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Paleogeography
& Palaeoenvironment
GeoArctic’s proprietary plate tectonic modeling
tools allow all available regional geological and geophysical
data to be used to build a detailed structural and palaeogeographic
history of a plate margin. We create Beta factor maps
for both divergent and convergent plate margins for
major sequence time-slices and use these maps as input
to restore the basin geometry and geophysical, structural
and palaeogeographic data to the time of deposition.
The restored data are then rotated around the Euler
pole for the plate margin to their original geographic
location for any period in the geological past, with
the common problems of overlap and under-fit now removed.
The ability to model deformable plates provides us with
information on the structural development of a basin,
the depositional setting and provenance of reservoir
rocks, source rock distribution, basin connectivity,
palaeo-climate and ocean currents.
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References
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Ady,
B & Whittaker R.C. 2008:
Development of a Global Plate Tectonic Reconstruction
Application for ArcGIS. Abstract ESRI User Conference,
Calgary.
Stemmerik, L., Hamman,
N.E. & Whittaker, R.C. 2005: Structural
and geological development of the North-East
Greenland Shelf. Petroleum Geology: North-West
Europe and Global Perspectives – Proceedings
of the 6th Petroleum Geology Conference.
Barnwell, A., Whittaker,
R. C. et al. 2004: A
New Palinspastic Plate Reconstruction of the
Southern North Atlantic, with Implications for
the Formation and Development of Basins on the
Grand Banks of Newfoundland. Abstract CSPG Convention,
Calgary.
Whittaker, R. C. Karpuz.
R., Wheeler. W, & Ady, B. 2000:
4D
regional tectonic modeling [of the North Atlantic]:
plate reconstructions using a geographic information
system. Abstract PETEX Convention, London.
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| Copyright © GeoArctic Ltd. - Geoscience Consulting and
Services
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The deformable plate model provides valuable
information on:
Reservoir and source rocks:
• Geometry of the receiving basin
• Sediment transport system
• Sediment provenance area
Structural development and thermal maturity:
• Rate of extension / tectonic subsidence
• Volcanism (mantle plume & magmatic underplating)
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