World-class training for the modern energy industry

Type: Field

Natural Hydrogen, Pau, France (G582)

Tutor(s)

Eric Gaucher: CEO, Lavoisier H2 Geoconsult and RockyH2.

Jean Gaucher: Development Officer, Lavoisier H2 Geoconsult.

Overview

The last few years has seen a growing interest in natural hydrogen accumulations. We know that there are a variety of processes that can lead to hydrogen being produced in the Earth’s crust but there is much still to understand about these, how much is perhaps present in subsurface stores and where these accumulations are. Commercial exploitation will also need to assess the engineering challenges for extracting this hydrogen and ultimately how best it can be utilised as part of the changing face of our modern energy landscape. This course will give an integrated view on the economic, strategic and scientific aspects of natural hydrogen exploration and its perspectives.

Duration and Logistics

Virtual version: Four 3.5-hour online sessions presented over four days comprising a mix of lectures, exercises, case studies and discussion. The course manual will be provided in digital format.

Fieldtrip version: A 5-day field course located in Pau, France with a focus on the geological aspects of natural hydrogen.

Level and Audience

Fundamental. The course is largely aimed at geologists interested in natural hydrogen occurrences but the trainers able to adapt the level of the course to the requirements of the attendees.

Exertion Level

This class requires and EASY exertion level. Travel is by small coach and there are hikes of less than 10 minutes in duration (less than 1 km) on well-graded terrain in the foothills of the Pyrenees.

Objectives

You will learn to:

  1. Evaluate the different types of hydrogen and the origins of natural hydrogen.
  2. Characterise the strategies for the exploration of natural hydrogen.
  3. Clarify and organize the different technical steps of a natural hydrogen exploration programme.
  4. Appraise the geological, geochemical and geophysical tools that can be used for natural hydrogen exploration.
  5. Assess the co-production of natural hydrogen with geothermal resources, Helium and the mining industry.
  6. Assess the techno-economic evaluation of natural hydrogen.

Basin-Scale Stratigraphy (Source-to-Sink): Basins of the Pyrenean Foreland, Spain (G117)

Tutor(s)

Rene Jonk: Director, ACT-Geo Consulting and Training; Honorary Professor, University of Aberdeen.

Overview

Well-exposed outcrops of the Pyrenean Foreland Basin (PFB) in northern Spain offer a unique opportunity for source-to-sink analyses across thrust and foreland basin settings. This course demonstrates regional linkages of continental to marine environments and teaches fundamentals of play-scale reservoir, source and seal mapping and prediction. We utilize 3D outcrop models, detailed biostratigraphic data and subsurface examples to enhance learning through making maps and predictions. The course presents sequence stratigraphic models across continental, shelfal and deep-water settings in order to understand the external controls on sediment flux from the proximal to distal environments.

Duration and Logistics

A 6-day field course, based in the Pyrenees, with the itinerary dependent on the technical objectives of the group and timeframe. 60-80% of the time will be spent in the field, making active observations and undertaking field exercises, in combination with some classroom exercises and lectures as well as the option for viewing core.

Level and Audience

Intermediate. The course is specifically designed for reservoir engineers, geologists and geophysicists interested in analysing a range of clastic reservoir types from a variety of depositional settings. The field course will examine the reservoir attributes of a wide range of sand-prone deposits focusing on the reservoir quality and property distribution as well as larger scale correlation and gross architecture of distinct stratigraphic units. In addition, play-scale prediction of reservoir, source and seal elements will be covered and play-based evaluation techniques will be discussed and practiced.

Exertion Level

This class requires an EASY exertion level. Access to the outcrops is easy with many being road cuts. The longest walk is approximately 3 km over scrubby land. The field area sits at an altitude of up to 1000 m and the weather can be warm with daily highs over 25 degrees Celsius.

