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Colorado School of Mines. Arthur Lakes Library

Faults and fractures in the Niobrara Formation of Wattenberg field, Colorado

Abstract

dc:description.abstract

Faults are an important element of reservoir characterization because they have the potential to compartmentalize a reservoir and create associated fractures that can profoundly influence fluid flow in the reservoir. This investigation describes details of the fault regime in a portion of the Wattenberg Field, Colorado. For the purposes of this study, seismic-scale faults are interpreted as horizons with displacements. Seismic-scale fractures are interpreted as linear amplitude discontinuities. Borehole image log scale faults show displacement. Borehole image log scale fractures do not show displacement. Both borehole image log scale faults and fractures are interpreted as seismic-scale fractures. Faults were discovered by interpreting inflection points in cumulative dip plots and azimuth walkout plots derived from a borehole image log in a vertical well. On the image log fractures are consistently found in both the Niobrara chalk and marl benches. The individual benches are not resolvable at the scale of the seismic data, but evidence that faults are present in both the chalks and marls lends credence to the potential that seismic data may be able to predict fracture zones either directly or indirectly. The hypothesis is tested on a 50 square mile 3D seismic survey. Generally, faults present in the Niobrara Formation in the survey are planar, normal faults that range up to two miles in length. Over 150 faults were picked. Rose diagrams illustrate a predominant strike direction of N 20 E. A predictive fracture volume was generated utilizing CGG’s proprietary software: InsightEarthTM. The algorithm generates this volume statistically based on fault geometry. Each seismic-scale fault indicates a high potential for fracture swarms in the nearby vicinity. Fracture prediction can assist future exploration and development in the Niobrara resource play.

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
2016

Author and committee

dc:creator, dc:contributor.*
Author dc:creator
  • Brush, Jennifer F.
Advisor dc:contributor.advisor
  • Davis, Thomas L. (Thomas Leonard), 1947-
Committee members dc:contributor.committeemember
  • Trudgill, Bruce, 1964-
  • Hurley, Neil F.
  • Nissen, Edwin

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 8070
OAI identifier oai:identifier
oai:repository.mines.edu:11124/170259

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

Brush, Jennifer F.. Faults and fractures in the Niobrara Formation of Wattenberg field, Colorado. Masters thesis, Colorado School of Mines. Arthur Lakes Library, 2016. https://hdl.handle.net/11124/170259