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By the USGS Sumatra Basins Assessment Team: Christopher J. Schenk, Timothy R. Klett, Marilyn E. Tennyson, Tracey J. Mercier, Michael E. Brownfield, Janet K. Pitman, Stephanie B. Gaswirth and Thomas M. Finn. USGS Fact Sheet 2016–3089, December 2016.

Using a geology-based method, the U.S. Geological Survey estimated a mean of 20 trillion cubic feet of undiscovered, technically recoverable gas in the coal beds of the Central and South Sumatra Basin Provinces, Indonesia.

Map of Sumatra showing the Central and South Sumatra basin provinces outlined in black, the two assessment units in blue and orange, the Barisan Mountains and Sumatran Fault, with an inset of Indonesia

The two basin provinces and the two assessment units. Base: National Park Service. Map: USGS.

What was assessed

For each basin the USGS defined a Neogene Coal Total Petroleum System and one assessment unit (AU): the Central Sumatra and South Sumatra Neogene Coalbed Gas AUs. Minable low-rank Neogene coal has been mapped in both basins, and there have been recent attempts to produce coalbed gas in South Sumatra. Coal thickness, composition, gas content and maturity there are well studied.

Three things shaped the assessment:

  1. Low rank: the coals are immature, under 0.5 percent vitrinite reflectance.
  2. Biogenic gas: the gas was made by bacteria, not by heat.
  3. Undersaturated: the coals hold less gas than they could.

Thermally generated coalbed gas was not assessed.

The geology

Both basins are backarc basins, formed behind the subduction zone along Sumatra's margin. In the late Paleogene, the Australian plate pushed obliquely against the Sumatran plate, forming the right-lateral Sumatran Fault and lifting the Barisan Mountains. Sediment shed from those mountains built a clastic wedge eastward across both basins, and the coals formed within it.

Buried only shallowly, the coals stayed thermally immature (except near intrusions). Bacteria made gas within them. Liptinite gives some coals hydrogen indices as high as 300 milligrams hydrocarbon per gram organic carbon, so they might yield liquids — but given their low rank, liquids were not assessed.

The inputs

Drainage areas, success ratios and recoveries per well come from U.S. analogs, especially the biogenic coalbed gas of Wyoming's Powder River Basin:

InputCentral SumatraSouth Sumatra
Potential production area (acres): min / mode / max1,000 / 2,569,000 / 12,844,0001,000 / 4,076,000 / 16,302,000
Production area, calculated mean (acres)5,137,9336,792,833
Well drainage area (acres): min / mode / max40 / 80 / 12040 / 80 / 120
Success ratio (%): min / mode / max (mean)50 / 60 / 70 (60)50 / 70 / 80 (66.7)
Recovery per well, billion cubic feet: min / median / max (mean)0.08 / 0.2 / 0.35 (0.206)0.08 / 0.2 / 0.35 (0.206)
AU probability1.01.0

The results

Fully risked estimates of undiscovered gas, in billion cubic feet (BCFG). F95 means a 95 percent chance of at least that amount; F5, a 5 percent chance.

Assessment unitF95F50F5Mean
Central Sumatra1,8807,21617,1608,119
South Sumatra2,98910,67724,82911,921
Total4,86917,89341,98920,040
  • In all: a mean of 20,040 BCFG (about 20 trillion cubic feet), with a range of 4,869 to 41,989 BCFG.
  • Liquids: none — natural gas liquids were estimated at 0.

More assessments: the USGS Energy Resources Program.

Sources

Based on Assessment of Coalbed Gas Resources of the Central and South Sumatra Basin Provinces, Indonesia, 2016, USGS Fact Sheet 2016–3089, U.S. Geological Survey; a work of the United States government in the public domain. The map and both tables are taken from the fact sheet's PDF; the import had lost them.

LanguagesEnglish

Licence: CC0 1.0 (public domain) · Adapted from pubs.usgs.gov

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