Ingrid Anell

• Anell, Ingrid; Indrevær, Kjetil & Serck, Christopher Sæbø (2022). Influence of structural highs on Triassic deposition on the western Barents Shelf. Geological Society Special Publication. ISSN 0305-8719. 495(1), s. 29–41. doi: 10.1144/SP495-2018-76.
• Faleide, Thea Sveva; Braathen, Alvar; Lecomte, Isabelle Christine & Anell, Ingrid (2022). Exploring seismic detection and resolution thresholds of fault zones and gas seeps in the shallow subsurface using seismic modelling. Marine and Petroleum Geology. ISSN 0264-8172. 143. doi: 10.1016/j.marpetgeo.2022.105776. Fulltekst i vitenarkiv
• Koehl, Jean-Baptiste Philippe; Magee, Craig & Anell, Ingrid (2022). Impact of Timanian thrust systems on the late Neoproterozoic–Phanerozoic tectonic evolution of the Barents Sea and Svalbard. Solid Earth (SE). ISSN 1869-9510. 13, s. 85–115. doi: 10.5194/se-13-85-2022. Fulltekst i vitenarkiv
• Würtzen, Camilla Louise; Osmond, Johnathon; Faleide, Jan Inge; Nystuen, Johan Petter; Anell, Ingrid & Midtkandal, Ivar (2021). Syn- to post-rift alluvial basin fill: seismic stratigraphic analysis of Permian-Triassic deposition in the Horda Platform, Norway. Basin Research. ISSN 0950-091X. doi: 10.1111/bre.12644.
• Anell, Ingrid Margareta; Zuchuat, Valentin; Röhnert, A.D.; Smyrak-Sikora, Aleksandra; Buckley, Simon John & Lord, Gareth Steven [Vis alle 12 forfattere av denne artikkelen] (2020). Tidal amplification and along‐strike process variability in a mixed‐energy paralic system prograding onto a low accommodation shelf, Edgeøya, Svalbard. Basin Research. ISSN 0950-091X. s. 1–35. doi: 10.1111/bre.12482. Fulltekst i vitenarkiv
• Smyrak-Sikora, Aleksandra; Osmundsen, Per Terje; Braathen, Alvar; Ogata, Kei; Anell, Ingrid Margareta & Mulrooney, Mark Joseph [Vis alle 7 forfattere av denne artikkelen] (2019). Architecture of growth basins in a tidally influenced, prodelta to delta-front setting: The Triassic succession of Kvalpynten, East Svalbard. Basin Research. ISSN 0950-091X. doi: 10.1111/bre.12410. Fulltekst i vitenarkiv
• Anell, Ingrid Margareta & Wallace, Malcolm W (2019). A fine balance: Accommodation dominated control of contemporaneous cool‐carbonate shelf‐edge clinoforms and tropical reef‐margin trajectories, North Carnarvon Basin, Northwestern Australia. Sedimentology. ISSN 0037-0746. 67, s. 96–117. doi: 10.1111/sed.12628.
• Midtkandal, Ivar; Faleide, Thea Sveva; Faleide, Jan Inge; Planke, Sverre; Anell, Ingrid Margareta & Nystuen, Johan Petter (2019). Nested intrashelf platform clinoforms—Evidence of shelf platform growth exemplified by Lower Cretaceous strata in the Barents Sea. Basin Research. ISSN 0950-091X. doi: 10.1111/bre.12377. Fulltekst i vitenarkiv
• Ogata, Kei; Mulrooney, Mark ; Braathen, Alvar; Maher, Harmon; Osmundsen, Per Terje & Anell, Ingrid Margareta [Vis alle 8 forfattere av denne artikkelen] (2018). Architecture, deformation style and petrophysical properties of growth fault systems: the Late Triassic deltaic succession of southern Edgeøya (East Svalbard). Basin Research. ISSN 0950-091X. 30(5), s. 1042–1073. doi: 10.1111/bre.12296. Fulltekst i vitenarkiv
• Anell, Ingrid Margareta & Midtkandal, Ivar (2017). The quantifiable clinothem – types, shapes and geometric relationships in the Plio-Pleistocene Giant Foresets Formation, Taranaki Basin, New Zealand. Basin Research. ISSN 0950-091X. 29, s. 277–297. doi: 10.1111/bre.12149.
