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Application of chemostratigraphy to the Mungaroo Formation, NW Shelf K.T. Ratcliffe and A.M. Wright Chemostrat Inc, Houston, USA P. Montgomery, Chevron Energy Technology Company, Aberdeen, UK A. Palfrey, A. Vonk, J. Vermeulen and M. Barrett Chevron Australia Pty Ltd, Perth WA 6000

Application of chemostratigraphy to the Mungaroo Formation, NW Shelf K.T. Ratcliffe and A.M. Wright Chemostrat Inc, Houston, USA P. Montgomery, Chevron

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Page 1: Application of chemostratigraphy to the Mungaroo Formation, NW Shelf K.T. Ratcliffe and A.M. Wright Chemostrat Inc, Houston, USA P. Montgomery, Chevron

Application of chemostratigraphy to the Mungaroo Formation, NW Shelf

K.T. Ratcliffe and A.M. WrightChemostrat Inc, Houston, USA

P. Montgomery, Chevron Energy Technology Company,

Aberdeen, UK

A. Palfrey, A. Vonk, J. Vermeulen and M. Barrett

Chevron Australia Pty Ltd, Perth WA 6000

Page 2: Application of chemostratigraphy to the Mungaroo Formation, NW Shelf K.T. Ratcliffe and A.M. Wright Chemostrat Inc, Houston, USA P. Montgomery, Chevron

Paper Outline

What is chemostratigraphy ?

Sample preparation and analysis

Background to study

Mungaroo Formation in the Gorgon Field

Why use chemostratigraphy on the Mungaroo Formation ?

Chemostratigraphic characterisation

Paleoclimate indicators

Provenance indicators

Chemostratigraphic correlation

What this means for stratigraphy in the Mungaroo Formation

Page 3: Application of chemostratigraphy to the Mungaroo Formation, NW Shelf K.T. Ratcliffe and A.M. Wright Chemostrat Inc, Houston, USA P. Montgomery, Chevron

What is Chemostratigraphy ?

The characterization, or ‘fingerprinting’ of sedimentary units using inorganic geochemical data

This characterization enables the identification of chemostratigraphic units on the basis of elemental concentrations, ratios or systematic trends

Inorganic geochemistry of sediments is highly variable and sensitive to subtle changes in source composition, facies, weathering or diagenesis. Therefore apparently uniform successions may show primary differences in the chemistry of constituent minerals, particularly in accessory phases

The keys to a successful chemostratigraphic study is to understand the association of elemental chemistry and geology

Page 4: Application of chemostratigraphy to the Mungaroo Formation, NW Shelf K.T. Ratcliffe and A.M. Wright Chemostrat Inc, Houston, USA P. Montgomery, Chevron

Why use Chemostratigraphy in the Mungaroo?

The Mungaroo Formation is a typical fluvial system, so tends to be poor in biostratigraphic and palynological markers

Wireline log correlations can be inaccurate since the tendency is to make simple layer-cake correlations and tie sandstones that occur in similar stratigraphic positions and have similar e-log signatures

Seismic correlations do not provide sufficient resolution and can often be ambiguous

Chemostratigraphy offers the potential to refine biostratigraphic and palynological stratigraphies, can remove ambiguity in seismic interpretations and shows that the Mungaroo is not layercake

Page 5: Application of chemostratigraphy to the Mungaroo Formation, NW Shelf K.T. Ratcliffe and A.M. Wright Chemostrat Inc, Houston, USA P. Montgomery, Chevron

Gorgon Field

Location and stratigraphy

Page 6: Application of chemostratigraphy to the Mungaroo Formation, NW Shelf K.T. Ratcliffe and A.M. Wright Chemostrat Inc, Houston, USA P. Montgomery, Chevron

Gorgon-1

Depth(m)

3600

3700

3800

3900

4000

4100

4200

4300

4400

GammaAPI

Pal

ynol

.ba

se T

R6A

top

Car

nian

Lith

stra

tBa

rrow

Gro

upM

unga

roo

For

mat

ion

Gorgon-3

Depth(m)

3500

3600

3700

3800

3900

4000

4100

4200

4300

4400

4500

GammaAPI

Pal

ynol

.ba

se T

r6A

top

Car

nian

Lith

stra

tBa

rrow

Gro

upM

unga

roo

For

mat

ion

Central Gorgon 1

Depth(m)

3600

3700

3800

3900

4000

4100

4200

4300

4400

4500

4600

GammaAPI

Pal

ynol

.ba

se T

r6A

top

Car

nian

Lith

stra

tB

arro

w G

roup

Mun

garo

o F

orm

atio

n

North Gorgon-6

Depth(m)

3500

3600

3700

3800

3900

4000

4100

4200

4300

GammaAPI

Pal

ynol

.ba

se T

r7A

iiito

p T

r6A

base

Tr6

A

Lith

stra

tB

arro

wG

roup

Mun

garo

o F

orm

atio

n

North Gorgon-1

Depth(m)

3400

3500

3600

3700

3800

3900

4000

4100

4200

4300

4400

4500

GammaAPI

Pal

ynol

.to

p T

r7Ai

icba

se T

r7A

iiito

p T

r6A

base

Tr6

Ato

p C

arni

an

Lith

stra

tB

arro

wG

roup

Mun

garo

o F

orm

atio

n

North Gorgon-2

Depth(m)

3400

3500

3600

3700

3800

3900

4000

4100

4200

4300

4400

GammaAPI

Pal

ynol

.to

p T

r7Ai

icba

se T

r7A

iiito

p T

r6A

base

Tr6

A

Lith

stra

tB

arro

wG

roup

Mun

garo

o F

orm

atio

n

North Gorgon-4

Depth(m)

3500

3600

3700

3800

3900

4000

4100

GammaAPI

Pal

ynol

.T

r8D

iiiT

r7A

iia

Lith

stra

tB

arro

wG

roup

Mun

garo

o F

orm

atio

n

North Gorgon-3

Depth(m)

3400

3500

3600

3700

3800

3900

4000

4100

4200

4300

GammaAPI

Pal

ynol

.T

r8C

iiiT

r8D

iT

r8D

iii

Lith

stra

tBa

rrow

Gro

upBr

igad

ier

Form

atio

nM

unga

roo

For

mat

ion

Gorgon-1

Depth(m)

3600

3700

3800

3900

4000

4100

4200

4300

4400

GammaAPI

Pal

ynol

.ba

se T

R6A

top

Car

nian

Lith

stra

tB

arro

w G

rou

pM

unga

roo

For

mat

ion

Gorgon-3

Depth(m)

