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Further development of a Precambrian
plate model and its application in
identifying sediment provenance

Bruce Eglington
University of Saskatchewan
Overview
►
►

Data available to aid model development
Current status of model

 Improvements to plate boundary delineation
 Meso- and Neo-Proterozoic and early
Palaeoproterozoic/Neoarchaean
 Better visualising different types of mineralisation
 Demo model

►
►

Definition of Precambrian plates and relevance to
Phanerozoic geology
Additional constraints provided by detrital zircon
provenance assessments
Overview
►
►

Data available to aid model development
Current status of model
 Improvements to plate boundary delineation
 Meso- and Neo-Proterozoic and early
Palaeoproterozoic/Neoarchaean
 Better visualising different types of mineralisation
 Demo model

►
►

Definition of Precambrian plates and relevance to
Phanerozoic geology
Additional constraints provided by detrital zircon
provenance assessments
Geochronology

~ 106,000 records in the DateView geochronology database
Dyke swarms

~ 6,500 records in the StratDB LIP database, many with geospatial
information in ArcMap compilation
Deposits

~ 15,000 deposit/mineralisation records in the StratDB database, most with latitude and
longitude information. ~4,500 have Pb isotope data
Nd

T DM
Overview
►
►

Data available to aid model development
Current status of model

 Improvements to plate boundary delineation
 Meso- and Neo-Proterozoic and early
Palaeoproterozoic/Neoarchaean
 Better visualising different types of mineralisation
 Demo model

►
►

Definition of Precambrian plates and relevance to
Phanerozoic geology
Additional constraints provided by detrital zircon
provenance assessments
Geophysical constraints
U-Pb Formation Ages
Nd TDM
Geographic extent of dated lithostratigraphic units
Interpreted maximum age of blocks
Overview
►
►

Data available to aid model development
Current status of model

 Improvements to plate boundary delineation
 Plate motion constraints
 Meso- and Neo-Proterozoic and early
Palaeoproterozoic/Neoarchaean
 Better visualising different types of mineralisation
 Demo model

►
►

Definition of Precambrian plates and relevance to
Phanerozoic geology
Additional constraints provided by detrital zircon
provenance assessments
Constraints for Palaeogeographic
Reconstructions
►

Palaeomag constraints are primary – modelled using




GPlates
Paleogis plugin for ArcMap
Customised software written by BE
Constraints for Palaeogeographic
Reconstructions
►

Palaeolongitude


Estimated based on the orthoversion concept presented by
Mitchell and Evans (2012)

Most likely
centroid of
supercontinent
Palaeogeographic
Reconstructions
►

Extensive set of plates based on



►

Palaeomag constraints are primary – modelled using




►

Geology
Aeromagnetic and Gravity Anomalies
GPlates
Paleogis plugin for ArcMap
Customised software written by BE

Consider structural vergence directions
Overview
►
►

Data available to aid model development
Current status of model

 Improvements to plate boundary delineation
 Plate motion constraints
 Meso- and Neo-Proterozoic and early
Palaeoproterozoic/Neoarchaean
 Better visualising different types of mineralisation
 Demo model

►
►

Definition of Precambrian plates and relevance to
Phanerozoic geology
Additional constraints provided by detrital zircon
provenance assessments
Available Palaeogeographic Models
►

Phanerozoic




►

►

Paleomap (Chris Scotese)
Earthbyte (GPlates)
Various commercial models

Meso- to Neo-Proterozoic



IGCP 440 (Li et al., 2008)
Various other ‘snap-shots’

Palaeoproterozoic to Archaean

Various, mostly schematic, ‘snapshots’
 Eglington et al. (2013)
 Pisarevsky et al. (2013)
 Pehrsson et al. (2013)


Paleomap

IGCP 440
Some available Palaeogeographic
Reconstructions for Nuna (Columbia)