Objectives

You will learn to:

  1. Review facies associations in siliciclastic depositional systems.
  2. Predict external controls on sediment flux from continent to basin.
  3. Study the effects of compressional tectonics and the interaction of tectonics and sedimentation.
  4. Assess proximal to distal environments of deposition (EoD) and link them in space and time.
  5. Employ sequence stratigraphic models to continental, shelf and deep-water settings.
  6. Build stratigraphic frameworks across various scales and EoD.
  7. Predict occurrence of basin-scale play elements.
  8. Place local interpretations into regional context for predictions away from well control.
  9. Examine where sediment is stored in shelf environments, as well as when and how sediment is transported to deep water.

Deepwater Clastics: Source-to-Sink Studies in the Exploration of Turbidite Reservoirs, San Diego, California (G103)

Tutor(s)

Zane Jobe: Research Professor, Colorado School of Mines and the Director of the Geology Center of Research Excellence (CoRE).

Overview

The course will visit spectacular outcrops along the California coastline just north of San Diego. Field work will follow a source-to-sink approach and will focus on specific deepwater architectural elements, including canyons, slope channels, channel-lobe-transition-zones and lobes. The course will provide insights into exploration and development themes and challenges in deepwater depositional systems, with direct analogs to Gulf of Mexico reservoirs.

Duration and Logistics

A 6-day field course based in La Jolla, California. Training will take place through in-class presentations, field observations, printed exercises and discussions in the field. Transport will be by coach.

Exertion Level

This class requires a MODERATE exertion level. Access to the coastal cliff outcrops is via sandy beaches with walks no more than 3km (1.9 miles). Field stops are all at approximately sea level and some are tide dependent. There are some steep steps to negotiate to reach some beach sections.

Level and Audience

Intermediate. The course is aimed at geoscientists, engineers, petrophysicists, geophysicists and managers who are working deepwater reservoirs or would like to improve their knowledge of these systems.

Objectives

You will learn to:

  1. Characterize the sedimentary processes and facies of turbidite systems and mass-transport deposits, and the broad nature of submarine depositional architecture.
  2. Evaluate submarine-channel systems, including scales/dimensions, axis-to-margin architecture, evolution, heterogeneity and potential baffles/barriers to flow.
  3. Predict connectivity in channelized systems from their seismic-geomorphic and well-log expression.
  4. Assess submarine canyon forming-and-filling processes, including mass wasting, bypass, sandy and muddy fill, and up-dip trapping mechanisms.
  5. Illustrate the importance of source-to-sink studies in the exploration of turbidite reservoirs.
  6. Evaluate submarine lobe/sheet systems, including scales/dimensions, axis-to-fringe architecture, compensational stacking, hierarchy and heterogeneity (e.g. hybrid-event-beds).
  7. Analyze channel-lobe-transition-zone deposits and supercritical-flow bedforms.
  8. Assess faulting in lobe deposits and impacts on connectivity.
  9. Appraise the facies variability in proximal/axial and distal/fringe lobe deposits, and the implications for connectivity between these sub-environments.

The Geology of the Paradox Basin and Implications for Deepwater Gulf of Mexico Exploration, Moab, Utah (G095)

Tutor(s)

Kate Giles: Lloyd A. Nelson Professor, University of Texas at El Paso; Consulting Geologist.

Overview

The primary technical goal is to provide a widely applicable introduction to the interrelationship between sedimentation and structural geology with a particular focus on salt tectonics and salt-sediment interaction. The geology is examined with reference to deepwater exploration themes with the Gulf of Mexico.

Duration and Logistics

A 4-day field course starting and finishing in Grand Junction, Colorado, comprising a mixture of lectures, field work and exercises.

Level and Audience

Intermediate. This course requires a basic understanding of geoscience and will suit those working in the geoscience, geotechnical and engineering fields. The aim is to facilitate knowledge and experience exchange among the participants, so is open to those from a very wide range of experience levels.

Exertion Level

This course requires a MODERATE exertion level. There will be hikes to outcrops of up to 6.5km (4 miles) round trip. Some of these will encounter uneven and rocky ground with some short, steep inclines. The climate in southern Utah is typically warm to hot and dry with temperatures up to 37.5°C (100°F) and the elevation is between 1,250–1,500m (4,000–5,000 ft).