3500

3600

3700

3800

3900

4000

4100

4200

4300

4400

4500

GammaAPI

Pal

ynol

.ba

se T

r6A

top

Car

nian

Lith

stra

tB

arro

wG

roup

Mun

garo

o F

orm

atio

n

Central Gorgon 1

Depth(m)

3600

3700

3800

3900

4000

4100

4200

4300

4400

4500

4600

GammaAPI

Pal

ynol

.ba

se T

r6A

top

Car

nian

Lith

stra

tB

arro

w G

roup

Mun

garo

o F

orm

atio

n

North Gorgon-6

Depth(m)

3500

3600

3700

3800

3900

4000

4100

4200

4300

GammaAPI

Pal

ynol

.ba

se T

r7A

iiito

p T

r6A

base

Tr6

A

Lith

stra

tB

arro

wG

roup

Mun

garo

o F

orm

atio

n

North Gorgon-1

Depth(m)

3400

3500

3600

3700

3800

3900

4000

4100

4200

4300

4400

4500

GammaAPI

Pal

ynol

.to

p T

r7Ai

icba

se T

r7A

iiito

p T

r6A

base

Tr6

Ato

p C

arni

an

Lith

stra

tB

arro

wG

roup

Mun

garo

o F

orm

atio

n

North Gorgon-2

Depth(m)

3400

3500

3600

3700

3800

3900

4000

4100

4200

4300

4400

GammaAPI

Pal

ynol

.to

p T

r7Ai

icba

se T

r7A

iiito

p T

r6A

base

Tr6

A

Lith

stra

tB

arro

wG

roup

Mun

garo

o F

orm

atio

n

North Gorgon-4

Depth(m)

3500

3600

3700

3800

3900

4000

4100

GammaAPI

Pal

ynol

.T

r8D

iiiT

r7A

iia

Lith

stra

tB

arro

wG

roup

Mun

garo

o F

orm

atio

n

North Gorgon-3

Depth(m)

3400

3500

3600

3700

3800

3900

4000

4100

4200

4300

GammaAPI

Pal

ynol

.T

r8C

iiiT

r8D

iT

r8D

iii

Lith

stra

tB

arro

wG

roup

Brig

adie

rF

orm

atio

nM

unga

roo

For

mat

ion

Gorgon-1

Depth(m)

3600

3700

3800

3900

4000

4100

4200

4300

4400

GammaAPI

Pal

ynol

.ba

se T

R6A

top

Car

nian

Lith

stra

tB

arro

w G

rou

pM

unga

roo

For

mat

ion

Gorgon-3

Depth(m)

3500

3600

3700

3800

3900

4000

4100

4200

4300

4400

4500

GammaAPI

Pal

ynol

.ba

se T

r6A

top

Car

nian

Lith

stra

tB

arro

wG

roup

Mun

garo

o F

orm

atio

n

Central Gorgon 1

Depth(m)

3600

3700

3800

3900

4000

4100

4200

4300

4400

4500

4600

GammaAPI

Pal

ynol

.ba

se T

r6A

top

Car

nian

Lith

stra

tB

arro

w G

roup

Mun

garo

o F

orm

atio

n

North Gorgon-6

Depth(m)

3500

3600

3700

3800

3900

4000

4100

4200

4300

GammaAPI

Pal

ynol

.ba

se T

r7A

iiito

p T

r6A

base

Tr6

A

Lith

stra

tB

arro

wG

roup

Mun

garo

o F

orm

atio

n

North Gorgon-1

Depth(m)

3400

3500

3600

3700

3800

3900

4000

4100

4200

4300

4400

4500

GammaAPI

Pal

ynol

.to

p T

r7Ai

icba

se T

r7A

iiito

p T

r6A

base

Tr6

Ato

p C

arni

an

Lith

stra

tB

arro

wG

roup

Mun

garo

o F

orm

atio

n

North Gorgon-2

Depth(m)

3400

3500

3600

3700

3800

3900

4000

4100

4200

4300

4400

GammaAPI

Pal

ynol

.to

p T

r7Ai

icba

se T

r7A

iiito

p T

r6A

base

Tr6

A

Lith

stra

tB

arro

wG

roup

Mun

garo

o F

orm

atio

n

North Gorgon-4

Depth(m)

3500

3600

3700

3800

3900

4000

4100

GammaAPI

Pal

ynol

.T

r8D

iiiT

r7A

iia

Lith

stra

tB

arro

wG

roup

Mun

garo

o F

orm

atio

n

North Gorgon-3

Depth(m)

3400

3500

3600

3700

3800

3900

4000

4100

4200

4300

GammaAPI

Pal

ynol

.T

r8C

iiiT

r8D

iT

r8D

iii

Lith

stra

tB

arro

wG

roup

Brig

adie

rF

orm

atio

nM

unga

roo

For

mat

ion

Gorgon-1

Depth(m)

3600

3700

3800

3900

4000

4100

4200

4300

4400

GammaAPI

Pal

ynol

.ba

se T

R6A

top

Car

nian

Lith

stra

tB

arro

w G

rou

pM

unga

roo

For

mat

ion

Gorgon-3

Depth(m)

3500

3600

3700

3800

3900

4000

4100

4200

4300

4400

4500

GammaAPI

Pal

ynol

.ba

se T

r6A

top

Car

nian

Lith

stra

tB

arro

wG

roup

Mun

garo

o F

orm

atio

n

Central Gorgon 1

Depth(m)

3600

3700

3800

3900

4000

4100

4200

4300

4400

4500

4600

GammaAPI

Pal

ynol

.ba

se T

r6A

top

Car

nian

Lith

stra

tB

arro

w G

roup

Mun

garo

o F

orm

atio

n

North Gorgon-6

Depth(m)

3500

3600

3700

3800

3900

4000

4100

4200

4300

GammaAPI

Pal

ynol

.ba

se T

r7A

iiito

p T

r6A

base

Tr6

A

Lith

stra

tB

arro

wG

roup

Mun

garo

o F

orm

atio

n

North Gorgon-1

Depth(m)

3400

3500

3600

3700

3800

3900

4000

4100

4200

4300

4400

4500

GammaAPI

Pal

ynol

.to

p T

r7Ai

icba

se T

r7A

iiito

p T

r6A

base

Tr6

Ato

p C

arni

an

Lith

stra

tB

arro

wG

roup

Mun

garo

o F

orm

atio

n

North Gorgon-2

Depth(m)

3400

3500

3600

3700

3800

3900

4000

4100

4200

4300

4400

GammaAPI

Pal

ynol

.to

p T

r7Ai

icba

se T

r7A

iiito

p T

r6A

base

Tr6

A

Lith

stra

tB

arro

wG

roup

Mun

garo

o F

orm

atio

n

North Gorgon-4

Depth(m)

