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Seismic quality in the Tuzgolu Basin is very poor for accurate interpretation of the subsurface.
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Residual gravity interpretation gives an understanding of the subsurface anomaly.
The structural interpretation depicts the subsurface reservoir as a fault-assisted closure within the deep water turbiditic environment.
The results obtained from this study may help the interpretation of subsurface data in those geological contexts in which the interplay of gravitational and tectonic processes is responsible for deformation.
A deep well may confirm the interpretation and provide the geothermal gradient of the subsurface process condition.
In contrast, the cryostratigraphic interpretation generally offered more nuanced analysis of the subsurface, but was limited in its ability to detect unconformities and the depth of drilling.
This model can fully represent the previous geological interpretations, comprehensively show the realistic conditions of the subsurface reservoir and greatly reduce the uncertainty of the model.
Meanwhile, visually disabled petroleum engineers may use the aural interpretation of subsurface data.
A comprehensive seismic interpretation integrating all the subsurface information has not yet been executed on the tectonic depression.
These data allowed the elaboration of topographic subsurface and isopach maps, and enabled an interpretation of the accumulation history of the aeolian system since about 2200 BC.
Integrated interpretation of all relevant subsurface information in a sequence stratigraphic approach has become a critical requirement for new discoveries.
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