• Ringdal, Kari; Buckley, Simon John; Lecomte, Isabelle; Anell, Ingrid Margareta & Braathen, Alvar (2016). From photorealistic outcrop models to synthetic seismic images. I Buckley, Simon John; Naumann, Nicole; Kurz, Tobias Herbert & Eide, Christian Haug (Red.), 2nd Virtual Geoscience Conference, Proceedings Volume. Uni Research AS. ISSN 978-82-8361-004-8.
• Anell, Ingrid Margareta; Lecomte, Isabelle; Braathen, Alvar & Buckley, Simon John (2016). Synthetic seismic illumination of small-scale growth faults, paralic deposits and low-angle clinoforms: A case study of the Triassic successions on Edgeøya, NW Barents Shelf. Marine and Petroleum Geology. ISSN 0264-8172. 77, s. 625–639. doi: 10.1016/j.marpetgeo.2016.07.005.
• Anell, Ingrid Margareta; Faleide, Jan Inge & Braathen, Alvar (2016). Regional tectono-sedimentary development of the highs and basins of the northwestern Barents Shelf. Norsk Geologisk Tidsskrift. ISSN 0029-196X. 96(1), s. 27–41. doi: 10.17850/njg96-1-04. Fulltekst i vitenarkiv
• Lecomte, Isabelle; Lubrano-Lavadera, Paul Louis Francois; Botter, Charlotte; Anell, Ingrid Margareta; Buckley, Simon John & Eide, Christian Haug [Vis alle 9 forfattere av denne artikkelen] (2016). 2(3)D convolution modelling of complex geological targets – beyond 1D convolution. First Break. ISSN 0263-5046. 34(5), s. 99–107.
• Lecomte, Isabelle; Lubrano-Lavadera, Paul Louis Francois; Anell, Ingrid Margareta; Buckley, Simon John; Schmid, Daniel Walter & Heeremans, Michel (2015). Ray-based seismic modeling of geologic models: Understanding and analyzing seismic images efficiently. Interpretation. ISSN 2324-8858. 3(4), s. SAC71–SAC89. doi: 10.1190/INT-2015-0061.1.
• Anell, Ingrid Margareta; Braathen, Alvar & Olaussen, Snorre (2014). The Triassic – Early Jurassic of the northern Barents Shelf: a regional understanding of the Longyearbyen CO2 reservoir. Norsk Geologisk Tidsskrift. ISSN 0029-196X. 94, s. 83–98. Fulltekst i vitenarkiv
• Anell, Ingrid Margareta; Midtkandal, Ivar & Braathen, Alvar (2014). Trajectory analysis and inferences on geometric relationships of an Early Triassic prograding clinoform succession on the northern Barents Shelf. Marine and Petroleum Geology. ISSN 0264-8172. 54, s. 167–179. doi: 10.1016/j.marpetgeo.2014.03.005.
• Anell, Ingrid Margareta; Braathen, Alvar & Olaussen, Snorre (2014). Regional constraints of the Sørkapp Basin: A Carboniferous relic or a Cretaceous depression? Marine and Petroleum Geology. ISSN 0264-8172. 54, s. 123–138. doi: 10.1016/j.marpetgeo.2014.02.023.
• Anell, Ingrid Margareta; Braathen, Alvar; Osmundsen, Per Terje & Olaussen, Snorre (2013). Evidence of faulting contradicting a Triassic quiescent northern Barents Shelf. First Break. ISSN 0263-5046. 31(6), s. 67–76. doi: 10.3997/1365-2397.2013017.
• Braathen, Alvar; Anell, Ingrid Margareta; Osmundsen, Per Terje & Olaussen, Snorre (2013). Just how quiescent was the northern Barents Shelf during the Triassic? First Break. ISSN 0263-5046. 31(9), s. 71–72.
• Anell, Ingrid Margareta; Braathen, Alvar; Senger, Kim & Osmundsen, Per Terje (2013). Evidence of faulting contradicts a quiescent northern Barents Shelf during the Triassic. First Break. ISSN 0263-5046. 31(6), s. 67–76. doi: 10.3997/1365-2397.2013017.
• Anell, Ingrid Margareta; Thybo, H. & Artemieva, I.M. (2009). Cenozoic uplift and subsidence in the North Atlantic region: Geological evidence revisited. Tectonophysics. ISSN 0040-1951. doi: 10.1016/j.tecto.2009.04.006.