3500

3600

3700

3800

3900

4000

4100

GammaAPI

Pal

ynol

.T

r8D

iiiT

r7A

iia

Lith

stra

tB

arro

wG

roup

Mun

garo

o F

orm

atio

n

North Gorgon-3

Depth(m)

3400

3500

3600

3700

3800

3900

4000

4100

4200

4300

GammaAPI

Pal

ynol

.T

r8C

iiiT

r8D

iT

r8D

iii

Lith

stra

tB

arro

wG

roup

Brig

adie

rF

orm

atio

nM

unga

roo

For

mat

ion

Gorgon-1

Depth(m)

3600

3700

3800

3900

4000

4100

4200

4300

4400

GammaAPI

Pal

ynol

.ba

se T

R6A

top

Car

nian

Lith

stra

tB

arro

w G

rou

pM

unga

roo

For

mat

ion

Gorgon-3

Depth(m)

3500

3600

3700

3800

3900

4000

4100

4200

4300

4400

4500

GammaAPI

Pal

ynol

.ba

se T

r6A

top

Car

nian

Lith

stra

tB

arro

wG

roup

Mun

garo

o F

orm

atio

n

Central Gorgon 1

Depth(m)

3600

3700

3800

3900

4000

4100

4200

4300

4400

4500

4600

GammaAPI

Pal

ynol

.ba

se T

r6A

top

Car

nian

Lith

stra

tB

arro

w G

roup

Mun

garo

o F

orm

atio

n

North Gorgon-6

Depth(m)

3500

3600

3700

3800

3900

4000

4100

4200

4300

GammaAPI

Pal

ynol

.ba

se T

r7A

iiito

p T

r6A

base

Tr6

A

Lith

stra

tB

arro

wG

roup

Mun

garo

o F

orm

atio

n

North Gorgon-1

Depth(m)

3400

3500

3600

3700

3800

3900

4000

4100

4200

4300

4400

4500

GammaAPI

Pal

ynol

.to

p T

r7Ai

icba

se T

r7A

iiito

p T

r6A

base

Tr6

Ato

p C

arni

an

Lith

stra

tB

arro

wG

roup

Mun

garo

o F

orm

atio

n

North Gorgon-2

Depth(m)

3400

3500

3600

3700

3800

3900

4000

4100

4200

4300

4400

GammaAPI

Pal

ynol

.to

p T

r7Ai

icba

se T

r7A

iiito

p T

r6A

base

Tr6

A

Lith

stra

tB

arro

wG

roup

Mun

garo

o F

orm

atio

n

North Gorgon-4

Depth(m)

3500

3600

3700

3800

3900

4000

4100

GammaAPI

Pal

ynol

.T

r8D

iiiT

r7A

iia

Lith

stra

tB

arro

wG

roup

Mun

garo

o F

orm

atio

n

North Gorgon-3

Depth(m)

3400

3500

3600

3700

3800

3900

4000

4100

4200

4300

GammaAPI

Pal

ynol

.T

r8C

iiiT

r8D

iT

r8D

iii

Lith

stra

tB

arro

wG

roup

Brig

adie

rF

orm

atio

nM

unga

roo

For

mat

ion

Stratigraphic correlation

3 Time lines7 chemostratigraphic packages

22 geochemical units

Page 7: Application of chemostratigraphy to the Mungaroo Formation, NW Shelf K.T. Ratcliffe and A.M. Wright Chemostrat Inc, Houston, USA P. Montgomery, Chevron

How do we get the data ?

1. Surface contaminationRemoved - washing

2. Cuttings chips selected for analysis - picking

3. Sample powdered -grinding

4. Powder “dissolved” –Li metaborate fusion

5. Concentrations for10 major elements23 trace elements

14 Rare earth elements

All reported in xls format

4. Solution analysed-ICP OES and ICP MS

Client BPProject Haynesville

Well Williams-22-3Date 12/11/2009

# Samples Sample ICP-OES ICP-OES ICP-OES ICP-OES ICP-OES ICP-OES ICP-OES ICP-OES ICP-OES ICP-OESwith data Well Name Depth SiO2 TiO2 Al2O3 Fe2O3 MnO MgO CaO Na2O K2O P2O5 Total

wt% wt% wt% wt% wt% wt% wt% wt% wt% wt% wt%1 Williams-22-3 11541.80 42.68 0.51 11.60 3.02 0.021 1.13 16.29 1.21 2.49 0.467 79.412 Williams-22-3 11543.80 46.74 0.58 13.13 4.04 0.035 2.34 12.22 1.09 2.89 0.202 83.273 Williams-22-3 11545.80 37.78 0.45 10.52 3.62 0.029 1.96 18.40 1.08 2.21 0.356 76.414 Williams-22-3 11547.80 53.89 0.66 15.41 4.00 0.019 1.52 7.13 1.11 3.40 0.098 87.245 Williams-22-3 11549.40 44.71 0.57 13.47 3.77 0.024 1.42 13.81 1.24 2.89 0.407 82.316 Williams-22-3 11551.80 45.05 0.61 14.18 3.95 0.022 1.46 12.70 1.20 3.10 0.229 82.527 Williams-22-3 11553.66 45.23 0.54 13.40 3.73 0.022 1.44 13.41 1.23 2.78 0.267 82.068 Williams-22-3 11555.70 46.41 0.57 14.83 4.01 0.022 1.57 12.27 1.00 3.24 0.542 84.479 Williams-22-3 11557.74 49.23 0.60 16.51 4.71 0.020 1.85 9.01 1.08 3.38 0.281 86.6510 Williams-22-3 11559.84 46.88 0.54 13.69 3.91 0.024 1.52 12.69 1.16 2.93 0.159 83.5011 Williams-22-3 11561.82 46.90 0.52 12.16 4.86 0.048 2.29 12.95 1.24 2.46 0.150 83.5812 Williams-22-3 11563.90 52.01 0.58 13.73 3.96 0.024 1.36 9.70 1.32 2.94 0.241 85.8513 Williams-22-3 11565.58 55.07 0.66 15.87 4.00 0.020 1.40 6.75 1.13 3.55 0.202 88.6514 Williams-22-3 11567.84 53.89 0.63 15.32 3.92 0.019 1.40 7.65 1.10 3.41 0.327 87.6715 Williams-22-3 11569.80 55.22 0.62 14.70 4.49 0.018 1.29 6.27 1.34 3.19 0.267 87.4116 Williams-22-3 11571.76 51.48 0.56 13.54 5.18 0.017 1.18 8.62 1.26 2.95 0.241 85.02

