Shelf Edge Trajectory Angle Calculator

Shelf-edge trajectory angle from vertical rise and horizontal run of shelf-edge migration: atan2(rise, run). Positive angles are aggradational, negative retrogradational.

Description

Shelf-edge trajectory angle from vertical rise and horizontal run of shelf-edge migration: atan2(rise, run). Positive angles are aggradational, negative retrogradational.

Shelf Edge Trajectory Angle Calculator: Shelf-edge trajectory angle from vertical rise and horizontal run of shelf-edge migration: atan2(rise, run). Positive angles are aggradational, negative retrogradational.

When to use Shelf Edge Trajectory Angle

Use this geological calculation for a transparent first-pass interpretation of measured rock, soil, fluid, well, stratigraphic, isotopic, geophysical, or seismic data under an explicitly selected model.

Rise (m)
Vertical component of shelf-edge migration in metres (positive up, negative down).
Run (m)
Horizontal progradation distance of the shelf edge in metres.

How Shelf Edge Trajectory Angle works

Shelf-edge trajectory angle from vertical rise and horizontal run of shelf-edge migration: atan2(rise, run). Positive angles are aggradational, negative retrogradational. The tool evaluates the supplied inputs together and returns the named outputs below; it does not infer omitted operating conditions or change the units shown.1

Trajectory
Shelf-edge trajectory angle in degrees from horizontal (-90 to +90).

Limitations and assumptions

  • Stratal terminations and systems tracts are interpretations sensitive to seismic resolution, datum, compaction, subsidence, sediment supply, chronology, and depositional model. A geometric angle or thickness alone does not identify sequence boundaries.
  • Use finite inputs in the displayed units and preserve more precision than the final presentation requires. Independently verify safety-critical, financial, compliance, or production decisions.

Alternative or Complementary approaches

Compare independent measurements and models, retain units and analytical metadata, propagate uncertainty, and validate interpretations against logs, cores, maps, laboratory data, or field observations.

References

  1. Sequence stratigraphy — Wikipedia contributors

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