Response of incised valley systems with sea level change during late pleistocene-holocene at Penyu Basin, Sunda Shelf
Valley incision and infilling, as well as the fluvial response of uppermost Pilong formation in penyu basin located offshore of present-day Pahang River Basin, Peninsular Malaysia during late pleistocene-mid holocene was studied.
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| Language: | English |
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Terengganu:
Universiti Malaysia Terengganu,
2016.
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