1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 160.00

10.00

20.00

30.00

40.00

50.00

60.00

SiO2 wt%

SiO2 wt%

1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 160.00

2.00

4.00

6.00

8.00

10.00

12.00

14.00

16.00

18.00

20.00

CaO wt%

CaO wt%

Page 8: Application of chemostratigraphy to the Mungaroo Formation, NW Shelf K.T. Ratcliffe and A.M. Wright Chemostrat Inc, Houston, USA P. Montgomery, Chevron

Central Gorgon 1

Depth

3600

3700

3800

3900

4000

4100

4200

4300

4400

4500

4600

Gamma API

clay

pa

ckag

es

Pac

ka

ge

10

Pac

kage

5P

acka

ge 4

Pac

kage

3P

acka

ge 2

Pac

kage

1

Nb/Al2O3MgO/Al2O3

North Gorgon-1

Depth

3400

3500

3600

3700

3800

3900

4000

4100

4200

4300

4400

4500

Gamma API

clay

pa

ckag

es

Pac

ka

ge 1

0P

acka

ge 5

Pac

kage

4P

acka

ge 3

Nb/Al2O3MgO/Al2O3

North Gorgon-2

Depth

3400

3500

3600

3700

3800

3900

4000

4100

4200

4300

4400

Gamma API

clay

pa

ckag

es

Pac

ka

ge

10

Pac

kage

5P

acka

ge 4

Nb/Al2O3MgO/Al2O3

North Gorgon-3

Depth

3400

3500

3600

3700

3800

3900

4000

4100

4200

Gamma API

clay

pa

ckag

es

Pac

ka

ge 1

0P

acka

ge 8

Pac

kage

7P

acka

ge 6

aP

acka

ge 6

Pac

kage

5

Nb/Al2O3MgO/Al2O3

0.5 1.0 1.5 2.00.00

0.03

0.06

0.09

0.12

0.15

0.5 1.0 1.5 2.00.00

0.03

0.06

0.09

0.12

0.15

0.5 1.0 1.5 2.00.00

0.03

0.06

0.09

0.12

0.15

Gorgon-1 Gorgon-3

North Gorgon-3

Barrow Group

Barrow Group

Barrow Group

Mungaroo Fm Mungaroo Fm

Mungaroo Fm

Brigadier Fm

Brigadier Fm

(absent)

Brigadier Fm

(absent)

BarrowGroupBrigadierFormationMungarooFormation

Mg

O/A

l 2O

3

Nb/Al2O

3

Mg

O/A

l 2O

3

Mg

O/A

l 2O

3

Nb/Al2O

3

Nb/Al

Chemically recognising lithostrat units

Gorgon-1

Depth(m)

3600

3700

3800

3900

4000

4100

4200

4300

4400

GammaAPI

Pal

ynol

.ba

se T

R6A

top

Car

nian

Lith

stra

tB

arro

w G

rou

pM

unga

roo

For

mat

ion

Gorgon-3

Depth(m)

3500

3600

3700

3800

3900

4000

4100

4200

4300

4400

4500

GammaAPI

Pal

ynol

.ba

se T

r6A

top

Car

nian

Lith

stra

tB

arro

wG

roup

Mun

garo

o F

orm

atio

n

Central Gorgon 1

Depth(m)

3600

3700

3800

3900

4000

4100

4200

4300

4400

4500

4600

GammaAPI

Pal

ynol

.ba

se T

r6A

top

Car

nian

Lith

stra

tB

arro

w G

roup

Mun

garo

o F

orm

atio

n

North Gorgon-6

Depth(m)

3500

3600

3700

3800

3900

4000

4100

4200

4300

GammaAPI

Pal

ynol

.ba

se T

r7A

iiito

p T

r6A

base

Tr6

A

Lith

stra

tB

arro

wG

roup

Mun

garo

o F

orm

atio

n

North Gorgon-1

Depth(m)

3400

3500

3600

3700

3800

3900

4000

4100

4200

4300

4400

4500

GammaAPI

Pal

ynol

.to

p T

r7Ai

icba

se T

r7A

iiito

p T

r6A

base

Tr6

Ato

p C

arni

an

Lith

stra

tB

arro

wG

roup

Mun

garo

o F

orm

atio

n

North Gorgon-2

Depth(m)

3400

3500

3600

3700

3800

3900

4000

4100

4200

4300

4400

GammaAPI

Pal

ynol

.to

p T

r7Ai

icba

se T

r7A

iiito

p T

r6A

base

Tr6

A

Lith

stra

tB

arro

wG

roup

Mun

garo

o F

orm

atio

n

North Gorgon-4

Depth(m)

3500

3600

3700

3800

3900

4000

4100

GammaAPI

Pal

ynol

.T

r8D

iiiT

r7A

iia

Lith

stra

tB

arro

wG

roup

Mun

garo

o F

orm

atio

n

North Gorgon-3

Depth(m)

3400

3500

3600

3700

3800

3900

4000

4100

4200

4300

GammaAPI

Pal

ynol

.T

r8C

iiiT

r8D

iT

r8D

iii

Lith

stra

tB

arro

wG

roup

Brig

adie

rF

orm

atio

nM

unga

roo

For

mat

ion

Page 9: Application of chemostratigraphy to the Mungaroo Formation, NW Shelf K.T. Ratcliffe and A.M. Wright Chemostrat Inc, Houston, USA P. Montgomery, Chevron

Gorgon-1

Depth(m)

3600

3700

3800

3900

4000

4100

4200

4300

4400

GammaAPI

Pal

ynol

.ba

se T

R6A

top

Car

nian

Lith

stra

tB

arro

w G

rou

pM

unga

roo

For

mat

ion

Gorgon-3

Depth(m)

3500

3600

3700

3800

3900

4000

4100

4200

4300

4400

4500

GammaAPI

Pal

ynol

.ba

se T

r6A

top

Car

nian

Lith

stra

tB

arro

wG

roup

Mun

garo

o F

orm

atio

n

Central Gorgon 1

Depth(m)

3600

3700

3800

3900

4000

4100

4200

4300

4400

4500

4600

GammaAPI

Pal

ynol

.ba

se T

r6A

top

Car

nian

Lith

stra

tB

arro

w G

roup

Mun

garo

o F

orm

atio

n

North Gorgon-6

Depth(m)

3500

3600

3700

3800

3900

4000

4100

4200

4300

GammaAPI

Pal

ynol

.ba

se T

r7A

iiito

p T

r6A

base

Tr6

A

Lith

stra

tB

arro

wG

roup

Mun

garo

o F

orm

atio

n

North Gorgon-1

Depth(m)

