Sains Malaysiana 44(4)(2015):
571–579
Petroleum Source Rock Properties of the Neogene Bhuban
Shales, Bengal Basin, Bangladesh
(Pencirian Punca Batuan Petroleum di Syal Neogene Bhuban, Lembangan
Bengal, Bangladesh)
MD. FARHADUZZAMAN1*, WAN HASIAH ABDULLAH1 & MD. AMINUL ISLAM2
1Department
of Geology, Faculty of Science, University of Malaya, 50603 Kuala Lumpur
Malaysia
2Department of
Petroleum Geoscience, Faculty of Science, Universiti Brunei Darussalam, Gadong
BE1410, Brunei Darussalam
Diserahkan: 10 Jun 2013/Diterima: 18 November 2014
ABSTRACT
The present study evaluates the petroleum source rock generation
potential of the Neogene Bhuban shales from Bangladesh. Organic geochemical and
organic petrological methods were used for analyzing 11 drill core samples from
4 gas fields in the basin. Source rock potential, maceral composition, organic
matter abundance, biomarker distribution, thermal maturity, hydrocarbon
generation and depositional environment were evaluated. Kerogen in the studied
shale samples is classified mainly as Type III with lesser amounts of Type II.
Vitrinite is the dominant maceral group observed in the analyzed Bhuban samples
followed by liptinite and inertinite. Vitrinite reflectance, Tmax and biomarker
parameters indicate the thermal maturity ranges from just pre-oil window to
mid-oil window. Based on its total organic carbon (TOC), extractable organic
matter (EOM)
and hydrogen index (HI), the analyzed Bhuban shales are ranked as
mainly poor to fair source rocks but with good gas generation potential. The
dominant terrestrial environment prevailed during the deposition of the studied
Bhuban shales while the condition was sub-oxic as indicated by cross-plots of
pristane versus phytane and sterane versus pristane/phytane ratios.
Keywords: Bengal Basin; Bhuban shale; hopane; hydrocarbon
potential; sterane
ABSTRAK
Kajian ini membincangkan penilaian batuan punca bagi petroleum sampel
syal Bhuban Neogene dari Bangladesh. Geokimia organik dan petrologi
organik telah digunakan untuk menganalisis 11 sampel teras gerudi
daripada 4 medan gas di kawasan tersebut. Potensi batuan punca,
komposisi maseral, kedapatan bahan organik, taburan petanda biologi,
kematangan terma penjanaan hidrokarbon dan persekitaran pengenapan
dinilai. Kerogen dalam sampel syal yang dikaji kebanyakannya dikelaskan
sebagai Jenis III dengan jumlah Jenis II yang lebih kecil. Vitrinit
adalah kumpulan maseral yang dominan dalam sampel Bhuban yang dianalisis
diikuti oleh liptinit dan inertinit. Pantulan vitrinit, Tmax dan
parameter bio penanda menunjukkan kematangan terma daripada hanya
pra-minyak ke tingkap-minyak pertengahan. Berdasarkan data TOC, EOM dan HI, syal Bhuban yang dianalisis
kebanyakannya dinilai sebagai miskin ke sederhana sebagai batuan
sumber dengan potensi penjanaan gas yang baik. Persekitaran daratan
dominan semasa pengenapan syal Bhuban dikaji manakala keadaan pengenapan
adalah sub-oksik sebagaimana yang dicadangkan berdasarkan plot pristana
melawan fitana dan sterana melawan nisbah pristana/fitana.
Kata kunci: Hopana;
lembangan Bengal; potensi hidrokarbon; sterana, syal Bhuban
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*Pengarang
untuk surat-menyurat; email: farhad.geo@siswa.um.edu.my
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