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THESIS PROPOSAL
DEGREE PROGRAMME: M. Sc.
SUPERVISOR and COMMITTEE: Supervisor - Grant Wach
Committee Members - Marcos Zentilli, Martin Gibling, David Brown (CNSOPB)
TITLE OF PROPOSAL: Examination of architectural elements of Mesozoic rift basin sediments, Scotian margin.
KEY WORDS Scotian Shelf, resevoir characterization, rift basin, salt, diapirs, ground penetrating radar (GPR),
light detection and ranging (LiDAR), 3D digital modeling
LIST INNOVATIONS or EXPECTED SIGNIFICANT OUTCOMES:
1. The first three-dimwnsional, high resolution (< 15 m ) geologic digital model of
subsurface siliciclastic bedforms with implication to Scotian Margin sediment fill. The
model will produce new insight into reservoir sediments in the Orpheus Basin with
implications to potential hydrocarbon production and liquid phase CO2 injection.
2. Develop improved sedimentation and structural constraints describing braided channel
architectural elements clearly defining fluid reservoirs and potential fluid flow.
3. Assess reservoir heterogeneity of basin fill, with implication for hydrocarbon potential
for the naturally occurring Orpheus Graben sedimentary basin.
SUMMARY OF PROPOSED RESEARCH: The preferred technique for examination of Scotian Basin sedimentary fill has principally been
sequence stratigraphy (Wade and MacLean 1990; Wade et al. 1995; Piper et al. 2005). However,
due to the presence of basin sediment deformation of architectural elements the Scotian Basin
reservoir rocks are not well understood (Piper et al. 2005). Through use of highresolution
geologic digital modeling, reservoir analogues depicting architectural elements and geometric
features of related outcrop sediments can be characterized and applied to determine the reservoir
sedimentological and structural analysis of offshore basin fill.
Recent investigation into analogous outcrops along the Scotian and Fundy Basins include studies
of the Wolfville Formation along the Bay of Fundy (Kettanah 2008; Nickerson 2010). The
Wolfville Formation provides 2D and 3D imagery of exposed braided channel siliciclastic
deposits, demonstrating reservoir complexities associated with mid- to Late-Triassic depositional
environments. This sedimentological and structural analogue will prove useful for interpretation
of subsurface log and core successions and in defining models of fluid flow in complex
reservoirs of Orpheus Graben sediment fill.
This study will focus on characterizing heterogeneities of architectural elements in midto Late-
Triassic reservoir sediments of the Orpheus Graben. Three stages of study will be used to resolve
reservoir heterogeneities of architectural elements: 1) Outcrop analysis, including gamma
scintillometer and permeameter readings, of the synchronously forming Wolfville and Eurydice
formations; 2) Subsurface analysis, including seismic and well log interpretation, core and
cuttings description, and thin section petrography, of the Orpheus Graben basin fill; and 3)
Development of a high-resolution three-dimensional geologic digital model of the Wolfville
Formation siliciclastic sediments, using innovative techniques of GPR and LiDAR, for
application to offshore Orpheus Graben Eurydice Formation sediments. The combination of all
three studies will allow for high-resolution architectural element conditions to be characterized
for onshore sediments and used as an analogue for offshore basin fill characterization.
Statement of Problem
Rift basins are elongate depressions overlying areas of lithospheric extension and are important,
ubiquitous depositional environments which often contain potential reservoir sediment fill (e.g.
Jeanne D'Arc Basin and Tupi Basin) (Olsen 1997; Burke, 1985). The Orpheus Graben (Fig. 1),
offshore Nova Scotia, is well acknowledged as a previous rift and passive margin basin
containing rift related braided stream deposits. These sediments also outcrop along coastal
sections of Nova Scotia, namely as siliciclastic braided channel complexes of the Wolfville
Formation. However, previous investigation into these basin reservoir rocks has revealed
sedimentological and structural deformation resulting in a poor understanding of the sedimentary
units (Wade and MacLean 1990; Piper 2005). Because the proximity of the Orpheus Graben to
Nova Scotia, the onshore coastal sections of braided channel complexes offer an exceptional
depositional analogue to refine the architectural elements of the offshore reservoir sediments.