3400

3500

3600

3700

3800

3900

4000

4100

4200

4300

4400

4500

GammaAPI

Pal

ynol

.to

p T

r7Ai

icba

se T

r7A

iiito

p T

r6A

base

Tr6

Ato

p C

arni

an

Lith

stra

tB

arro

wG

roup

Mun

garo

o F

orm

atio

n

North Gorgon-2

Depth(m)

3400

3500

3600

3700

3800

3900

4000

4100

4200

4300

4400

GammaAPI

Pal

ynol

.to

p T

r7Ai

icba

se T

r7A

iiito

p T

r6A

base

Tr6

A

Lith

stra

tB

arro

wG

roup

Mun

garo

o F

orm

atio

n

North Gorgon-4

Depth(m)

3500

3600

3700

3800

3900

4000

4100

GammaAPI

Pal

ynol

.T

r8D

iiiT

r7A

iia

Lith

stra

tB

arro

wG

roup

Mun

garo

o F

orm

atio

n

North Gorgon-3

Depth(m)

3400

3500

3600

3700

3800

3900

4000

4100

4200

4300

GammaAPI

Pal

ynol

.T

r8C

iiiT

r8D

iT

r8D

iii

Lith

stra

tB

arro

wG

roup

Brig

adie

rF

orm

atio

nM

unga

roo

For

mat

ion

First order chemostratigraphic divisions

Page 10: Application of chemostratigraphy to the Mungaroo Formation, NW Shelf K.T. Ratcliffe and A.M. Wright Chemostrat Inc, Houston, USA P. Montgomery, Chevron

Gorgon-3

Depth

3500

3600

3700

3800

3900

4000

4100

4200

4300

4400

4500

Gamma API

cla

yp

acka

ges

Pac

kage

10P

acka

ge4

Pac

kage

3P

acka

ge2

Pac

kage

1

Tim

elin

e

T1

GA_RB0.12 0.21-

AL_BASES5 0.9-

North Gorgon-6

Depth

3500

3600

3700

3800

3900

4000

4100

4200

4300

Gamma API

cla

yp

acka

ges

Pa

ck

ag

e

10

Pac

kage

5P

acka

ge4

Pac

kage

3

Tim

elin

e

T2

T1

GA_RB0.12 0.21-

AL_BASES5 0.9-

North Gorgon-1

Depth

3400

3500

3600

3700

3800

3900

4000

4100

4200

4300

4400

4500

Gamma API

cla

yp

acka

ges

Pa

ck

ag

e10

Pac

kage

5P

acka

ge4

Pac

kage

3

Tim

elin

e

T2

T1

GA_RB0.12 0.21-

AL_BASES5 0.9-

North Gorgon-2

Depth

3400

3500

3600

3700

3800

3900

4000

4100

4200

4300

4400

Gamma API

cla

yp

acka

ges

Pa

ck

ag

e

10

Pac

kage

5P

acka

ge4

Tim

elin

e

T2

GA_RB0.12 0.21-

AL_BASES5 0.9-

North Gorgon-3

Depth

3400

3500

3600

3700

3800

3900

4000

4100

4200

4300

Gamma API

cla

yp

acka

ges

Pac

kage

10P

acka

ge8

Pac

kage

7P

acka

ge6a

Pac

kage

6P

acka

ge5

Tim

elin

e

T3

GA_RB0.12 0.2-

AL_BASES5 0.9-

Ga/Rb increases through time

Al2O3/bases (CaO+MgO+K2O+Na2O) increases through time

Notable steps that define the solid lines

SO WHAT ????

First order chemostratigraphic divisions

Page 11: Application of chemostratigraphy to the Mungaroo Formation, NW Shelf K.T. Ratcliffe and A.M. Wright Chemostrat Inc, Houston, USA P. Montgomery, Chevron

Ga/Rb = kaolinite / illite in claystones – intensely weathered claystones tend to be more kaolinitic

Al/bases = CIA (chemical index of alteration) which is a proxy for the degree of weathering

Gorgon-3

Depth

3500

3600

3700

3800

3900

4000

4100

4200

4300

4400

4500

Gamma API

cla

yp

acka

ges

Pac

kage

10P

acka

ge4

Pac

kage

3P

acka

ge2

Pac

kage

1

Tim

elin

e

T1

GA_RB0.12 0.21-

AL_BASES5 0.9-

North Gorgon-6

Depth

3500

3600

3700

3800

3900

4000

4100

4200

4300

Gamma API

cla

yp

acka

ges

Pa

ck

ag

e

10

Pac

kage

5P

acka

ge4

Pac

kage

3

Tim

elin

e

T2

T1

GA_RB0.12 0.21-

AL_BASES5 0.9-

North Gorgon-1

Depth

3400

3500

3600

3700

3800

3900

4000

4100

4200

4300

4400

4500

Gamma API

cla

yp

acka

ges

Pa

ck

ag

e10

Pac

kage

5P

acka

ge4

Pac

kage

3

Tim

elin

e

T2

T1

GA_RB0.12 0.21-

AL_BASES5 0.9-

North Gorgon-2

Depth

3400

3500

3600

3700

3800

3900

4000

4100

4200

4300

4400

Gamma API

cla

yp

acka

ges

Pa

ck

ag

e

10

Pac

kage

5P

acka

ge4

Tim

elin

e

T2

GA_RB0.12 0.21-

AL_BASES5 0.9-

North Gorgon-3

Depth

3400

3500

3600

3700

3800

3900

4000

4100

4200

4300

Gamma API

cla

yp

acka

ges

Pac

kage

10P

acka

ge8

Pac

kage

7P

acka

ge6a

Pac

kage

6P

acka

ge5

Tim

elin

e

T3

GA_RB0.12 0.2-

AL_BASES5 0.9-

Therefore blue = less intense weathering, red = more intense hydrolytic weathering

First order chemostratigraphic divisions

Page 12: Application of chemostratigraphy to the Mungaroo Formation, NW Shelf K.T. Ratcliffe and A.M. Wright Chemostrat Inc, Houston, USA P. Montgomery, Chevron

Chemostratigraphic packages

Gorgon-1

Depth(m)

3600

3700

3800

3900

4000

4100

4200

4300

4400

GammaAPI

Pal

ynol

.ba

se T

R6A

top

Car

nian

Lith

stra

tB

arro

w G

rou

pM

unga

roo

For

mat

ion

Gorgon-3

Depth(m)

3500

3600

3700

3800

3900

4000

4100

4200

4300

4400

4500

GammaAPI

Pal

ynol

.ba

se T

r6A

top

Car

nian

Lith

stra

tB

arro

wG

roup

Mun

garo

o F

orm

atio

n

Central Gorgon 1

Depth(m)