Objectives

You will learn to:

  1. Describe the regional stratigraphy and principal structural features of the Paradox Basin, Utah.
  2. Characterize and interpret controls on Paradox Basin salt-related structures and key features of passive diapiric systems, including halokinetic sequences, caprock development, non-evaporite stringers / inclusions, welds, megaflaps, counter-regional faults, radial faults and burial wedges.
  3. Examine stratal geometries and halokinetic sequences and how these relate to intervals of salt inflation / evacuation and sediment flux.
  4. Assess the controls on basin fill architecture, fluid flow and deformation within the Paradox Basin and compare this to analogous salt basins worldwide.
  5. Understand the importance of salt basins to the energy industry for hydrocarbon production.

Slope-Channel Depositional Systems: Brushy Canyon Formation, SE New Mexico and West Texas​ (G091)

Tutor(s)

Art Saller: Independent Geological Consultant.

Overview

This field course is designed for geoscientists and engineers exploring and developing deepwater clastic reservoirs anywhere in the world. The course examines excellent (classic) exposures showing depositional facies and stratal geometries developed in deepwater slope and channel environments and their controls on reservoir presence, quality and production. Outcrop description and exercises with subsurface data are integrated into the course. Analog fields from West Africa, Gulf of America/Mexico, southeast Asia and the Permian Basin are discussed on outcrops.

Duration and Logistics

A 6-day field course beginning and ending in El Paso, Texas. Most training will take place through observation and discussion in the field.

Level and Audience

Advanced. The course is aimed at geoscientists, petrophysicists, reservoir engineers and production engineers working deepwater siliciclastic reservoirs. Basic principles are presented on the first morning to bring participants to a common level of understanding. Outcrop viewing, description and exercises will give even advanced level participants improved understanding of these systems.

Exertion Level

This class requires a DIFFICULT exertion level. The outcrops are in west Texas and southeast New Mexico, where the weather is arid with hot summers and cool winters. This trip is run in spring or fall when temperatures are more moderate, although hot, cold or wet weather is possible. Daily temperatures can range from 5–30°C (40–90°F). The course includes a hike of around 6 km/4 miles with an ascent of 400m (1300 ft), and shorter hikes, frequently over very steep and uneven ground. Transport on the course will be by coach. Most of the driving is on black-top roads, with some driving on graded dirt roads.

Objectives

You will learn to:

  1. Visualize the seismic-scale geometries of major slope channel systems including incised upper slope valleys, amalgamated mid-slope channel-complexes, and middle to lower slope channel-levee complexes for use in subsurface interpretation.
  2. Assemble a predictive model for those different sand geometries relative to slope position.
  3. Describe different deep-water (turbidite) facies and understand variations in their distribution and reservoir characteristics in different architectural elements (channel, levees, splays).
  4. Relate outcrop and core scale variations of deepwater sands to wireline log characteristics within channel complexes to help interpret facies in logs.
  5. Predict how turbidites and their characteristics change laterally which can be applied to static and dynamic reservoir models for appraisal and development.
  6. Assess thin turbidite sand beds and understand where they occur deep-water systems and how their continuity can vary from relatively limited areal continuity in levees to sheets in thin-bedded basin floor fans.
  7. Evaluate variation in grain size and lateral continuity of sand bodies, understand why they can cause large variations in permeability, production rates and oil recovery.
  8. Relate characteristic of outcrops to analogous oil fields along the West African margin, Gulf of America/Mexico, southeast Asia and the Permian Basin
 

Geologic Carbon Storage at Outcrop: Lessons for Subsurface Characterization, Modeling, Risk and Monitoring, Utah (G579)

Tutor(s)

Alex Bump: Research Science Associate, University of Texas at Austin.

Michael Sweet: Co-Director and Research Scientist, University of Texas at Austin.