This study will investigate the architectural elements of the outcropping Wolfville and Eurydice
formations, through digital geologic reconstruction, in order to better constrain the
characterization of architectural elements of Scotian margin sediments. The first part of the study
uses a combination of standard descriptive methods to identify commonalities between onshore
outcrops to offshore subsurface data. Collected data will be used to determine the architectural
elements of onshore and offshore sediments, constraining the use of the onshore sediments as an
analogue for offshore basin fill. The second part of this study uses innovative methods to
digitally reconstruct architectural elements of the onshore Wolfville Formation to further
improve reservoir characterization of offshore subsurface sediments. Interpretation of 2D and 3D
GPR reflection data will be conducted to determine variation in braided channel architectural
elements to determine sedimentation patterns. Part three of this study will use the created model
to employ interpretive reservoir conditions to analyze fluid flow with implications to potential
hydrocarbon emplacement and CO2 liquid injection storage. This study will improve
understanding of small scale architectural elements of Scotian margin basin fill and will put
constraint on areas suitable for hydrocarbons exploration and CO2 liquid injection storage.
Figure 1 Generalized map approximately during the Triassic illustrating depositional environments around Nova Scotia. The three locations of study
are indicated by yellow boxes (outcropping Wolfville and Eurydice formations) and a red box (offshore Orpheus Graben). The current outcrops are noted as either lowland or lake depositional environments. The Orpheus Graben is noted to contain similar lowland environments but with the
addition of shallow salt water and salt evaporites (after Wade 1990)
Background The study region is located in the Northern Canadian Cordillera in the Mackenzie Mountains and
Mackenzie Plain, around the region of Norman Wells (approximately 65o W, 126o N) (Fig. 1).
The project will use apatite fission-track thermochronology (AFT) to determine upper cooling
history of Mackenzie Mountains and Plain in order to determine temporal correlations between
cooling history and key structural events.
Regional Geology - Scotian Basin
The Scotian Basin is a passive conjugate margin recording 250 million years of fluvialdeltaic-
lacustrine and deep water sedimentation, offshore Nova Scotia, Canada. Sedimentation occurred
during the continental breakup and rifting events, during the early- to Late-Triassic, as North
America separated from Africa forming a number of juxtaposed and interconnected subbasins
(Wade and MacLean 1990; Wade et al. 1996; Weir-Murphy 2004;). These subbasins have a
maximum sediment thickness of over 24 km and are known from south to north as the
Shelburne, Sable, and Abenaki subbasins, and the Orpheus Graben. Syn-rift mid- to late-Triassic
mixed clastic and carbonate redbeds (Eurydice Formation) were the earliest sediments deposited
into the subbasins (Wade et al. 1996) (Fig. 2). Late Triassic rifting furthered plate separation
with episodic incursion of marine waters into the newly formed basins. At equatorial latitude,
restricted marine waters formed a succession of evaporitic deposits. These deposits of salt are
separated sporadically by thin red shale beds (Argo Formation) (Wade et al. 1996; Weir-Murphy
2004) (Fig. 2.0). A period of tectonic quiescence followed until the mid-Sinemurian, recorded by
complex and heavy faulting of the mid to Late-Triassic Eurydice and Argo formations (Weir-
Murphy 2004). This tectonic renewal coevolved with the opening of the Atlantic Ocean and
complete separation of the North American and African plates. In the Late Sinemurian to Early
Bajocian, shales deposited during marine transgression largely covered the sedimentary basins.
Shallow marine dolomites and clastics (Iroquois Formation) and terrestrial fluvial coarse-grained
clastics (Mohican Formation) were deposited (Wade and MacLean 1990). Increased overburden
pressure initiated salt mobilization with the formation of a number of salt pillows and diapirs
(Wade and MacLean 1990). Delta progradation followed, producing shallow marine sandstone
and limestone beds during the Late Jurassic (Wade et al. 1996). Eustacy changes during the
Cretaceous resulted in a series of coarse clastic fluvial deposits and marine shales, marl, and
chalk deposits (Dawson Canyon Formation) and have continued into the Tertiary (Wade and
MacLean 1990).
