., El Toukhy, M., Gharieb, A., & Saad, H., 2019. Source Rock Potentiality, Basin Modeling, and Oil to Source Correlation in Northern Shushan Basin, Western Desert, Egypt. Offshore Mediterranean Conference.
[7] Rao, P. S., Kamesh Raju, K. A., Ramprasad, T., Nagender Nath, B., Ramalingeswara Rao, B., Rao, C. M., Nair, R. R., 1996. Evidence for hydrothermal activity in the Andaman Backarc Basin. Curr. Sci. 70, 379–385.
[8] Gary Scaife Spectrum; Andy Billings Hornet Geoconsulting, 2010. GeoExpro regional Andaman basin. GEO ExPro Explor. Asia.
[9] Information Handling Services Energy, 2012. The Moattama Basin, Basin Monitor.
[10] Polachan, S., Pradidtan, S., Tongtaow, C., Janmaha, S., Intarawijitr, K., Sangsuwan, C., 1991. Development of Cenozoic basins in Thailand. Mar. Pet. Geol. 8, 84–97. https://doi.org/10.1016/0264-8172(91)90047-5
[11] Polachan, S., 1988. The geological evolution of the Mergui Basin, S. E. Andaman Sea, Thailand. Ph.D. Thesis, Univ. London. University of London.
[12] Yang, W., Escalona, A., 2011. Basin modelling and source rock evaluation in the Guyana Basin. EAGE vol. 8.
[13] Magoon, L. B., Dow, W. G., 1994. The petroleum system - from source to trap, The petroleum system - from source to trap. AAPG.
[14] Lopatin, N. V, 1971. Temperature and geologic time as factors in coalification. Akad. Nauk. seies Geol. Izwestiya 3, 95–106.
[15] Waples, D. W., 1980. Time and temperature in petroleum formation: application of Lopatin’s method to petroleum exploration. Am. Assoc. Pet. Geol. Bull. 64, 916–926.
Author Information
  • School of Energy Resources, China University of Geosciences, Beijing, China

  • Faculty of Earth Resources, China University of Geosciences, Wuhan, China

  • Department of Earth Science and Resources, China University of Geosciences, Beijing, China

Cite This Article
  • APA Style

    Jonathan Atuquaye Quaye, Sihuang Xu, Yanick Brice Lemdjou. (2019). Present-Day Two-Dimension Maturity History Modelling of Source Rocks from the Central Region of the Andaman Sea Back Arc Depression. Earth Sciences, 8(5), 268-276. https://doi.org/10.11648/j.earth.20190805.12

    Copy | Download

    ACS Style

    Jonathan Atuquaye Quaye; Sihuang Xu; Yanick Brice Lemdjou. Present-Day Two-Dimension Maturity History Modelling of Source Rocks from the Central Region of the Andaman Sea Back Arc Depression. Earth Sci. 2019, 8(5), 268-276. doi: 10.11648/j.earth.20190805.12

    Copy | Download

    AMA Style

    Jonathan Atuquaye Quaye, Sihuang Xu, Yanick Brice Lemdjou. Present-Day Two-Dimension Maturity History Modelling of Source Rocks from the Central Region of the Andaman Sea Back Arc Depression. Earth Sci. 2019;8(5):268-276. doi: 10.11648/j.earth.20190805.12

    Copy | Download

  • @article{10.11648/j.earth.20190805.12,
      author = {Jonathan Atuquaye Quaye and Sihuang Xu and Yanick Brice Lemdjou},
      title = {Present-Day Two-Dimension Maturity History Modelling of Source Rocks from the Central Region of the Andaman Sea Back Arc Depression},
      journal = {Earth Sciences},
      volume = {8},
      number = {5},
      pages = {268-276},
      doi = {10.11648/j.earth.20190805.12},
      url = {https://doi.org/10.11648/j.earth.20190805.12},
      eprint = {https://download.sciencepg.com/pdf/10.11648.j.earth.20190805.12},
      abstract = {Basin modelling is an essential research tool that aids geologists improve the description and analysis of subsurface activity. The central region of the Andaman Sea back arc basin is a potential oil and gas prospect. Herein, two-dimension present-day maturity models are constructed from four seismic sections of the study area using Basin Mod™ software (Platte River Associates, Inc. of USA). Designated study areas are the South to North Moattama Basin, western Moattama to the Mergui Shelf, Western to Eastern Moattama basin centres through Eastern Moattama basin centre to the Eastern section of Mergui basin and Eastern Andaman Sea Basin to Western Mergui Basin. The two-dimension (2D) maturity models are generated from known data burial and geothermal data. Vitrinite Reflectance (Ro%) which is the main variable in determining source rock (s) maturity showed that the source units were within the oil (0.5% ≤ Ro ≤ 1%) and gas (1.3% ≤ Ro ≤ 4.5%) and had commenced generation of some quantities of hydrocarbons. Data analyzed revealed that most portions of the Oligocene and Lower Miocene shales source units in all study areas buried below 2000 m are matured to generate oil and / or gas. The outcome of modelling also indicated that source units from the Moattama Basin center and the Mergui Basin were mostly matured to produce some form of hydrocarbons, principally gas or dry gas. However, no oil expulsion into limestone reservoirs was observed; only gas or dry gas.},
     year = {2019}
    }
    

    Copy | Download

  • TY  - JOUR
    T1  - Present-Day Two-Dimension Maturity History Modelling of Source Rocks from the Central Region of the Andaman Sea Back Arc Depression
    AU  - Jonathan Atuquaye Quaye
    AU  - Sihuang Xu
    AU  - Yanick Brice Lemdjou
    Y1  - 2019/10/17
    PY  - 2019
    N1  - https://doi.org/10.11648/j.earth.20190805.12
    DO  - 10.11648/j.earth.20190805.12
    T2  - Earth Sciences
    JF  - Earth Sciences
    JO  - Earth Sciences
    SP  - 268
    EP  - 276
    PB  - Science Publishing Group
    SN  - 2328-5982
    UR  - https://doi.org/10.11648/j.earth.20190805.12
    AB  - Basin modelling is an essential research tool that aids geologists improve the description and analysis of subsurface activity. The central region of the Andaman Sea back arc basin is a potential oil and gas prospect. Herein, two-dimension present-day maturity models are constructed from four seismic sections of the study area using Basin Mod™ software (Platte River Associates, Inc. of USA). Designated study areas are the South to North Moattama Basin, western Moattama to the Mergui Shelf, Western to Eastern Moattama basin centres through Eastern Moattama basin centre to the Eastern section of Mergui basin and Eastern Andaman Sea Basin to Western Mergui Basin. The two-dimension (2D) maturity models are generated from known data burial and geothermal data. Vitrinite Reflectance (Ro%) which is the main variable in determining source rock (s) maturity showed that the source units were within the oil (0.5% ≤ Ro ≤ 1%) and gas (1.3% ≤ Ro ≤ 4.5%) and had commenced generation of some quantities of hydrocarbons. Data analyzed revealed that most portions of the Oligocene and Lower Miocene shales source units in all study areas buried below 2000 m are matured to generate oil and / or gas. The outcome of modelling also indicated that source units from the Moattama Basin center and the Mergui Basin were mostly matured to produce some form of hydrocarbons, principally gas or dry gas. However, no oil expulsion into limestone reservoirs was observed; only gas or dry gas.
    VL  - 8
    IS  - 5
    ER  - 

    Copy | Download

  • Sections