3600

3700

3800

3900

4000

4100

4200

4300

4400

4500

4600

GammaAPI

Pal

ynol

.ba

se T

r6A

top

Car

nian

Lith

stra

tB

arro

w G

roup

Mun

garo

o F

orm

atio

n

North Gorgon-6

Depth(m)

3500

3600

3700

3800

3900

4000

4100

4200

4300

GammaAPI

Pal

ynol

.ba

se T

r7A

iiito

p T

r6A

base

Tr6

A

Lith

stra

tB

arro

wG

roup

Mun

garo

o F

orm

atio

n

North Gorgon-1

Depth(m)

3400

3500

3600

3700

3800

3900

4000

4100

4200

4300

4400

4500

GammaAPI

Pal

ynol

.to

p T

r7Ai

icba

se T

r7A

iiito

p T

r6A

base

Tr6

Ato

p C

arni

an

Lith

stra

tB

arro

wG

roup

Mun

garo

o F

orm

atio

n

North Gorgon-2

Depth(m)

3400

3500

3600

3700

3800

3900

4000

4100

4200

4300

4400

GammaAPI

Pal

ynol

.to

p T

r7Ai

icba

se T

r7A

iiito

p T

r6A

base

Tr6

A

Lith

stra

tB

arro

wG

roup

Mun

garo

o F

orm

atio

n

North Gorgon-4

Depth(m)

3500

3600

3700

3800

3900

4000

4100

GammaAPI

Pal

ynol

.T

r8D

iiiT

r7A

iia

Lith

stra

tB

arro

wG

roup

Mun

garo

o F

orm

atio

n

North Gorgon-3

Depth(m)

3400

3500

3600

3700

3800

3900

4000

4100

4200

4300

GammaAPI

Pal

ynol

.T

r8C

iiiT

r8D

iT

r8D

iii

Lith

stra

tB

arro

wG

roup

Brig

adie

rF

orm

atio

nM

unga

roo

For

mat

ion

Page 13: Application of chemostratigraphy to the Mungaroo Formation, NW Shelf K.T. Ratcliffe and A.M. Wright Chemostrat Inc, Houston, USA P. Montgomery, Chevron

Packa

ge 2

Package 1

Central Gorgon 1

Depth

3600

3700

3800

3900

4000

4100

4200

4300

4400

4500

4600

Gamma API

clay

pac

kage

sP

ac

ka

ge

10

Pac

kage

5P

acka

ge 4

Pac

kage

3P

acka

ge 2

Pac

kage

1

Nb/Al2O3 Cr/Na2O Na2O/Al2O3MgO/Al2O3

North Gorgon-1

Depth

3400

3500

3600

3700

3800

3900

4000

4100

4200

4300

4400

4500

Gamma API

clay

pac

kage

sP

ac

ka

ge

10

Pac

kage

5P

acka

ge 4

Pac

kage

3

Nb/Al2O3 Cr/Na2O Na2O/Al2O3MgO/Al2O3

North Gorgon-2

Depth

3400

3500

3600

3700

3800

3900

4000

4100

4200

4300

4400

Gamma API

clay

pac

kage

sP

ac

ka

ge

10

Pac

kage

5P

acka

ge 4

Nb/Al2O3 Cr/Na2O Na2O/Al2O3MgO/Al2O3

North Gorgon-3

Depth

3400

3500

3600

3700

3800

3900

4000

4100

4200

Gamma API

clay

pac

kage

sP

ac

ka

ge

10

Pac

kage

8P

acka

ge 7

Pac

kage

6a

Pac

kage

6P

acka

ge 5

Nb/Al2O3 Cr/Na2O Na2O/Al2O3MgO/Al2O3

Packages defined using variations in Nb, Cr and Na

SO WHAT ????

Chemostratigraphic packages

Page 14: Application of chemostratigraphy to the Mungaroo Formation, NW Shelf K.T. Ratcliffe and A.M. Wright Chemostrat Inc, Houston, USA P. Montgomery, Chevron

-0.3

-0.2

-0.1

0

0.1

0.2

0.3

0.4

-0.2 -0.1 0 0.1 0.2

Al

Si

Ti

FeMn

Mg

Ca

NaK

P

Ba

Be

Cr

Ni

Sc

Sr

Zn

Zr

V

Co

CuGa

Rb

Y

Nb

Mo

Sn

Cs

HfTa Th

U

LREEs

MREEs

HREEs

EV1

EV

2

Group 1. Quartz

Group 2. ClayMinerals

Group 3. HeavyMinerals

Illite

Kaolinite

Non Zircon

Zircon

Group 4. Siderite

Group 5. PlagioclaseFeldspar

Chemostratigraphic packages

Page 15: Application of chemostratigraphy to the Mungaroo Formation, NW Shelf K.T. Ratcliffe and A.M. Wright Chemostrat Inc, Houston, USA P. Montgomery, Chevron

Gorgon-1

Depth(m)

3600

3700

3800

3900

4000

4100

4200

4300

4400

GammaAPI

Pal

ynol

.ba

se T

R6A

top

Car

nian

Lith

stra

tB

arro

w G

rou

pM

unga

roo

For

mat

ion

Gorgon-3

Depth(m)

3500

3600

3700

3800

3900

4000

4100

4200

4300

4400

4500

GammaAPI

Pal

ynol

.ba

se T

r6A

top

Car

nian

Lith

stra

tB

arro

wG

roup

Mun

garo

o F

orm

atio

n

Central Gorgon 1

Depth(m)

3600

3700

3800

3900

4000

4100

4200

4300

4400

4500

4600

GammaAPI

Pal

ynol

.ba

se T

r6A

top

Car

nian

Lith

stra

tB

arro

w G

roup

Mun

garo

o F

orm

atio

n

North Gorgon-6

Depth(m)

3500

3600

3700

3800

3900

4000

4100

4200

4300

GammaAPI

Pal

ynol

.ba

se T

r7A

iiito

p T

r6A

base

Tr6

A

Lith

stra

tB

arro

wG

roup

Mun

garo

o F

orm

atio

n

North Gorgon-1

Depth(m)

3400

3500

3600

3700

3800

3900

4000

4100

4200

4300

4400

4500

GammaAPI

Pal

ynol

.to

p T

r7Ai

icba

se T

r7A

iiito

p T

r6A

base

Tr6

Ato

p C

arni

an

Lith

stra

tB

arro

wG

roup

Mun

garo

o F

orm

atio

n

North Gorgon-2

Depth(m)

