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Colorado School of Mines. Arthur Lakes Library

Microseismic guided wave eigenfunction theory with application to event depth classification in the Eagle Ford shale

Abstract

dc:description.abstract

The properties of guided waves that propagate in deep low-velocity zones are investigated using eigenfunction theory, and a novel application for microseismic event depth constraint to an unconventional reservoir is developed. Eigenfunctions, historically used in the analysis of Rayleigh and Love surface waves, allow rapid calculation of response functions that are linearly-correlated with guided wave displacements as a function of source depth, with only a 1-D velocity model required for their input. These response functions are used to investigate the impact of velocity contrast, reservoir thickness, and receiver depth on guided wave amplitudes for discrete frequencies. It is found that receivers located within the low-velocity zone record larger guided wave amplitudes, which may be used to infer the location of a recording array in relation to a low-velocity reservoir. The energy distribution of guided waves between layers and dispersion modes in a model representing the Eagle Ford Shale is then studied. High frequency guided wave energy is found to be largely confined to the Eagle Ford, and the modal energy distribution shows a nodal point in the first higher mode for events originating in the middle of the Eagle Ford. These observations are corroborated with field microseismic data recorded in the Eagle Ford during hydraulic fracturing, and provide possible constraints for microseismic event depth. To this end, a depth classification algorithm is developed based on the confinement of guided wave energy. This algorithm is applied to microseismic DAS data from the Eagle Ford, and quantifies the amplitude of guided wave energy relative to background noise in order to classify events with strong guided waves as occurring within or close to the Eagle Ford, circumventing the large depth uncertainties associated with measurements from surface arrays. Analysis of the horizontal locations of the in-reservoir events shows them to be closer to the stimulation well than the out-of-reservoir events, providing a constraint on stimulated reservoir volume that may improve well-spacing decisions.

Degree

thesis:*
Name thesis:degree_name
Master of Science (M.S.)
Level thesis:degree_level
Masters
Discipline thesis:degree_discipline
Geophysics
Grantor dc:publisher
Colorado School of Mines. Arthur Lakes Library
Year dc:date.issued
2021

Author and committee

dc:creator, dc:contributor.*
Author dc:creator
  • Huff, Owen R.
Advisor dc:contributor.advisor
  • Jin, Ge
Committee members dc:contributor.committeemember
  • Simmons, James
  • Lellouch, Ariel
  • Sonnenberg, Stephen A.

Subjects

dc:subject × 6

Rights

dc:rights
Statement dc:rights
  • Copyright of the original work is retained by the author.
Language dc:language.iso
eng, English

Identifiers

dc:identifier.*
Identifier
T 9158
OAI identifier oai:identifier
oai:repository.mines.edu:11124/176469

Chain of custody

source
Harvested from
Colorado School of Mines
Base URL
repository.mines.edu/server/oai/request
Last updated
2026-07-24
Source record
OAI-PMH GetRecord
citation

Huff, Owen R.. Microseismic guided wave eigenfunction theory with application to event depth classification in the Eagle Ford shale. Masters thesis, Colorado School of Mines. Arthur Lakes Library, 2021. https://hdl.handle.net/11124/176469