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• Braathen, Catherine & Anell, Ingrid (2021). CCS at the OHG-conference - Key note lecture from Anell & Co.
• Machado Garcia, Aurora; Bellwald, Benjamin; Midtkandal, Ivar; Anell, Ingrid; Planke, Sverre & Sternai, Pietro [Vis alle 7 forfattere av denne artikkelen] (2021). Sedimentary Processes and Deposits of the Last Glaciation at the North Sea Fan, Offshore Norway. Vis sammendrag

  Understanding the sedimentary processes and resulting deposits along glaciated margins, that can be recorded in trough mouth fans (TMF), is crucial to increase knowledge about ice sheet dynamics. Their behavior influences Earth’s climate system and sea level variations, from regional to global scale, during relatively rapid timescales (up to millennia). This study uses high-quality 3D seismic reflection data of the uppermost North Sea Trough Mouth Fan to document the seismic stratigraphy, sedimentary processes and glacio-marine landforms shaped during the last glacial highstand (23-19 ka). The stratigraphy of the fan is characterized by thick (~400m) prograding sequences. Facies analyses and seismic geomorphology show three main depositional processes (contour-currents, gravity-driven flows and setting of plumes), mappable as seven seismic sub-units in the studied interval. Contour currents are responsible for the deposition of the lowermost two sub-units (U1 and U2), characterized by continuous reflections with increasing amplitude contrasts near the Tampen Slide escarpment. U1 is dominated by positive amplitudes with mostly tabular geometry. U2, identified in the northern part, is dominated by negative amplitudes with lenticular geometry and is synchronous with the glaciation onset. These sub-units are followed by a succession of relatively homogeneous facies interrupted by continuous high-frequency horizons that subdivide the succession into four sub-units (U3-6). These sub-units are characterized by channels, presumably generated by meltwater-fed turbidity flows, varying in width, varying in depth from 10 to 60m and with suggesting high-energy episodes that creates channels deeper than 100m. They are pervasive throughout the sequences and across the fan and are commonly isolated with low sinuosity. The uppermost sequence (U7) is dominated by deposition of the suspended load and ice-raft debris, characterized by parallel and slightly undulated continuous inner reflections, thinning out downslope. Along the shelf, multiple cross-cutting of iceberg scours and pits are observed. The succession with channels evidence that meltwater can play a major role in TMF sedimentation. These new insights about the smaller-scale processes within seismic resolution demonstrate the variability of active processes during a fast sedimentation period of the Weichselian Glaciation at the North Sea Trough Mouth Fan.

• Machado Garcia, Aurora; Midtkandal, Ivar; Bellwald, Benjamin & Anell, Ingrid Margareta (2021). A Source to Sink Approach to the North Sea Fan Pleistocene Glacial Sediments.
• Würtzen, Camilla Louise; Osmond, Johnathon L.; Faleide, Jan Inge; Nystuen, Johan Petter; Anell, Ingrid Margareta & Midtkandal, Ivar (2021). Syn- to post rift alluvial basin fill: seismic stratigraphic analysis of Permian-Triassic deposition in the Horda Platform.
• Faleide, Thea Sveva; Braathen, Alvar; Lecomte, Isabelle; Mulrooney, Mark Joseph; Anell, Ingrid Margareta & Midtkandal, Ivar [Vis alle 7 forfattere av denne artikkelen] (2020). Testing seismic interpretation of faults by modelling; viable geometries versus seismic resolution in the subsurface. EAGE extended abstracts. 2020. doi: 10.3997/2214-4609.202011930.
• Anell, Ingrid Margareta & Mulrooney, Mark Joseph (2020). Combatting Climate Change: An introduction to geological storage of CO2.
• Anell, Ingrid Margareta (2020). CO2 Storage Demonstration.
• Buckley, Simon John; Ringdal, Kari; Lecomte, Isabelle; Anell, Ingrid Margareta & Braathen, Alvar (2020). Virtual field trip to seismic scale outcrops of the Triassic, Edgeøya, Svalbard.
• Anell, Ingrid Margareta; Serck, Christopher Sæbø; Zuchuat, Valentin & Braathen, Alvar (2020). Structural influence on Triassic deposition on the Northern Barents Shelf.
• Faleide, Thea Sveva; Braathen, Alvar; Lecomte, Isabelle; Anell, Ingrid Margareta; Midtkandal, Ivar & Planke, Sverre (2020). Seismic modelling of faults; viable geometries vs seismic resolution in the subsurface. Vis sammendrag

  Resolution and illumination issues in seismic data curtails identification of fault geometries and fault-initiated rock damage when mapping subsurface faults. Seismic modelling can be utilized to bridge the gap in identifying what can be imaged with certainty in seismic data, with respect to the original geology, especially when also comparing to outcrop data. In this study, we explore how seismic modelling can distinguish between real structures versus seismic artefacts. 2(3)D Point-Spread-Function based convolution modelling is used in a sensitivity study. One input is detailed fault interpretations of high-resolution P-Cable data and comparable conventional 3D seismic data from the Hoop area in the Barents Sea. Another dataset comes from detailed fault geometries observed in outcrops, which were used to build geological models as input to the seismic modelling. In addition to the host-rock lithofacies, parameters of importance for the geological model building include overall fault geometry and the distribution of architectural elements (fault facies) within the fault zone. By varying fault input, lithofacies, a wide range of frequencies, and illumination, we analyse a variety of synthetic seismic images. Finally we compare our modelled outcomes with seismic data from the Hoop area. The scope of the workflow is to increase confidence in seismic interpretations and to identify limitations in the analysis of steep, normal faults in seismic data.

