Inversion tectonics in the Malay Basin: evidence and timing of events
Pre-Oligocene half grabens of the Malay Basin suggest a tensional origin, while their uparched/folded Oligocene to upper Miocene sedimentary fills have been accepted to represent a laterstage compressional deformation. This structural inversion probably took place in middle to late Miocene time. The...
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Geological Society of Malaysia
1994
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