3400

3500

3600

3700

3800

3900

4000

4100

4200

4300

4400

GammaAPI

Pal

ynol

.to

p T

r7Ai

icba

se T

r7A

iiito

p T

r6A

base

Tr6

A

Lith

stra

tB

arro

wG

roup

Mun

garo

o F

orm

atio

n

North Gorgon-4

Depth(m)

3500

3600

3700

3800

3900

4000

4100

GammaAPI

Pal

ynol

.T

r8D

iiiT

r7A

iia

Lith

stra

tB

arro

wG

roup

Mun

garo

o F

orm

atio

n

North Gorgon-3

Depth(m)

3400

3500

3600

3700

3800

3900

4000

4100

4200

4300

GammaAPI

Pal

ynol

.T

r8C

iiiT

r8D

iT

r8D

iii

Lith

stra

tB

arro

wG

roup

Brig

adie

rF

orm

atio

nM

unga

roo

For

mat

ionCentral Gorgon 1

Depth

3600

3700

3800

3900

4000

4100

4200

4300

4400

4500

4600

Gamma API

clay

pack

ages

Pa

cka

ge

10

Pac

kage

5P

acka

ge4

Pac

kage

3P

acka

ge2

Pac

kage

1

Nb/Al2O3 Cr/Na2O Na2O/Al2O3Ga/Rb

Al2O3/bases

North Gorgon-1

Depth

3400

3500

3600

3700

3800

3900

4000

4100

4200

4300

4400

4500

Gamma API

clay

pack

ages

Pa

ck

ag

e10

Pac

kage

5P

acka

ge4

Pac

kage

3

Nb/Al2O3 Cr/Na2O Na2O/Al2O3Ga/Rb

Al2O3/bases

North Gorgon-2

Depth

3400

3500

3600

3700

3800

3900

4000

4100

4200

4300

4400

Gamma API

clay

pack

ages

Pa

ck

ag

e1

0P

acka

ge5

Pac

kage

4

Nb/Al2O3 Cr/Na2O Na2O/Al2O3Ga/Rb

Al2O3/bases

North Gorgon-3

Depth

3400

3500

3600

3700

3800

3900

4000

4100

4200

Gamma API

clay

pack

ages

Pa

ck

ag

e10

Pac

kage

8P

acka

ge7

Pac

kage

6aP

acka

ge6

Pac

kage

5

Nb/Al2O3 Cr/Na2O Na2O/Al2O3Ga/Rb

Al2O3/bases

Ga/Rb : Al/bases – change in paleoclimate through time

Na/Al, Cr/Na and Nb/Al in provenance through time

Chemostratigraphic packages

Page 16: Application of chemostratigraphy to the Mungaroo Formation, NW Shelf K.T. Ratcliffe and A.M. Wright Chemostrat Inc, Houston, USA P. Montgomery, Chevron

Central Gorgon 1

Depth

3600

3700

3800

3900

4000

4100

4200

4300

4400

4500

4600

Gamma API

clay

packa

ges

Pac

ka

ge

10

Pac

kage

5P

acka

ge4

Pac

kage

3P

acka

ge2

Pac

kage

1

Na/Al2O3K2O/Al2O3

Rb/CsGa/Rb

Al2O3/bases

North Gorgon-1

Depth

3400

3500

3600

3700

3800

3900

4000

4100

4200

4300

4400

4500

Gamma API

clay

packa

ges

Pac

ka

ge

10P

acka

ge5

Pac

kage

4P

acka

ge3

Na/Al2O3K2O/Al2O3

Rb/CsGa/Rb

Al2O3/bases

North Gorgon-2

Depth

3400

3500

3600

3700

3800

3900

4000

4100

4200

4300

4400

Gamma API

clay

packa

ges

Pac

ka

ge

10

Pac

kage

5P

acka

ge4

Na/Al2O3K2O/Al2O3

Rb/CsGa/Rb

Al2O3/bases

North Gorgon-3

Depth

3400

3500

3600

3700

3800

3900

4000

4100

4200

Gamma API

clay

packa

ges

Pac

ka

ge

10P

acka

ge8

Pac

kage

7P

acka

ge6a

Pac

kage

6P

acka

ge5

Na/Al2O3K2O/Al2O3

Rb/CsGa/Rb

Al2O3/bases

Sandstone data

Page 17: Application of chemostratigraphy to the Mungaroo Formation, NW Shelf K.T. Ratcliffe and A.M. Wright Chemostrat Inc, Houston, USA P. Montgomery, Chevron

Gorgon-1

Depth(m)

3600

3700

3800

3900

4000

4100

4200

4300

4400

GammaAPI

Pal

ynol

.ba

se T

R6A

top

Car

nian

Lith

stra

tB

arro

w G

rou

pM

unga

roo

For

mat

ion

Gorgon-3

Depth(m)

3500

3600

3700

3800

3900

4000

4100

4200

4300

4400

4500

GammaAPI

Pal

ynol

.ba

se T

r6A

top

Car

nian

Lith

stra

tB

arro

wG

roup

Mun

garo

o F

orm

atio

n

Central Gorgon 1

Depth(m)

3600

3700

3800

3900

4000

4100

4200

4300

4400

4500

4600

GammaAPI

Pal

ynol

.ba

se T

r6A

top

Car

nian

Lith

stra

tB

arro

w G

roup

Mun

garo

o F

orm

atio

n

North Gorgon-6

Depth(m)

3500

3600

3700

3800

3900

4000

4100

4200

4300

GammaAPI

Pal

ynol

.ba

se T

r7A

iiito

p T

r6A

base

Tr6

A

Lith

stra

tB

arro

wG

roup

Mun

garo

o F

orm

atio

n

North Gorgon-1

Depth(m)

3400

3500

3600

3700

3800

3900

4000

4100

4200

4300

4400

4500

GammaAPI

Pal

ynol

.to

p T

r7Ai

icba

se T

r7A

iiito

p T

r6A

base

Tr6

Ato

p C

arni

an

Lith

stra

tB

arro

wG

roup

Mun

garo

o F

orm

atio

n

North Gorgon-2

Depth(m)

3400

3500

3600

3700

3800

3900

4000

4100

4200

4300

4400

GammaAPI

Pal

ynol

.to

p T

r7Ai

icba

se T

r7A

iiito

p T

r6A

base

Tr6

A

Lith

stra

tB

arro

wG

roup

Mun

garo

o F

orm

atio

n

North Gorgon-4

Depth(m)

3500

3600

3700

3800

3900

4000

4100

GammaAPI

Pal

ynol

.T

r8D

iiiT

r7A

iia

Lith

stra

tB

arro

wG

roup

Mun

garo

o F

orm

atio

n

North Gorgon-3

Depth(m)