Rogers and Santosh, 2002

Zhao et al, 2002

Evans and Mitchell, 2011
►

Started with Palaeoproterozoic Nuna

►

Working forward in time through Mesoproterozoic to
Neoproterozoic Rodinia

►

Also extending back towards Neoarchaean
Overview
►
►

Data available to aid model development
Current status of model

 Improvements to plate boundary delineation
 Plate motion constraints
 Meso- and Neo-Proterozoic and early
Palaeoproterozoic/Neoarchaean
 Better visualising different types of mineralisation
 Demo model

►
►

Definition of Precambrian plates and relevance to
Phanerozoic geology
Additional constraints provided by detrital zircon
provenance assessments
Overview
►
►

Data available to aid model development
Current status of model

 Improvements to plate boundary delineation
 Plate motion constraints
 Meso- and Neo-Proterozoic and early
Palaeoproterozoic/Neoarchaean
 Better visualising different types of mineralisation
 Demo model

►
►

Definition of Precambrian plates and relevance to
Phanerozoic geology
Additional constraints provided by detrital zircon
provenance assessments
Overview
►
►

Data available to aid model development
Current status of model

 Improvements to plate boundary delineation
 Plate motion constraints
 Meso- and Neo-Proterozoic and early
Palaeoproterozoic/Neoarchaean
 Better visualising different types of mineralisation
 Demo model

►
►

Definition of Precambrian plates and relevance to
Phanerozoic geology
Additional constraints provided by detrital zircon
provenance assessments
Reconstruction at 1500 Ma
Ages from 1500 – 1580 Ma
W. Africa

N. Australia

Siberia
Amazonia

W. Australia
Gawler

Slave

Baltica
Mawson

W. Gneiss
Complex
Superior

Plutonic / volcanic crystallization
Metamorphic
Cooling

Ni-Cu-PGE

VMS

U
Basement control
of younger
sedimentation

From Paul Ramaekers (2011)
Basement control
of younger
sedimentation

From Paul Ramaekers (2011)
Basement control
of younger
sedimentation

From Paul Ramaekers (2011)
Basement control
of younger
sedimentation

From Tankard et al (2009)
Basement control
of younger
sedimentation

From Tankard et al (2009)
Basement control
of younger
sedimentation

From Tankard et al (2009)
Basement control
of younger
sedimentation

From Tankard et al (2009)
Overview
►
►

Data available to aid model development
Current status of model

 Improvements to plate boundary delineation
 Plate motion constraints
 Meso- and Neo-Proterozoic and early
Palaeoproterozoic/Neoarchaean
 Better visualising different types of mineralisation
 Demo model

►
►

Definition of Precambrian plates and relevance to
Phanerozoic geology
Additional constraints provided by detrital zircon
provenance assessments
Probability
Unit Age (Ma)

Kaapvaal

1200

3600
1200

3800
Grain Age (Ma)
Pilbara
Zimbabwe

Kaapvaal

Neylan Fm

Lower Selika
Formation

1940 Ma
Detrital
provenance

From Tankard et al (2009)
Detrital zircon age spectra for Cape and Karoo sediments
Detrital zircon age spectra for Cape and Karoo sediments
Detrital zircon age spectra for Cape and Karoo sediments
U-Pb Formation Ages
U-Pb Formation Ages
Cape-Karoo potential provenance sources 850 – 960 Ma
Detrital
provenance
Acknowledgements
►
►

IGCP 509 project
University of Saskatchewan and NSERC


►

Geological Survey of Canada


►

The Rothwell Group
Chris Scotese

GPlates software


►

Newmont
Areva
De Beers

Paleogis plugin for ArcMap



►

Ore deposit information (especially via Lesley Chorlton) + various coworkers

Various mining companies for student support and money to purchase
hardware and software




►

Databases housed at U of S

Dietmar Mueller and John Cannon in Sydney, Australia

Various software companies for providing academic versions





Embarcadero
Steema
AtoZed
HK Systems

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