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Dr Kate Robertson [email protected] Senior Geophysicist Lithospheric Architecture Geological Survey of South Australia Department of the Premier and Cabinet, South Australia Geometry and origin of the Curnamona Conductivity Anomaly from AusLAMP magnetotelluric data Presentation for UNCOVER, Curnamona 26 July 2017

Geometry and origin of the Curnamona Conductivity …minerals.statedevelopment.sa.gov.au/__data/assets/pdf... ·  · 2017-07-31Geometry and origin of the Curnamona Conductivity Anomaly

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Confidentiality-I#-A#

Dr Kate Robertson

[email protected]

Senior Geophysicist – Lithospheric Architecture

Geological Survey of South Australia

Department of the Premier and Cabinet, South Australia

Geometry and origin of the Curnamona

Conductivity Anomaly from AusLAMP

magnetotelluric data

Presentation for UNCOVER, Curnamona 26 July 2017

Confidentiality-I#-A# Presentation for UNCOVER, Curnamona 26 July 2017

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• In SA as a collaborative

project between GSSA,

GA and UoA

• Victoria complete

• Tasmania complete

• SA almost complete

• NSW underway

In SA funding from GSSA,

NCRIS/ANSIR, GA

Presentation for UNCOVER, Curnamona 26 July 2017

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• 73 sites

• Average spacing around 55 km

• NeoProterozoic Ikara-Flinders Ranges

• Paleo-Mesoproterozoic Curnamona Province

• Intraplate deformation

• High heat flow and elevated seismicity

SURVEY AREA

Presentation for UNCOVER, Curnamona 26 July 2017

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MAGNETOTELLURICS (MT)

• Passive electromagnetic method

• Measurement of naturally

occurring magnetic and electric

fields at the earths surface

• We use long period MT here

(deep sounding)

• Obtain information on the

electrical resistivity structure of

the subsurface (down to 100’s of

km’s)

Fluxgate Magnetometer

(Hx, Hy, Hz)

Presentation for UNCOVER, Curnamona 26 July 2017

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PHASE TENSOR ELLIPSESInterpreting ellipses:

Colour

Red: increasing conductivity with depth

Blue: decreasing conductivity with depth

Shape

Circle= 1D resistivity, ellipse = 2- or 3D resistivity structure

Orientation

Orientation along direction of preferred current flow

Crust Upper mantleLower

lithosphere

Presentation for UNCOVER, Curnamona 26 July 2017

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Yellow circles- locations of diamondiferous

kimberlites

Black dots- earthquakes

Blue triangles- MT site locations

Black lines- tectonic zone boundaries

Blue regions are resistive, red are conductive

• No obvious correlations of earthquakes with

conductors

• Conductive sediments at 1 km of Murray and

Cooper Basins

• Conductive anomalies apparent at 10 km

and greater.

3D INVERSION RESULTS

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CURNAMONA EAST-WEST 03GA-CU1

0

0.5

3

1

1.5

2

2.5

Yarramba

Warrakimbo

Lo

g r

esis

tivity (

oh

m.m

)

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08GA-C1 DEEP

REFLECTION

SEISMIC

SURVEY

NORTHSOUTH

0

0.5

3

1

1.5

2

2.5

YarrambaWarrakimbo??

Log r

esis

tivity (

ohm

.m)

Presentation for UNCOVER, Curnamona 26 July 2017

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CRUSTAL FLUIDS

NORTH SOUTH

o Stable, old region only minor reworking at

edges from Delamerian Orogeny

o Seismic tomography models show cratonic

signatures

o From geochemistry, lithospheric thinning in

Broken Hill Domain resulted in primitive,

depleted melts in partial melt

o Less thinning in Olary Domain, refertilised

from Olarian subduction?

o Saline sediments and fluids/fossil fluids

Presentation for UNCOVER, Curnamona 26 July 2017

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CURNAMONA INFILL TRANSECT

Presentation for UNCOVER, Curnamona 26 July 2017

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ACKNOWLEDGEMENTS

• Field personnel

• Landholders and Traditional Owners for

land access

• Goran Boren for technical assistance

• GSSA for funding

• Geoscience Australia for logistical

assistance

• Gary Egbert, Anna Kelbert and Naser

Meqbel for ModEM, and Naser Meqbel for

3D grid

Presentation for UNCOVER, Curnamona 26 July 2017

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DisclaimerThe information contained in this presentation has been compiled by the Department of State

Development (DSD) and originates from a variety of sources. Although all reasonable care has

been taken in the preparation and compilation of the information, it has been provided in good faith

for general information only and does not purport to be professional advice. No warranty, express

or implied, is given as to the completeness, correctness, accuracy, reliability or currency of the

materials.

DSD and the Crown in the right of the State of South Australia does not accept responsibility for and

will not be held liable to any recipient of the information for any loss or damage however caused

(including negligence) which may be directly or indirectly suffered as a consequence of use of these

materials. DSD reserves the right to update, amend or supplement the information from time to

time at its discretion.

www.minerals.statedevelopment.sa.gov.au

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Contact

www.minerals.statedevelopment.sa.gov.au

Department of State Development - Mineral Resources Division

Geological Survey of South Australia

Dr Kate Robertson: [email protected]

Level 4, 101 Grenfell Street

Adelaide, South Australia 5000

GPO Box 320

Adelaide, South Australia 5001

T: +61 8 8463 3000

E: [email protected]