3400

3500

3600

3700

3800

3900

4000

4100

4200

4300

GammaAPI

Pal

ynol

.T

r8C

iiiT

r8D

iT

r8D

iii

Lith

stra

tB

arro

wG

roup

Brig

adie

rF

orm

atio

nM

unga

roo

For

mat

ion

Sandstone correlation

Page 18: Application of chemostratigraphy to the Mungaroo Formation, NW Shelf K.T. Ratcliffe and A.M. Wright Chemostrat Inc, Houston, USA P. Montgomery, Chevron

Gorgon-1

Depth

3800

3900

4000

4100

4200

4300

4400

Gamma API

clay

pack

ages

Pac

kage

4P

acka

ge3

Pac

kage

2P

acka

ge1

san

du

nits

S a n d 4 e

S a n d 4 b

Sand3a

San

d2

Lith

stra

t

Top z 20

S Sand

Top z 10

T Sand

Tsu

rfa

ce

T1

Gorgon-3

Depth

3900

4000

4100

4200

4300

4400

4500

Gamma API

clay

pack

ages

Pac

kage

4P

acka

ge3

Pac

kage

2P

acka

ge1

san

du

nits

Sand3a

San

d2

San

d1

Lith

stra

t

Top z 20

S Sand

Top z 10

T Sand

Tsu

rfa

ce

T1

Central Gorgon 1

Depth

4100

4200

4300

4400

4500

4600

Gamma API

clay

pack

ages

Pac

kage

4P

acka

ge3

Pac

kage

2P

acka

ge1

san

du

nits

S a n d 4 b

S a n d 4 a

Sand3a

San

d2

Lith

stra

t

Top z 20

S Sand

Top z 10

T Sand

Tsu

rfa

ce

T1

North Gorgon-6

Depth

4000

4100

4200

4300

Gamma API

clay

pack

ages

Pac

kage

4P

acka

ge3

san

du

nits

Sand4b

Sand4a

San

d3a

ii

Sand3a

Lith

stra

t

Top z 20

S Sand

Top z 10

T Sand

Tsu

rfa

ce

T1

North Gorgon-1

Depth

4100

4200

4300

4400

Gamma API

clay

pack

ages

Pac

kage

4P

acka

ge3

san

du

nits

Sand4b

Sand4a

Sand3aii

San

d3a

iS

and

3a

Lith

stra

t

Top z 20

Q sand

R sand

S Sand

Top z 10

T Sand

Tsu

rfa

ce

T1

T1Marker

Topzone 20

Top T sand

Top Q sand

Gorgon-1

Depth

3800

3900

4000

4100

4200

4300

4400

Gamma API

clay

pack

ages

Pac

kage

4P

acka

ge3

Pac

kage

2P

acka

ge1

san

du

nits

S a n d 4 e

S a n d 4 b

Sand3a

San

d2

Lith

stra

t

Top z 20

S Sand

Top z 10

T Sand

Tsu

rfa

ce

T1

Gorgon-3

Depth

3900

4000

4100

4200

4300

4400

4500

Gamma API

clay

pack

ages

Pac

kage

4P

acka

ge3

Pac

kage

2P

acka

ge1

san

du

nits

Sand3a

San

d2

San

d1

Lith

stra

t

Top z 20

S Sand

Top z 10

T Sand

Tsu

rfa

ce

T1

Central Gorgon 1

Depth

4100

4200

4300

4400

4500

4600

Gamma API

clay

pack

ages

Pac

kage

4P

acka

ge3

Pac

kage

2P

acka

ge1

san

du

nits

S a n d 4 b

S a n d 4 a

Sand3a

San

d2

Lith

stra

t

Top z 20

S Sand

Top z 10

T Sand

Tsu

rfa

ce

T1

North Gorgon-6

Depth

4000

4100

4200

4300

Gamma API

clay

pack

ages

Pac

kage

4P

acka

ge3

san

du

nits

Sand4b

Sand4a

San

d3a

ii

Sand3a

Lith

stra

t

Top z 20

S Sand

Top z 10

T Sand

Tsu

rfa

ce

T1

North Gorgon-1

Depth

4100

4200

4300

4400

Gamma API

clay

pack

ages

Pac

kage

4P

acka

ge3

san

du

nits

Sand4b

Sand4a

Sand3aii

San

d3a

iS

and

3a

Lith

stra

t

Top z 20

Q sand

R sand

S Sand

Top z 10

T Sand

Tsu

rfa

ce

T1

T1Marker

Topzone 20

Top T sand

Top Q sand

Page 19: Application of chemostratigraphy to the Mungaroo Formation, NW Shelf K.T. Ratcliffe and A.M. Wright Chemostrat Inc, Houston, USA P. Montgomery, Chevron

Each lithostratigraphic unit has a unique geochemical signature The Mungaroo Formation contains three chemostratigraphic surfaces that approximate to chronostratigraphic markers Seven chemostratigraphic packages and 22 units are identified and correlated in the Mungaroo Formation The paleoclimate during deposition of the Mungaroo Formation was becoming increasingly wet, resulting in more intense hydrolytic weathering and increased abundance of kaolinite in the claystone lithologies The older parts of the Mungaroo Formation contain common plagioclase feldspar, implying an intermediate igneous provenance. The intermediate provenance was replaced through time with greater influence of a mafic igneous provenance The Brigadier Formation contains an unknown Nb-rich heavy mineral species, implying that the provenance of this formation is different to that of the Mungaroo Formation

In places, the chemostratigraphic sand unit correlation deviates from the lithostratigraphic sand correlation to an extent that may impact upon gas production. The variation between litho- and chemostratigraphic correlation are potentially vitally important for building reservoir models in the Mungaroo Formation of the Gorgon Field.

Page 20: Application of chemostratigraphy to the Mungaroo Formation, NW Shelf K.T. Ratcliffe and A.M. Wright Chemostrat Inc, Houston, USA P. Montgomery, Chevron

ACKNOWLEDGEMENTS Chemostrat would like to thank David Wray and Lorna Dyer of Greenwich University for carrying out

the ICP OES MS analyses and Bill Ellington of Ellington and Associates for carrying out the XRD analyses. We are also grateful to Chemostrat and Chevron Australia for allowing us time and resources

to prepare this manuscript. The authors are grateful to Eric Tenthorey, Andrew Jones and Ben Van Aarssen who reviewed the original manuscript and whose comments were invaluable to the final

document. The authors would like to thank the Gorgon Joint Venture partners, Mobil Australia Resources and Shell Development (Australia) for allowing permission for this paper to be published.