• No results found

Bright opportunities in the Dutch offshore

N/A
N/A
Protected

Academic year: 2022

Share "Bright opportunities in the Dutch offshore"

Copied!
1
0
0

Bezig met laden.... (Bekijk nu de volledige tekst)

Hele tekst

(1)

Shallow gas

Bright opportunities in the Dutch offshore

For questions contact info@nlog.nl or exploration@ebn.nl

Seismic data in the northern Dutch offshore shows many shallow amplitude anomalies, often indicating the presence of gas.

Miocene-Pleistocene unconsolidated sands form reservoirs (300-800 m depth), sealed by intercalating clays. Traps are generally low relief anticlines formed by underlying salt domes.

Reservoir properties

*

* Based on fields currently in production

• Expected ultimate recovery around 70 %

• Porosities range between 20-25 %

• Good to excellent permeability (100-500 mD)

Why explore for shallow gas?

• 8 discovered fields of which 4 are currently successfully producing.

• Production rates of 3 million Nm³/day have been achieved in the A12-FA field, making it one of the best producing gas fields in the Netherlands.

• Significant additional potential: many shallow leads identified.

-1200-1000-800-600-400

0 500m

Sand 5 Sand 6 Sand 7 Sand 3

Sand 8 Sand 4

MMU

F07-01

Main target

W Z3FUG2011A (Courtesy Spectrum) N

TWT (ms)

GR

Lead F12- Pliocene Lead

F07/F10- P-01

Licence Open acreage

Seismic data 3D coverage, seismic data in public domain

Seismic response Amplitude anomaly conformable to structure, flat-spot, push-down effect and attenuation

Structure 4-way dip closure

Thickness ~ 50 m (net-to-gross: 85 %) Porosity > 25 %

Gas saturation 60 %

GIIP 0.5 – 0.8 – 1.1 bcm (P90-P50-P10)

Licence Mainly open acreage

Seismic data 3D multiclient survey (Spectrum, 2011)

Seismic response 8 stacked amplitude anomalies of which 2 major bright spots and velocity push-down

Structure Fault-dip closure

Thickness 2 layers, 10 – 20 m each

GIIP 1.0 - 2.5 - 5 bcm (P90-P50-P10)

Information from neighbouring wells F07-01 drilled the edge of the lead – it has gas shows between 300-1000 m

Lead F12-Pliocene Lead F07/F10-P1

-700 -700 -700

-700 -700 -700

-675 -675

-675 -675 -675

-675 -675

-675

-675 -675 -675

-650 -650

-650 -650

-650 -650 -650

-625 -625

-625 -625

-625

-625 -625

-625 -625

-625 -625

-600 -600 -600 -600

-600 -600 -600

-600

-575 -575

-575 -575 -575 -575

-550 -550

-550 -550

-550 -550

-675 -725

-725

-650

-650 -650 -625

-625 -725

-725 -750

-600 -600

-700 -650

-650

-600

-600

-600 -575

-600

-600

-575

-625 -550

-625

F12-02-S1

0 500m -1200

-1000-800-600-400-200

0 500m

F12-02-S1

TWT

SW Z3WES2003A SE

GR -700

-700 -700

-700 -700 -700

-675 -675

-675 -675 -675

-675 -675

-675

-675 -675 -675

-650 -650

-650 -650

-650 -650 -650

-625 -625

-625 -625

-625

-625 -625

-625 -625

-625 -625

-600 -600 -600 -600

-600 -600 -600

-600

-575 -575

-575 -575

-575 -575

-550 -550

-550 -550

-550 -550

-675 -725

-725

-650

-650 -650 -625

-625 -725

-725 -750

-600 -600

-700 -650

-650

-600

-600

-600 -575

-600

-600

-575

-625 -550

-625

F12-02-S1

0 500m -1200

-1000-800-600-400-200

0 500m

F12-02-S1

TWT

SW Z3WES2003A SE

GR

-1200-1000-800-600-400

0 500m

Sand 5 Sand 6 Sand 7 Sand 3

Sand 8 Sand 4

MMU

F07-01

Main target

W Z3FUG2011A (Courtesy Spectrum) N

TWT (ms)

GR 100 ms

Referenties

GERELATEERDE DOCUMENTEN

Shallow Gas in the Dutch Offshore Geological Setting2. London Reference: Kuhlmann et al.,

These bright spots often indicate the presence of shallow gas, defined as gas in unconsolidated sediments of Miocene-Pliocene age.. The traps are generally low relief

a number of wells in the DEAB area and are possibly present in large parts of the the DEFAB area. Charge could come from intra- formational coals or from other source rocks via

For information on Exploration and Production issues and E&P data see the Netherlands Oil and Gas Portal www.nlog.nl Future infrastructure evolution is modeled using

Figure 5 shows the V 0 -distribution for the layer of the Upper and Lower Germanic Trias groups, whereas the kriging standard deviation of this distribution is shown in Figure

Structure 90% • Seismic data hosts abundant amplitude anomalies or bright spots that indicate the presence of gas. • 4-way dip closure, presence of seismic amplitude anomalies

The presence of high contrast seismic facies suggests the presence of coal and allows regional mapping of these

Cenozoic sediments in the northern Dutch offshore host abundant seismic amplitude anomalies or bright spots at the interval of 300-800 m depth, of which several are.. proven to