Characteristics of bottom-simulating reflectors for Hydrate-filled fractured sediments in Krishna–Godavari basin, eastern Indian margin

The bottom-simulating reflector (BSR) is weak and patchy on the seismic section in the Krishna–Godavari basin, eastern Indian margin, where massive gas-hydrates have been recovered at Site 10 of the Indian National Gas-hydrates Program Expedition 01 (NGHP-01). The depth of the BSR near this site is...

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Bibliographic Details
Published in:Journal of petroleum science & engineering 2014-10, Vol.122, p.515-523
Main Authors: Wang, Jiliang, Sain, Kalachand, Wang, Xiujuan, Satyavani, Nittala, Wu, Shiguo
Format: Article
Language:English
Subjects:
Applied sciences
Basins
Crude oil, natural gas and petroleum products
Energy
Exact sciences and technology
Fracture
Fracture mechanics
Free gas
Fuels
Gas hydrate
Geological faults
Krishna–Godavari basin
Methane
Natural gas
Patchy distribution
Reflectors
Rock
Seismic phenomena
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Summary:The bottom-simulating reflector (BSR) is weak and patchy on the seismic section in the Krishna–Godavari basin, eastern Indian margin, where massive gas-hydrates have been recovered at Site 10 of the Indian National Gas-hydrates Program Expedition 01 (NGHP-01). The depth of the BSR near this site is around 160m below the sea floor (mbsf). The average reflection coefficient from the BSR is −0.06, significantly smaller than the common global values of −0.1 to −0.2. The BSR shows a strong lateral variation in amplitudes along the seismic line due to the presence of faults. The methane solubility is modeled using a theoretical model of the gas-hydrates system, and methane concentrations from the pressure core show that the distribution of free gas below BSR is not uniform. A combination of synthetic seismogram analysis and rock physics modeling leads to the conclusion that weak and patchy BSRs are primarily caused by lateral discontinuities induced by the gas-filled fractures below BSRs. The free gas zone is thin and it shows segmented characteristics on the seismic section and acoustic impedance profile that we inverted. Fault zones increase the permeability and therefore trap gas in associated fractures that can scatter seismic energy and create low velocity zones. •Reflection coefficients of BSRs were calculated using impedance contrast and amplitudes.•Lateral discontinuity of BSR is controlled by the faults.•Weak and patchy BSRs are mainly due to gas-filled fractures below the BSR.
ISSN:0920-4105
1873-4715
DOI:10.1016/j.petrol.2014.08.014