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© 2013 TGS-NOPEC GEOPHYSICAL COMPANY ASA. ALL RIGHTS RESERVED. 
© 2013 TGS-NOPEC GEOPHYSICAL COMPANY ASA. ALL RIGHTS RESERVED. 
WWW.TGS.COM 
WWW.TGS.COM 
TGS | SOUTH JAVA JANUARY 2013 
TGS | SOUTH JAVA JANUARY 2013 
Legend2D Seismic Survey Lines Multibeam Survey ¯ JAVASUMATRA INDIAN OCEAN 010020030040050Kilometers 
SOUTH JAVA 
MULTI-CLIENT 2D SEISMIC LIBRARY 
AUS 
Tel: +61 8 9480 0000 
Email: info@tgs.com 
For more information, contact TGS at: 
TGS has 8,700 km of long offset seismic and gravity data in the South Java forearc. The data covers the South East Java Basin which is a large frontier petroleum exploration basin, nearly half the size of the Makassar Strait. 
For the first time, the new data reveals a thick package of sediment in a complex geological setting. TGS believes the complexity is a result of its current forearc tectonic regime in addition to its probable earlier history as a rifted fragment of Gondwanaland, as the deeper imaged sediments have similar characteristics to the Mesozoic and Paleozoic of the North West Shelf of Australia. 
There are many questions that will remain unanswered until the area is tested. However, with the current 2D seismic grid of ~25 km, tentative assessments of hydrocarbon prospectivity can be made. In terms of petroleum geology, and despite being undrilled, the main elements of a prospective basin are expected to be present; (i) prospective structures (carbonate reefs and likely sandstone reservoirs) in shallow-medium water depths that are (ii) up-dip migration pathways from potential source rocks in the deeper Outer Forearc Basin and Paleogene half-graben under the Inner Forearc basin.
WWW.TGS.COM © 2013 TGS-NOPEC GEOPHYSICAL COMPANY ASA. ALL RIGHTS RESERVED. 
TGS | SOUTH JAVA JANUARY 2013 
South Java 
South Java Recon 2009 (SJR09) 1,901 
South Java Recon 2010 (SJR10) 4,016 
South Java Infill 2010 (SJi10) 2,783 
Survey 
South Java Recon 
South Java Infill 
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INDIAN OCEAN B 
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¯ 
JAVA 
INDIAN OCEAN 
A 
A' 
2D Km Seismic

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TGS AP Indonesia South Java

  • 1. © 2013 TGS-NOPEC GEOPHYSICAL COMPANY ASA. ALL RIGHTS RESERVED. © 2013 TGS-NOPEC GEOPHYSICAL COMPANY ASA. ALL RIGHTS RESERVED. WWW.TGS.COM WWW.TGS.COM TGS | SOUTH JAVA JANUARY 2013 TGS | SOUTH JAVA JANUARY 2013 Legend2D Seismic Survey Lines Multibeam Survey ¯ JAVASUMATRA INDIAN OCEAN 010020030040050Kilometers SOUTH JAVA MULTI-CLIENT 2D SEISMIC LIBRARY AUS Tel: +61 8 9480 0000 Email: info@tgs.com For more information, contact TGS at: TGS has 8,700 km of long offset seismic and gravity data in the South Java forearc. The data covers the South East Java Basin which is a large frontier petroleum exploration basin, nearly half the size of the Makassar Strait. For the first time, the new data reveals a thick package of sediment in a complex geological setting. TGS believes the complexity is a result of its current forearc tectonic regime in addition to its probable earlier history as a rifted fragment of Gondwanaland, as the deeper imaged sediments have similar characteristics to the Mesozoic and Paleozoic of the North West Shelf of Australia. There are many questions that will remain unanswered until the area is tested. However, with the current 2D seismic grid of ~25 km, tentative assessments of hydrocarbon prospectivity can be made. In terms of petroleum geology, and despite being undrilled, the main elements of a prospective basin are expected to be present; (i) prospective structures (carbonate reefs and likely sandstone reservoirs) in shallow-medium water depths that are (ii) up-dip migration pathways from potential source rocks in the deeper Outer Forearc Basin and Paleogene half-graben under the Inner Forearc basin.
  • 2. WWW.TGS.COM © 2013 TGS-NOPEC GEOPHYSICAL COMPANY ASA. ALL RIGHTS RESERVED. TGS | SOUTH JAVA JANUARY 2013 South Java South Java Recon 2009 (SJR09) 1,901 South Java Recon 2010 (SJR10) 4,016 South Java Infill 2010 (SJi10) 2,783 Survey South Java Recon South Java Infill                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                     101-SJR10 161-SJR10 151-SJR10 131-SJR10 120-SJR10 140-SJR10 110-SJR10 150-SJR10 111-SJR10 130-SJR10141-SJR10 100-SJR10 1-SJR 7-SJR 6-SJR 3-SJR 2-SJR 4-SJR 5-SJR 101-SJi10 500-SJi10 510-SJi10 100-SJi10 410-SJi10 210-SJi10 110-SJi10 310-SJi10 300-SJi10 200-SJi10 400-SJi10 600-SJi10 121-SJR10 ¯ JAVA INDIAN OCEAN B B'                                                                                                                                                                                                                                                                                                                                      131-SJR10 151-SJR10 161-SJR10 101-SJR10 141-SJR10 160-SJR10 121-SJR10 170-SJR10 120-SJR10 140-SJR10 110-SJR10 150-SJR10 111-SJR10 130-SJR10 1-SJR 6-SJR 3-SJR 4-SJR 7-SJR 5-SJR 101-SJi10 610-SJi10 200-SJi10 700-SJi10 600-SJi10 500-SJi10 710-SJi10 510-SJi10 100-SJi10 410-SJi10 800-SJi10 210-SJi10 110-SJi10 310-SJi10 300-SJi10 400-SJi10 ¯ JAVA INDIAN OCEAN A A' 2D Km Seismic