Geological cross-section — Malay Basin
WHERE arif-fazil.com / earth / malay-basin / cross-section
WHAT NW–SE transect, ~500 km
SCALE vertical ~32× exaggerated
LAYERS 8 groups · 4 founder wells
◈ Spatial Locator · NW–SE Transect A–A' (~500 km)
TRANSECT: A (Terengganu Granite) → A' (Central Malay Basin Flank)
ORIENTATION: NW–SE (140° Strike)
REAL-TIME COORDS: 5.5000° N, 104.5000° E
PIPE: Macrostrat Tile API (Live)
Tectonic Phases · 4 Acts
- L. Eoc.Syn-rift — Group L/M lacustrine fill, source rocks deposited
- E. Mio.Transition / sag — Group K, J, I fluvial-deltaic
- M–L. Mio.Inversion — normal faults reverse, anticlines form
- Plio–Rec.Post-inversion — regional subsidence, marine transgression
Reservoir Quality · Group A→M
- Group D: Claystone, sandstone, coal · Deltaic · Excellent
- Group E: Sandstone (Dulang field) · Excellent
- Group F: Sandstone, claystone, coal · Good + regional seal
- Group H: Lower coastal plain · Excellent–Good
- Group I: Siltstone (Angsi, Sotong) · Good
- Group K: Coarse sandstone · Deep play · Fair
- Porosity: 12–28% · Perm: 10–1000 mD
Founder Wells (4) · Plays Tested
- LEBAH EMAS-1 — Western Hinge · 2025 · new play fairway
- BEKANTAN-1 — Central basin · 2018 · shallowest oil
- BUNGA TASBIH-1 — Angsi flank · 2024 · MBR+ field
- PUTERI BASEMENT-1 — Eastern flank · 2020 · fractured granite
Provenance · Group A→M
- Stratigraphy: Madon 2013, Ishlah 2015, PETRONAS convention
- Tectonics: Tjia 1989 (inversion), Madon 2013 (sag)
- Plays: Scherer 2018 (anticline), PETRONAS MPM 2024 (MBR+)
- Wells: /earth/data/wells.json (sovereign canon, F10)
- F7 humility: body shapes are schematics, well positions are basin-level not step-out
Cross-section · SRTM topography via open-meteo.com · Stratigraphy from PETRONAS Group A–M convention · Tectonics from Cenozoic failed rift + Miocene inversion · Vertical exaggeration ~32×. F7 humility: body shapes are interpretive schematics, not seismic picks.
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