Pgce 2010 2010
DOI: 10.3997/2214-4609-pdb.255.85
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Application of High-Resolution Biofacies for Better Depositional Environment Interpretation in the Malay Basin Tertiary Sedimentary Successions

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“…In the deep basin centre the BTU is a much less prominent reflector ( Figure 3A), so the actual basin depth is not always known with certainty. 2) No sediments older than the Eocene are known to exist above the BTU and no older Tertiary sediments occur below it (e.g., Azmi et al, 1996;Morley & Shamsudin, 2006;Shamsudin et al, 2010). Hence, the BTU represents the base of Tertiary sediments overlying the pre-rift basement and filling the basins (Figures 2, 3).…”
Section: Bulletin Of the Geological Society Ofmentioning
confidence: 99%
“…In the deep basin centre the BTU is a much less prominent reflector ( Figure 3A), so the actual basin depth is not always known with certainty. 2) No sediments older than the Eocene are known to exist above the BTU and no older Tertiary sediments occur below it (e.g., Azmi et al, 1996;Morley & Shamsudin, 2006;Shamsudin et al, 2010). Hence, the BTU represents the base of Tertiary sediments overlying the pre-rift basement and filling the basins (Figures 2, 3).…”
Section: Bulletin Of the Geological Society Ofmentioning
confidence: 99%