Malay Basin, a northward-trending pull-apart extensional rift basin, formed during the late Eocene-early Oligocene and then underwent thermal subsidence and sedimentation during the early Miocene. Reorientation of regional stress fields during the mid-Miocene caused structural inversion resulting in east-west anticlines and half grabens. © 2010 Society of Exploration Geophysicists.
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Ghosh, D., Halim, M. F. A., Brewer, M., Viratno, B., & Darman, N. (2010). Geophysical issues and challenges in Malay and adjacent basins from an e & P perspective. The Leading Edge, 29(4), 436–449. https://doi.org/10.1190/1.3378307