• Braathen, Catherine & Anell, Ingrid (2019). Successfull “Outside the BoCCS” seminar – The role of law in CCS deployment.
• Anell, Ingrid Margareta; Banet, Catherine; Weber, Viktor; Vold, Sofie Fogstad; Riseng, Cathrine & Seglem, Heidi [Vis alle 7 forfattere av denne artikkelen] (2019). The role of law in CCS deployment – Regulatory incentives to enable carbon capture and storage (CCS) in Norway.
• Anell, Ingrid Margareta; Backer, Dag; Sundal, Anja; Torvanger, Asbjørn; Meisingset, Egil & Rørvik, Kari-Lise [Vis alle 7 forfattere av denne artikkelen] (2019). Feasibility of CO2 storage as a climate mitigation measure in Norway.
• Faleide, Thea Sveva; Midtkandal, Ivar; Planke, Sverre; Corseri, Romain; Faleide, Jan Inge & Nystuen, Johan Petter [Vis alle 8 forfattere av denne artikkelen] (2019). High-resolution seismic imaging and modelling of structural and stratigraphical features in the SW Barents Sea. Vis sammendrag

  Poster at the AAPG 2019 conference, San Antonio, Texas, USA

• Anell, Ingrid Margareta (2019). NCCS – Education, mobility, student engagement and visions for the future.
• Buckley, Simon John; Ringdal, Kari; Dolva, Benjamin; Lecomte, Isabelle; Anell, Ingrid Margareta & Braathen, Alvar (2018). A virtual field trip to seismic-scale outcrops of the Triassic, Edgeøya, Svalbard. Vis sammendrag

  Large-scale cliff sections on Edgeøya, an island in the eastern part of the Svalbard Archipelago, comprise mostly Triassic sedimentary successions, and are onshore outcrops of formations found on the offshore Barents Shelf. These outcrops are of high interest for studying the subsurface geology found offshore on the Barents Shelf, using seismic-scale features such as small-scale growth faults, paralic deposits and low-angle clinoforms (Anell et al., 2016). At Kvalpynten, an outcrop at the southern end of Edgeøya, these features can be observed, providing the opportunity to compare offshore seismic data with the outcrop expression using seismic modelling. Synthetic seismic modelling provides a means of aiding interpretation of seismic data by quantitatively and qualitatively assessing resolution, scale and level of detail of modelled onshore structures (Lecomte et al., 2015). This can give valuable insights into potential resolution and survey parameter issues, as well as limitations with seismic data. Developments in digital outcrop modelling techniques, such as lidar and photogrammetry, now allow the accurate and high-resolution capture of large and inaccessible outcrop sections, at scales comparable with seismic vertical resolution. This opens up new possibilities for generating georeferenced input to synthetic seismic modelling, which allows generation of highly visual end products for educational purposes. This contribution presents a virtual field trip to the Triassic outcrops at Kvalpynten. The dataset is based on virtual outcrop models collected using boat-based photogrammetry, covering over 10km of continuous cliff sections. The 3D outcrop model is combined with geological interpretations, logs, field photos and information panels, as well as regional elevation data to set the context of the trip. In addition, synthetic seismic data are fused with the virtual outcrop models to highlight the scale of the exposures compared to offshore seismic data. The combined dataset is explored in LIME, a high performance viewer designed for displaying disparate geospatial and field datasets (http://virtualoutcrop.com/lime).