Overview

Using outcrops from the Cretaceous and Jurassic of Utah, this course will analyze some of the major subsurface challenges facing the storage of CO2 in subsurface formations, with particular reference to the planned Oligo-Miocene carbon stores on the Gulf Coast. It is intended to give participants the opportunity to consider the key factors of injectivity, capacity and confinement, and the range of storage play concepts available to match project needs with practically accessible storage sites. The course will explore the impact of multi-scale reservoir heterogeneity on migration and trapping of CO2, the propagation and dissipation of pressure, and the risks of unintended lateral or vertical migration of CO2 and/or displaced brine. We will also look specifically at boundary conditions and potential leakage paths, including faults and wells, using a variety of outcrops as a natural laboratory to facilitate the learning points.

Duration and Logistics

A 6-day field course comprising a mix of field activities with classroom lecture sessions and discussions. Transport will be by minivan or bus.

Level and Audience

Intermediate. This course is intended for geoscience and engineering professionals working in, or soon to transfer to, CCS projects.

Exertion Level

This class requires a MODERATE exertion level. There will be some short hikes to outcrops with some of these over uneven and rocky ground. The climate in southern Utah during the spring and fall is variable, with temperatures from 50°F (10°C) to 100°F (38°C). The elevation is between 4,000 and 5,000 feet (1200 and 1500 meters).

Objectives

You will learn to:

  1. Describe the subsurface requirements for a successful storage project, including similarities and differences with oil and gas exploration.
  2. Illustrate the CCS reservoir details of proposed Gulf Coast carbon stores and the state-of-play of these projects.
  3. Characterize the main depositional features that influence reservoir properties and CCS reservoir development, as well as likely performance, with special reference to clastic coastal/shallow marine depositional systems.
  4. Gauge fluid transport parameters, including the impact of geological heterogeneity and permeability on CO2 injection and plume migration.
  5. Evaluate sustainable injection rates for different carbon stores, including pressure propagation and interference, and factors such as loss of injectivity and pressure build-up.
  6. Manage containment risks with respect to both structural and depositional heterogeneities.
  7. Validate models for plume migration and integrate the key uncertainties.

Sand-rich and Confined Turbidite Systems: Annot, France (G048)

Tutor(s)

Mark Bentley: TRACS International Consultancy and Langdale Geoscience.

Overview

Experience the classic, well-exposed Grès d’Annot turbidite outcrop area in the French Alps, an excellent analogue for deepwater exploration and development targets in structurally active slope and basin settings. This course will provide insights into field development challenges in relatively confined, high-net, submarine fan systems by using the world-class exposures along with static/dynamic models of the outcrops to support discussions. Seismic forward-models of 3-D and 4-D responses to waterfloods in these systems add to the conversation. The setting allows reservoirs to be observed at a range of scales from seismic- and field-scale, to the scale of a core plug, and is intended for a cross-discipline, geoscience and petroleum engineering audience.

Duration and Logistics

A 7-day field course in the French Alps, comprising field activities and exercises on-site, unless weather doesn’t allow. The manual will be provided in paper format, with a digital copy available as a take-away.

Level and Audience

Advanced. The course is designed for integrated teams (geologists, geophysicists and reservoir engineers) evaluating development opportunities for fields in deepwater confined basins. The ideal group would be an asset team, who would be encouraged to bring their own field issues (and data where possible) to discuss live on the analogue.

Exertion Level

This class requires a DIFFICULT exertion level. The Grès d’Annot is quite comfortable in the early summer, with temperatures of 10–25°C (50–80°F) and occasional rain showers. Some field locations require path-based hillwalking involving ascents up to 600m (2000 feet). The longest excursion involves a full-day hike and will be conducted at a leisurely pace.

