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 · first well in the play; fairway unproven
- BEKANTAN-1 — Central basin · 2018 · shallowest oil
- BUNGA TASBIH-1 — Angsi flank · 2020 · MBR+ 2024 award
- PUTERI BASEMENT-1 — Eastern flank · 2020 · fractured granite
Settled · Open · What Would Decide It
- Settled: failed rift (Late Eocene–Oligocene extension) with Miocene inversion making the anticlines (Tjia 1989; Madon 2013) · fill >14 km in the deepest centre (Madon 2021) · two overpressure compartments — basin centre top-OP 1,900–2,000 m sealed by Group F shale, basin flank 2,600–3,000 m sealed by Group L shale (Madon 2004, SPE 88455)
- Open: Western Hinge fairway — one well (2025), not a fairway yet · basement play — one well (Puteri Basement-1, 2020) · deep syn-rift K/L/M play — Group K is both reservoir and source, so charge risk drops while seal risk rises; reservoir below ~3,000 m is compaction-degraded · remaining potential ~2 bboe needs new play concepts (Madon 2021)
- Would decide it: 3D seismic over the Western Hinge · a deep well into K/L/M below ~3,000 m · flank pressure data against the 2,600–3,000 m Group L seal prediction · AVO validation of the deep-Group-M Class III anomaly (currently a low-confidence hypothesis)
Basin in numbers: ~500 × 200 km · ~80,000 km² · fill >14 km · >700 exploration wells · ~40% of Malaysia's hydrocarbon resources (Madon 2021).
Licensing 2026: MTJDA Block A-18-01 PSC — 35-year term effective 1 January 2026, awarded to PC JDA Ltd + PTTEP JDX (50/50); exchanged 14 September 2026 at Gastech, Bangkok (Reuters · The Star · NST, 2026-09-14). The effective date precedes the ceremony.
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+)
- Source rock: Group K source facies TOC 0.35–2.0 wt% (mixed Type II/III); Group L best source, HI 300–400 (Madon 2010, GSM). Drawn TOC ranges are regional synthesis values, not single-well measurements.
- Nomenclature: Group labels follow PETRONAS / Madon 2013; other schemes omit Group C (EPMI) or insert Group G (marine transition) — labels are convention, not load-bearing
- Machine layer: geox://basins/malay-basin/profile · geox://literature/GSM-MADON-2021-MALAY-BASIN (Madon 2021, GSM Bull. 72, doi:10.7186/bgsm72202106)
- 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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