Figure 2 Stratigraphic column of the Scotian margin. Located above the metasediment and igneous
basement rocks are the Eurydice Formation redbeds formed during the mid- to Late-Triassic. These
sediments are under investigation in this study as potential sources of hydrocarbon exploration and
liquid phase CO2 injection. Using synchronously formed outcrops (Wolfville and Eurydice
formations), offshore Eurydice formation architectural elements can be characterized
(www.CNSOPB.ns.ca- modified from Wade et al. 1996)
Regional Geology - Fundy Basin
The Fundy Basin is composed of a number of Mesozoic rift basins (Minas, Fundy, and
Chignecto subbasins) representing Triassic, stratigraphically complex half grabens fluids with 6-
12 km of clastic sediments (Leleu & Hartley 2010; Wade et al. 1996). The Minas subbasin
contains two stratigraphic units of approximately 1050 m in total thickness; the Wolfville
Formation (800 m) and Blomidon Formation (250 m), each extending from onshore outcrop to
offshore subsurface (LeLeu and Hartley 2010; LeLeu et al. 2009). The Wolfville Formation
(mid- to Late Triassic) comprises a range of depositional environments from coarse- to
finegrained fluvial sandstones, aeolian dune sandstones, and alluvial fan sediments, all of which
unconformably lie on the Carboniferous sediments (Klein 1962; Hubert & Mertz 1980; Leleu &
Hartley 2010; Wade et al. 1996). The overlying Blomidon Formation (Late-Triassic to Early-
Jurassic) contains tabular, massive, and cross-bedded fluvial sandstones, and laminated
lacustrine mudstones with rare evaporites (Leleu & Hartley 2010). Both formations are exposed
along the south-eastern shore of the Minas subbasin, and demonstrate the internal 2D and 3D
stratigraphic and structural complexities of the early sedimentation of clastic fluvial and alluvial
sandstone.
Physical Analysis Physical analyses of both onshore outcrops and offshore core have been largely used to describe
variability in large-scale, basin-wide sedimentation and structural properties (Wade et al. 1996;
Leleu et al. 2009; Leleu & Hartley, 2010). Application of small-scale physical elements (i.e.
sedimentary structures, gamma ray spectra, permeability, and porosity measurements) will allow
for comparison, and geological linkage, between the two sedimentary systems (Vaughan, 2011).
Successful comparison between onshore and offshore sediments is fundamental for application
of a 3D geologic model to offshore sediments.
Conceptual Modeling Analogues Most work for describing architectural elements of sedimentary fill has relied on the use of either
GPR (Neal, 2004) or LiDAR (Labourdette, 2011; Hajek & Heller, 2004) separately creating 2D
models. Recent innovative work (Vaughan, 2011) has conjoined both GPR 3D profile data with
LiDAR outcrop measurements to form digital 3D models illustrating stratigraphic and structural
complexities of braided channel complexes.
Both 2D and 3D digital modeling from ground penetrating radar (GPR) and light detection and
ranging (LiDAR) have tested the analysis of architecture and dimensional distribution of fluvial
and alluvial depositional systems, principally in conjugate margin settings of Nova Scotia
(Vaughan, 2011) and Spain (Labourdette, 2011). The use of these digital models has shown to be
effective for high resolution application in understanding the distribution and connectivity of
related lithological bodies (i.e. permeable paths and barriers) in both hydrocarbon and
hydrological reservoirs (Labourdette 2011; Larue & Hovadik 2006; Neal 2004; Nickerson 2010).
Other uses include the formation and distinction of fluvial and alluvial depositional systems
(Vaughan, 2011; Labourdette, 2011), the differentiation between distribution of differing
lithologies (i.e. muds and sands) (Lynds and Hajek, 2006), and the influence of tectonic regimes
on basin structure. Such models allow for the incorporation of specific morphological data (i.e.
strata orientation, thickness, width, relationships to each other) to both small scale physical
outcrop entities (i.e. grain size, fossil fragments) and large scale physical outcrop entities (i.e.
faulting). Incorporating physical outcrop measurements (permeability, porosity, gamma ray) into
the 2D and 3D digital models will yield more geologically comprehensive digital models.
Comparing digital models and physical analysis Recent studies using LiDAR have described the stratigraphic and structural characterization of
outcrop in regards to creating 2D reservoir analogues (Labourdette, 2011; Labourdette, 2007;
Hajek & Heller, 2004; Lynds & Hajek, 2005). Only few studies have attempted creation of 3D
digital analogues using 2D GPR profiles and 2D LiDAR images to compare subsurface and
outcrop data (Vaughan, 2011). This work demonstrates that 1) The technique in creating a 3D
digital analogue is viable, and 2) The feasibility of using the digital model for assessment of
comparable rock formations is possible. This shows that it is possible to combine the digital
model with physical outcrop and core measurements to create a comprehensive and complete 3D
geologic model. This coupled framework will provide increased understanding on reservoir
architectural elements with implication for potential hydrocarbon production and liquid phase
CO2 injection (Wade et al. 1996; Leleu & Hartley, 2010; Kettanah, 2009). OBJECTIVES
Using three-dimensional data and description of analogous outcrop and subsurface data, the
overall good of the proposed research is to assess the small-scale (< 15 m) reservoir architectural
elements of Orpheus Graben sediment fill. Regional correlation, through comparison of onshore
outcrop to offshore subsurface sediment, will allow for application of high-resolution, 3D digital
geologic models to offshore basin fill and will be completed using the following objectives:
Construct a type log from existing well data (seven wells) from the Orpheus Graben.