Objectives

You will learn to:

  1. Assess discrete, structurally controlled sediment transport pathways into bathymetrically complex deepwater basins.
  2. Assess the role of relative structural and flow confinement on turbidite reservoir architecture.
  3. Characterize internal reservoir architecture in different parts of the system and assess the impact of heterogeneities on fluid flow.
  4. Formulate reservoir and simulation modelling requirements, in order to forecast production performance from reservoirs of these types.
  5. Determine the level of detail required for reservoir characterization under a range of fluid fills and production mechanisms.
  6. Understand how much of the observed heterogeneity would be detectable on seismic, and predict how fluid-sensitive heterogeneities would be visible on 4-D seismic for a field on production.

Reservoir Characterization and Subsurface Uncertainties in Carbon Stores, Cheshire, UK (G578)

Tutor(s)

Richard Worden: Professor in the Department of Earth Ocean and Ecological Sciences, University of Liverpool, UK.

Overview

This course will give participants the opportunity to see some of the rocks at outcrop that are planned UK CO2 storage sites and to analyze the associated range of subsurface challenges. Visiting these outcrops will allow subsurface geoscientists, who generally use logs and limited core to build models, the opportunity to see the larger and smaller scale architecture and heterogeneity of the rocks they are working on and to consider the key processes of injectivity, migration and trapping of CO2. The course will also discuss post-depositional changes to sandstones, including petrophysical and geomechanical property evolution (pre- and post-CO2 injection), and some of the risks (migration and leakage) associated with developing saline aquifers and depleted gas fields as CO2 storage sites in these sandstones.

Duration and Logistics

A 5-day field course comprising a mix of field activities with classroom lectures and discussions. Transport will be by bus.

Exertion Level

This class requires an EASY exertion level. Field locations are mainly relatively easy walks of less than 1km (0.6 mile) along paths from road access points, although there is some walking down and up gentle slopes. One outcrop involves a 6km (3.7 miles) round trip walk over an intertidal sandflat.

Level and Audience

Intermediate. This course is intended for geoscience and engineering professionals working in CCS projects, especially those with an active interest in the Triassic Bunter/Sherwood Sandstones.

Objectives

You will learn to:

  1. Appraise the main depositional and diagenetic features that influence Triassic Sandstone (Bunter/Sherwood) reservoir properties and CCS reservoir development and likely performance.
  2. Validate the CO2 storage volumetrics from the micro (pore-scale) to the macro (aquifer volumes).
  3. Predict CO2 flow away from injector wells controlled by permeability and aquifer architecture with reference to injection rates and subsurface pressure.
  4. Assess the range of effects that CO2 can have on the host aquifer, from geomechanical to geochemical.
  5. Create plume migration models with respect to compartmentalization risk, pressure barriers, faults and fractures.
  6. Assess the role of top-seal and fault-seal properties and how they will influence CO2 storage, from risk of fracking, or induced seismicity, to mineral dissolution.

Building a Reservoir Model, Pembrokeshire, UK (G055)

Tutor(s)

Mark Bentley: TRACS International Consultancy and Langdale Geoscience.

Overview

This course offers a software-independent view on the process of reservoir model design and simulation model-building, addresses the underlying reasons why some models disappoint and offers solutions that support the building of more efficient, fit-for-purpose models. The thread through the week is a model design for the notional ‘Pembroke Field’ – a synthetic field constructed from reservoir analogue outcrops in South Pembrokeshire.  The Pembroke Field contains three contrasting reservoir types: continental clastics, shallow marine deltaics and naturally fractured carbonates, in both structurally deformed and undeformed settings. Data from producing oil and gas fields has been scaled to the synthetic models to create a realistic hydrocarbon field accumulation, ready for development.

Objectives

You will learn to:

  1. Create a fluid-sensitive conceptual model for a heterogeneous reservoir, built from a selection of elements and placed in a realistic architectural framework: the “sketch”.
  2. Guide the use of geostatistical tools intuitively, balancing deterministic and probabilistic components with awareness of the limits of the tools.
  3. Select appropriate methods for modeling of matrix properties, including the handling of net (cut-off’s vs total property modeling).
  4. Evaluate options for multi-scale modelling and the possible need for multi-scale approaches based on hierarchical understanding of Representative Elementary Volumes (REV).
  5. Understand issues surrounding permeability modeling and why this differs from the handling of other properties.
  6. Learn a rule of thumb (“Flora’s rule”) to help assess what level of static model detail matters to flow modeling and forecasting.
  7. Review how to use well test analysis to constrain models.
  8. Review options for model-based uncertainty handling (base case led, multi-deterministic scenarios, multi-stochastic ensembles), learn how to post-process the results and how to select an appropriate workflow which minimizes impact of behavioral bias.

