Oil and Gas

Oil and Gas | Basin Analysis

Reservoir Analogues for the Southwestern Barents Sea: Outcrop Examples from Svalbard (Norway)

Course Code: N298
Instructors:  Andy Thurlow
Course Outline:  Download
Format and Duration:
6 days

Summary

The focus of this course is an outcrop examination of a variety of depositional systems including the Carboniferous/Permian marine-carbonate succession and Mesozoic shallow-marine, deltaic and continental successions. Focus will be placed on the facies architecture and stratigraphy with application to coeval reservoir rocks and petroleum systems of the southwestern Barents Sea. Observations and analyses will be placed in a context of subsurface data from core, wireline logs and seismic profiles.

Business impact: The geology of Svalbard is especially suitable as a reference for the geology of the Norwegian Barents Sea and also serves as an analogue for sequence stratigraphic concepts applicable to the Norwegian Continental Shelf. Svalbard offers world-class outcrops, enabling reservoir study from pore- to seismic-scale, as well as the examination of play concepts and the integral role of sequence stratigraphic relationships.

Feedback

The one thing I wanted out of this course is how Svalbard outcrops and stratigraphy related to other parts of the Barents Sea, to get a regional picture. This was done very well and clearly. Greatly enhanced my knowledge of the regional geology of the area.

Duration and Training Method

A field course with days spent ashore and evening lectures and discussion sessions onboard the ship.

Course Overview

Participants will learn to:

  1. Illustrate the broad tectonic setting and evolution of the SW Barents Sea region.
  2. Characterise a wide range of carbonate and clastic depositional processes and products and their recognition in the subsurface.
  3. Validate facies distributions with respect to regional correlations.
  4. Assess the large-scale controls with particular emphasis on high-resolution sequence stratigraphy on basin floor, slope and associated deltaic systems.
  5. Characterise regional petroleum systems in terms of spatial distribution of reservoir development, the nature of permeability baffles and barriers, seal, trap and source rock distribution.
  6. Evaluate regional scale links and make well constrained predictions of reservoir presence and potential quality.
  7. Predict regional basin infill depositional elements and the implications for reservoir modelling, as well as exploration and development risks.

The field-based component will investigate a variety of carbonate and clastic depositional systems ranging in age from Carboniferous-Tertiary. Attendees will examine superbly-exposed, often seismic-scale sequences from a variety of basins and explore the contrasting reservoir components that are developed within different tectonic and climatic regimes. Comparison with subsurface examples from the North Sea, Barents Sea, and other Arctic Basins will be made throughout the course. Stratal relationships will be analysed in the field at vertical scales of tens of metres and horizontal scales of kilometres. All observations and analyses will be placed in a context of subsurface data from core, wireline log and seismic profiles. Participants will be able carry out field analysis of a wide variety of carbonate and clastic systems and use data to determine patterns of relative sea level change and correlate between successions.

Course themes:

1. Middle Carboniferous continental and shallow marine successions denote the onset of major rifting forming north-south orientated rift-basins across Central Svalbard. The post-rift transition into the Permian is characterised by a variety of shallow marine carbonates. Such carbonates may have reservoir potential.

2. Triassic sequences are dominantly of shallow marine and shelfal origin and notably preserve shales with high organic content (Botnheia Formation) that may prove to be a prolific source rock in the Barents Sea. Major uplift in the Late Triassic led to incision and continental-shallow marine deposition extending into the Early Jurassic. Reservoir units in the Tromsø and Hammerfest Basins of the SW Barents region are are of similar paralic to shallow marine origin (Havert, Klappmyss, Kobbe, Snadd, Fruholmen, Tubåen, Nordmela and Stø Formations).

3. Middle-Jurassic to Early Cretaceous deposits were formed in response to marine transgression across Svalbard with further deposition of high TOC shales as well as a variety of shallow marine and deltaic units. Petroleum systems related to the Late Jurassic (Hekkingen) source rock are considered dominant in the SW Barents Sea. Uplift in the Early Cretaceous is marked by a regional unconformity with fluvial deposits overlying shelfal mudstones. Adventdalen Group successions are considered analogous to Brent Group units in the North Sea.

Approximate Itinerary (dependent on weather, sea conditions and polar bears):

Arrival into Longyearbyen based on flight availability.

Day 1: Ship departure

  • Transfer to ship for afternoon departure.

Days 2-6:

  • Localities in Van Keulenfjorden, Van Mijenfjorden, and the inner Isfjorden area.
  • Return to Longyearbyen harbour on the evening of day 6.
  • Overnight onboard.

Day 7: Departure and return home

The course is designed not only for exploration and development geologists working the Barents Sea and Arctic regions, but is also relevant to all subsurface geoscientists who wish to broaden and deepen their knowledge of carbonate and clastic plays. Tuition will provide a broad working knowledge of these systems for graduate and inexperienced staff, while providing further insights to experienced workers.

Andy Thurlow

Background
Andrew is an experienced reservoir geologist with a proficient background in both clastics and carbonates. His postgraduate research focussed on sequence stratigraphic controls on the interplay of shallow marine carbonates and clastics in the Lower Carboniferous of NW England. Following this, he worked as a reservoir geologist with Ichron for 19 years, principally on clastic projects from around the world and throughout the stratigraphic column. Since 2006 Andrew has largely focussed on the regional geology of the Norwegian Barents Sea and has been pivotal in the delivery of numerous multi-client and proprietary technical reports in this area. One benefit of the longevity of this period is that it has enabled him to gain a level of experience rarely matched in the stratigraphy and reservoir geology of the exploration well database in this high profile area. Andrew left Ichron at the end of 2014 to pursue an independent role. His current project work is as a consultant in client offices within multi-disciplinary teams tasked with the preparation of application documents for licencing rounds and play fairway analysis for production licences.

Affiliations and Accreditation
PhD The University of Manchester - Sedimentology
BSc University of Durham - Geology

Courses Taught
N298: Reservoir Analogues for the Southwestern Barents Sea: Outcrop Examples from Svalbard (Norway)

CEU: 4.8 Continuing Education Units
PDH: 48 Professional Development Hours
Certificate: Certificate Issued Upon Completion
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