Analyze and spatially correlate lithological, sedimentological, and structural
characteristics of mid- to Late-Triassic Eurydice and Wolfville formations and Orpheus
Graben basin fill.
Create a three-dimensional model of high-resolution (< 15 m) structural and stratigraphic
heterogeneity of braided channel complexes of the Wolfville Formation, determining
variation in channel architecture and geometry with implication on sedimentation patterns
and potential fluid flow.
Application of three-dimensional geologic model for potential hydrocarbon production
and liquid phase CO2 injection.
METHODS
Outcrop and Well Core Analysis
Measured Sections: This analysis will involve a detailed description of lithological and sedimentological elements of
the Wolfville and Eurydice formation outcrops (Fig. 1.0) can be completed using outcrop
analysis through measured sections. Through direct outcrop examination, characterization of
lithology (clast size and composition), laminae and bed thickness, physical and biogenic
sedimentary structures, and structural features will be measured and recorded.
Thin Sections: Through use of thin sections, the grain shape and size, cement, and major rock forming minerals
can be identified for outcrop and well cores. Using a polarized-reflected light petrographic
microscope, mounted thin sections can be placed under the field of view. Objectives between
10X to 40X magnification, depending on the level of magnification needed, sample properties
can be identified and collected.
Scintillometer: Outcrop and well core can be classified through gamma scintillometer measurements of
radioactive elements uranium, thorium, and potassium. By resting the handheld gamma
scintillometer next to a representative sample of interest, the radioactive content of the sample
can be measured.
Permeameter: The permeameter (Tiny Perm II) is a handheld tool used for determining rock sample
permeability (i.e. the measurement of the ability for a material to transmit fluid or air). The unit
consists of a cylinder air piston wired to a palm sized computer and display. Holding the
permeameter to a clean, flat, dry rock sample surface, and engaging the air piston, the
permeability of that sample can be measured.
Core Analysis: Cores stored at the Canada-Nova Scotia Offshore Petroleum Board (CNSOPB) are described by
examining and recording colour, lithology, induration, sedimentary structure, clasts presence,
and mineralogy. Through physical and photographic observation the sedimentological and
lithological characteristics of the well core are collected, described, and recorded.
Well Cuttings Analysis: Rock sample lithology and porosity can be determined through well cuttings analysis. Well
cuttings are analyzed by placing them in a sample tray under an optical microscope field of view
(FOV). The correct magnification (usually 10X objective) must be used to identify the rock
characteristics.
Seismic Reflection Data: Publicly available digital portable document format (PDF) files of seismic records were obtained
through the Data Management Center (DMC) of the CNSOPB. These will be used to describe
the Orpheus Basin rift architectural elements with identification of faults, salt movement, and
lithological changes. PDF seismic lines will be converted into SEG-Y files and imported into
Petrel computational software for interpretations.
Application: A complete and detailed physical characterization of outcropping Wolfville and Eurydice
formations and Orpheus Graben well core provides can be completed using the above methods.
The combination of these tools allows for complete insight on large scale (~20 m) to small scale
(grain size) features of onshore and offshore rock units. Together these methods provide insight
on architectural element characteristics, along with reservoir quality, to allow for type log
construction and the comparison of onshore Wolfville and Eurydice formations to offshore basin
fill. When applied to the 3D digital geologic model, these methods will be used for
characterizing reservoir quality and fluid flow with implication for describing potential
hydrocarbon production and liquid phase CO2 injection.
Outcrop Subsurface and 3D Digital Environment Reconstruction
Ground Penetrating Radar (GPR): GPR is a surficial geophysical method which uses electromagnetic energy transmission and
reflection to detect electrical discontinuities within changing shallow Earth subsurface materials
(Neal 2004). Through detection of changes in lithology, varying subsurface architectural
elements of the Wolfville Formation braided channel complex can be identified.
In this study GPR is used in a common offset geometry consisting of two, separate antennae, one
each for transmitting and receiving, set at a predetermined fixed spacing, oriented perpendicular
to the survey line, and attached to a mobile carbon fibre cart. The antennas are directly attached
to the electromagnetic transmitting and receiving devices and act as beginning and end points for
propagating electromagnetic energy. As electromagnetic pulses are sequentially collected
following reflection, a radar reflection profile is built (Neal 2004). This study will use two
different frequencies of antennae: 50 Hz and 100 Hz. The low frequency 50 Hz antennae allow
for deep subsurface penetration, up to ~20 m depending on lithology, but at a low subsurface
resolution. The 100 Hz antennae have a maximum depth penetration of ~12 m, but have
increased subsurface resolution (Neal 2004).