Exertion Level

This class requires an EASY exertion level. Field stops require short walks along coastal paths, beaches and wave cut platforms. The longest walk is <5km (3 miles). Field stops are all at approximately sea level and some are tide dependent. Transport will be by coach.This class requires an EASY exertion level. Field stops require short walks along coastal paths, beaches and wave cut platforms. The longest walk is <5km (3 miles). Field stops are all at approximately sea level and some are tide dependent. Transport will be by coach.

Level and Audience

Intermediate. The course is aimed at geoscientists with knowledge of reservoir modeling software, petrophysicists who provide input to static reservoir models and reservoir engineers involved in simulation work who deal with the static-dynamic interface on a regular basis. The course is also of benefit to team leaders who wish to have a deeper understanding of the principles behind modeling and how to QC models made by others.

Duration and Logistics

7 days; a mix of field work (70%), and classroom exercises (30%).

Characterization, Modeling, Simulation and Development Planning in Deepwater Clastic Reservoirs, Tabernas, Spain (G076)

Tutor(s)

Mark Bentley: TRACS International Consultancy and Langdale Geoscience.

Overview

This course is led by a production geologist and reservoir engineer involved in deepwater reservoir development, and is presented as a practical reservoir discussion rather than purely a traditional geological field trip. The objective of this field course is to explore the reservoir modelling and petroleum engineering aspects of deepwater clastic reservoirs. The discussions highlight the linkage from depositional processes to geological architecture and flow heterogeneity in development planning. The Tabernas outcrops are very well exposed and offer examples of sand-rich and debris-flow-dominated reservoirs, high net:gross fan systems and classic mud-dominated facies. In particular, they give excellent insights into the reservoir heterogeneities occurring within apparently continuous ‘sand lobes’ and major channels.

Duration and Logistics

A 7-day field course based in Almeria, Spain, comprising a mix of field activities and exercises. Transport will be by SUV on paved roads and unpaved tracks.

Level and Audience

Advanced. The course is largely aimed at geologists and reservoir engineers working on deepwater developments. The course is best suited to multidisciplinary team of geologists, geophysicists, petrophysicists and reservoir engineers.

Exertion Level

This class requires a MODERATE exertion level. There will be multiple walks of up to 1km (0.5 mile) most days. The longest walk of the class is approximately 2km (1 mile), with an ascent (and descent) of 75m (245 ft). The field area is in Europe’s only desert region and participants should expect high temperatures and an arid working environment. Participants should also be prepared for sudden and heavy rain showers.

Objectives

You will learn to:

  1. Assess the genetic processes that produce slumps, slides, debrites and high/low density turbidites, and explain why the concept of confinement underpins the description of heterogeneity in deepwater clastic systems.
  2. Evaluate the extent to which pay is under-/over-estimated in mud-rich/sand-rich systems, respectively, and the resulting errors in STOIIP and PI estimation.
  3. Organise a detailed sedimentological description into key reservoir elements and build an architectural model using those elements.
  4. Assess the basic principle of flow in porous media (Darcy) and describe how flow heterogeneity varies in layered and amalgamated clastic systems.
  5. Appraise the contrasting heterogeneities in sand- and mud-rich systems and determine how much detail is required in a reservoir description based on a consideration of fluid type and production mechanism.
  6. Evaluate how kv/kh impacts recovery in typical deepwater clastic architectures; optimally locate a well to optimize sweep for a range of architectural cases.
  7. Judge length scale variations for a typical deepwater clastic system, and discuss how this would be handled in a reservoir modelling and simulation context.