--> Figure 7. Reconstruction of Sabah during Late Miocene to Pliocene shows continued deposition of deltaic to shallow marine clastics following the wide spread regional unconformity during Late Miocene which is known from onshore and offshore data as the Shallow Regional Unconformity (SRU, 8.6 Ma).

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Figure 7. Reconstruction of Sabah during Late Miocene to Pliocene shows continued deposition of deltaic to shallow marine clastics following the wide spread regional unconformity during Late Miocene which is known from onshore and offshore data as the Shallow Regional Unconformity (SRU, 8.6 Ma).