Carnain Attributes Plugin is the first Ocean Plug-in to use Unsupervised AI Methods for seismic interpretation.

Dip Estimation

In seismic exploration, a Dip estimate refers to the measurement or estimation of the dip angle of subsurface geological features, such as rock layers or fault lines, based on seismic data.The dip angle represents the inclination or slope of these features relative to the horizontal plane. Dip estimates are crucial in seismic interpretation for several reasons: Structural Analysis, Fault Detection and Mapping, Stratigraphic Interpretation, Reservoir Characterization, Geological Modeling, Seismic Data Processing, and Risk Assessment.

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Fluvial system and Facies Identification

In geology, facies refers to the distinct characteristics of a rock unit, including its lithology, sedimentary structures, and fossil content.Facies can vary horizontally and vertically within a geological formation, reflecting changes in environmental conditions during deposition.Seismic facies analysis involves the interpretation of seismic data to identify and characterize different facies or rock types.This analysis helps geoscientists understand the geological history of an area, map different depositional environments, and infer the potential presence of hydrocarbons.

Fluvial refers to processes, landforms, or deposits associated with rivers and streams.Fluvial environments are characterized by the transportation and deposition of sediments by flowing water. When seismic data reveals characteristics associated with fluvial environments, geoscientists can infer the presence of river channels, floodplains, and other features related to the action of rivers.Identification of fluvial deposits is important in understanding the sedimentary history of an area and can be significant for hydrocarbon exploration, as fluvial environments are often associated with reservoir formations.

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Attributes Standalone

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Fluvial system and Facies Identification

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Fault Segmentation

Identifying faults in seismic data is crucial for several reasons in geological and geophysical studies. Faults can act as both barriers and conduits for fluid flow within subsurface reservoirs.Identifying faults helps in understanding how fluids, such as oil and gas, migrate and accumulate within reservoirs.

By identifying faults, geologists can reconstruct the tectonic history of an area, including past deformation events and the kinematics of fault movements. They can better identify seismic hazzards, Reservoir compartmentalization and hydrocarbon traps.

Salt Deliniation

Salt bodies often exhibit complex structural geometries, including diapiric, salt wall, and salt dome structures.These structures can influence the deformation of surrounding sedimentary rocks and create structural traps for hydrocarbons.Detecting and characterizing salt bodies in seismic data aids in structural interpretation, allowing geoscientists to map out fault systems, folds, and other structural features associated with salt tectonics. Salt deposits can host hydrocarbon reservoirs themselves or serve as structural traps for hydrocarbons in adjacent sedimentary rocks.

Detecting salts in seismic data is essential for understanding subsurface geology,evaluating hydrocarbon exploration prospects, and mitigating seismic imaging challenges associated with salt tectonics.Salt bodies play significant roles in trapping hydrocarbons, shaping structural geology, and influencing sedimentary basin evolution, making their identification and characterization critical for various applications in the oil and gas industry and geological research.