GPR Profile Processing: Processing of raw GPR radar profiles will be performed using the software package
EKKO_View Delux. Radar profile processing is essential in removing several types of noise to
yield a useful subsurface profile for identification of structural and stratigraphic subsurface
properties.
Data lines are imported into EKKO_View Delux as unprocessed subsurface 2D profiles. A series
of processing operations (gains and filters) must be applied. Processing filters used by Jol and
Smith (1991) and Vaughan (2011) include the removal of low frequencies, reduction in
electromagnetic noise, the removal of background noise, and the compensation for amplitude
attenuation with propagation. These allow for a clear 2D subsurface profile to be created. After
completing data processing, the radar profiles are exported in SEG-Y seismic format (Vaughan
2011).
Light Detection and Ranging (LiDAR): LiDAR is a remote sensing technology used to optically map and measure distance to and shape
of a given surface. Using LiDAR, this study will demonstrate lithological, sedimentological, and
structural changes in surface outcrop of the Wolfville Formation. LiDAR is able to detect
surficial changes in outcrop by using pulses of light, ranging from ultraviolet to infrared, from an
onboard laser. By detecting surficial changes in outcrop, architectural elements, geometries, and
fluid flow of braided channel complex sediments can be characterized for geologic
reconstruction and modeling (Labourdette 2011). Data collection consisted of placing the unit 25
m to 100 m from the outcrop, positioned so laser propagation and reception were facing the
outcrop. High resolution photos and a grid over a predetermined surficial region are acquired.
The laser beam is emitted toward the surface and is reflected back to the receiver on the LiDAR.
These laser point clouds are processed to generate three-dimensional pixel point-clouds of the
scanned area (Labourdette 2011)
LiDAR Post Processing: Processing of LiDAR data is completed using Polyworks to align, edit, and views three-
dimensional data, and merge multiple scans into a single three-dimensional point cloud.
Construction of 3-D Digital Environment: Developing a three-dimensional model of the Wolfville Formation braided channel complex
involves the incorporation of processed GPR radar profiles with LiDAR point-cloud images.
Adjacent data sets are combined and are spatially oriented, allowing for visualization of the
lithologies and structural geometries into the subsurface GPR radar profiles. Individual radar
horizons are identified and mapped on each radar profile through manual digitization of the
three-dimensional polygons.
Application: Radar reflection profiles from GPR surveys demonstrate subsurface lithological
contacts and provide initial insight into stratigraphic characteristics of gross lithological and
structural information (Neal and Roberts 2000). Processed GPR radar profiles produce
highresolution subsurface images revealing heterogeneities of architectural elements of braided
channel complexes in the Wolfville Formation. Specific subsurface architectural elements can be
determined, such as faults and changing lithologies, which are important for characterizing
reservoir quality and fluid flow.
Point-cloud images from LiDAR surveys provide high-resolution three-dimensional photos for
characterizing the complexities of reservoir quality. LiDAR is capable of aiding in discerning
physical outcrop heterogeneity while providing a surficial basis for which subsurface
interpretation can be made. These three dimensional point-clouds can be used to define
stratigraphic and structural outcrop geometries of braided channel complexes.
Together the GPR profiles and LiDAR point-cloud images will provide a basis for construction
of the three-dimensional digital geologic model, later applied to the Orpheus Graben reservoir
system. Understanding the subsurface architectural elements of the Wolfville Formation braided
channel complexes allows for characterization of offshore reservoirs with insight on potential
fluid flow and further implication in deciphering potential hydrocarbon production and liquid
phase CO2 injection.
Results and Significance
Develop improved sedimentation and structural constraints describing braided channel
architectural elements clearly defining fluid reservoirs and potential fluid flow.
Introduction of the three-dimensional model to offshore basin fill sediments will allow
for reservoir characterization of sedimentological and structural elements. At a
highresolution, the model will produce new insight into reservoir sediments in the
Orpheus Basin with implications to fluid flow.
Assess the reservoir potential of the Orpheus Graben for both hydrocarbon potential and
CO2 liquid injection. Overall, this study will illustrate the importance of using
highresolution geologic models as analogues for reservoir characterization of offshore
sediment.
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