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Deepened Knowledge Shallow Gas

in the Netherlands

Poster 5 Prospex 2011 mjvg

Introduction

Shallow gas is defined as gas in unconsolidated, low pressure Tertiary sandstone formations. Depths typically range from 400 to 1000 ms. Sourcing can be thermogenic, biogenic or a mixture of the two.

Why exploring for shallow gas now?

1. First shallow gas fields in production The occurrence of shallow gas

in the Dutch offshore sector has been known for a long time.

However, only recently we have started producing shallow gas (2009).

There are 8 proven shallow gas fields in the Netherlands of which 3 are currently producing,

accounting for ~8.5 BCM recoverable.

The earlier identified risk of sand and water production, given the unconsolidated reservoir, has been shown to be no problem.

2. New 3D seismic

The northern Dutch offshore is largely covered by 3D seismic data and in 2012 a new 3D seismic survey will become available in the DEF blocks (Fugro).

3. Marginal field tax incentive applicable

For details, see poster “Fallow acreage incentive in the Netherlands and marginal E&P projects”.

4. Significant shallow gas potential

Currently, 59 shallow prospects of interest have been identified (classification type 1-3) in the northern Dutch offshore (A-H blocks). A significant number of these prospects are situated in open acreage.

Bright spot classification

Different types of bright spots have been identified.

The classification is a measure of potential (ranking):

1 A12-FA type BS

2 F02a-Pliocene type BS 3 Flat medium size BS 4 Foreset BS

5 Elongated BS 6 Very shallow BS 7 Flat small size BS

1 A12-FA type bright spot

• Relatively flat

• Stacked levels

• Depth 300-800 m

2 F02a-Pliocene type bright spot

• Relatively large column in anticlinal structure

• Additional minor stacked bright levels

• Depth 550-800 m

3 Flat medium size bright spot

• Relatively flat

• Partly fault bound

• Few stacked bright levels

• Area > 2 km2

NU_base

N_base CK_base

ZE_base

Prospectivity?

Bright spot area (km2) Nr. of bright spots

88

18 44

148

40 139

7

34

A12-FA type BS F02a-Pliocene type BS Flat medium size BS Flat small size BS

In the northern part of the Dutch offshore, many amplitude anomalies can be identified on seismic. These so-called bright spots indicate the presence of shallow gas.

The traps are generally low relief anticlines related to salt domes. Shales act as partial seal; only limited gas columns can exist. Venting to shallower units often creates a stacked pattern of bright spots containing separate gas columns.

For information on Exploration and Production issues and E&P data see the Netherlands Oil and Gas Portal www.nlog.nl & www.ebn.nl

Exploring for shallow gas

From Bright Spot to Volume

Northern Dutch offshore

N N

BS = bright spot Southern offshore will

be investigated in 2012

Joint Industry Project Shallow Gas TNO (2011)

Rock and reservoir properties of bright spots are poorly constrained, hampering effective exploration, production and hazard assessment.

The relation with depositional setting (i.e. reservoir type) is unclear.

TNO is developing:

• A 3D basin scale reservoir model of the shallow gas occurrences where key external controls can be linked directly to depositional elements (fans, clinoforms, topsets, etc.) calibrated by extensive existing and new well data.

• A migration and charging model for the shallow gas reservoirs based on present-day fluid dynamic data and basin modelling to predict (economically profitable or hazardous) shallow gas occurrences.

Referenties

GERELATEERDE DOCUMENTEN

Projec�on: UTM, Zone 31N Map datum: ED50 November 18, 2015. (c)

applied for Open area. Licenced

applied for Open area. Licenced

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

The prospects per formation type, are split for offshore and onshore and are characterized by the number of prospects and the associated Expectation (MSV X POS) volume of gas..

a 3D, basin scale reservoir model of the shallow gas occurrences (Eridanos D, tunnel-valleys) where key external controls can be linked directly to depositional elements