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Regional geological GIS and detailed license studies

Iraq Regional Geological ArcView GIS

NPA are continuing their seamless digital geo-referenced ArcView geological database of the Middle East into Iraq. The database contains the following thematic layers:

  • High resolution Landsat ETM satellite imagery.
  • Co-registered detailed Structural and Stratigraphic interpretations.
  • Spatial Earthquake Fault Plane Solution data.
  • Digital Elevation Data.
  • Cross-sections detailing the structural style of the main basins.
  • ASTER generated 3D views of the Kirkuk Embayment.

The image extract (right) from the north-western margin of the Lurestan fold-belt shows the Landsat ETM data overlain by the co-registered detailed Structural and Stratigraphic interpretations. All of the project is provided in ArcView in virtually any projection to enable integration with the clients data-set. The data-set extends into Iran and covers the entire external zones of the Zagros Mountains. It can be purchased completely or as bespoke extractions.

Structural modelling of the the Euphrates-Anah graben

The Euphrates-Anah Graben

The Euphrates and Anah graben systems occur between two stable Palaeozoic blocks - the Rutbha and Khlessia highs. The intervening mobile zones are topographic lows which have undergone Jurassic extension, mid Cretaceous transtension, Neogene inversion and the formation of flower structures. Its stratigraphic section is similar to the proven SE Syria fields. Many of the fields present in SE Syria have a surface representation that is clearly evident across the border in Iraq, also there are several zones of fault intersections that show excellent follow-up potential.

Careful analysis of the satellite imagery indicated that the topographic nature of the area is related directly to the underlying geology; this is an area that is sparsely mapped and in which the structural configuration is only poorly understood.

Integration of geophysical data and structural models help to better define the basin architecture and enable the prediction of structural trends and areas of possible structural closure such as roll-over anticlines, transpressional flower structures.

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