• Smyrak-Sikora, Aleksandra Anna; Osmundsen, Per Terje; Braathen, Alvar; Ogata, Kei; Anell, Ingrid Margareta & Husteli, Berit [Vis alle 8 forfattere av denne artikkelen] (2017). Sedimentary architecture of siliciclastic, syntectonic graben and halfgraben fill in Kvalpynten, Edgeøya, Svalbard. Vis sammendrag

  An array of ten grabens/ half-grabens and their associated syntectonic basin fill (averaging approx. 700 m across) are exposed along a 9 km cliff section at Kvalpynten, Edgeøya, offering a unique opportunity to study the silisiclastic architecture of listric graben basin fill. The exposures at Kvalpynten provide a unique opportunity to correlate fault-controlled sedimentary architecture on the scale of meters to hundreds of meters with detailed facies relationships, and thus fault-induced differential accommodation with the depositional environments that filled it. The basins developed in the Late Triassic, during the deposition of the Early Carnian to Early Norian deltaic successions of Tchermakfjellet and De Geerdalen formations which is approximately the onshore equivalent to the offshore Snadd Formation. The lowermost part of the ca 400 m high Kvalpynten cliff section reveals a number of NW–SE striking growth faults with 50–100 m offset, which bound basins filled with shale and sandstone wedges. Up section, the growth faults tip out, and are buried by undeformed deltaic deposits. Integrated field studies including sedimentology and structural geology combined with surfaces mapping on a photogrammetric virtual outcrop model allowed incremental reconstruction of the grabens/ half-grabens evolution. Four transgressive surfaces were identified and mapped, allowing correlation of the sandstone packages between each basin. The sequence of faulting has been defined with respect to the mapped flooding surfaces. Faulting clearly occurred in several phases as evident by the syn-kinematic fault’s control on sediments of different ages, and from the occurrence of later forming faults rotating earlier formed fault blocks. In general, early faults defined a relatively symmetrical basin configuration whereas later phases of movement were localized mainly along south-dipping faults. This gave rise to a change to more asymmetric basins and to the formation of asymmetric, composite sedimentary bodies with stacked shoreface and offshore transition deposits. Locally, fault crests were eroded. Our sedimentological observations suggest that tidal processes were dominant during sandstone deposition within the grabens/half-grabens, expressed by the widespread occurrence of tidal bar and tidal flat deposits.

• Buckley, Simon John; Ringdal, Kari; Dolva, Benjamin; Lecomte, Isabelle; Eide, Christian Haug & Anell, Ingrid Margareta [Vis alle 7 forfattere av denne artikkelen] (2017). Digital outcrop modelling results and workflows for derived synthetic seismic imaging.
• Ogata, Kei; Mulrooney, Mark; Braathen, Alvar; Maher, Harmon; Smyrak-Sikora, Aleksandra Anna & Anell, Ingrid Margareta [Vis alle 12 forfattere av denne artikkelen] (2017). Architecture, deformation style and petrophysical properties of a Late Triassic growth fault system in southern Edgeøya, East Svalbard.
• Anell, Ingrid Margareta; Braathen, Alvar; Røhnert, Daniela; Ogata, Kei; Osmundsen, Per Terje & Smyrak-Sikora, Aleksandra Anna [Vis alle 10 forfattere av denne artikkelen] (2017). Findings of five field foragings. Sandbody distribution, clinoform geometries and depositional environments of Edgeøya, Svalbard.
• Braathen, Alvar; Mulrooney, Mark; Haile, Beyene Girma; Appleyard, Tyler Ross; van Yperen, Anna Elisabeth & Smyrak-Sikora, Aleksandra Anna [Vis alle 12 forfattere av denne artikkelen] (2017). “Delta collapse” – Edgeøya delta system compared to the Ferron delta (Utah) .
• Anell, Ingrid Margareta; Lecomte, Isabelle; Braathen, Alvar & Buckley, Simon John (2016). Synthetic seismic expression of the onshore Kvalpynten case study: Growth-faults. Low-angle prograding deltaic system.
• Ogata, Kei; Mulrooney, Mark; Braathen, Alvar; Maher, Harmon; Smyrak-Sikora, Aleksandra Anna & Anell, Ingrid Margareta [Vis alle 12 forfattere av denne artikkelen] (2016). Field-based characterisation and analogue modelling of the South Edgeøya growth faults systems.
• Eide, Christian Haug; Klausen, Tore Grane; Anell, Ingrid Margareta; Suslova, Anna; Katov, Denis & Helland-Hansen, William (2016). Source-to-sink and mass-balance of the entire Triassic Barents Sea - Ideas, Plans and preliminary results.
• Buckley, Simon John; Ringdal, Kari; Lecomte, Isabelle; Anell, Ingrid Margareta; Braathen, Alvar & Eide, Christian Haug (2016). Virtual outcrops to synthetic seismic modelling.
• Anell, Ingrid Margareta; Braathen, Alvar & Faleide, Jan Inge (2015). Hidden below – Paleo-highs and deep structural influence on sedimentation on the Northern Barents Shelf.
• Buckley, Simon John; Dolva, Benjamin; Braathen, Alvar; Anell, Ingrid Margareta; Mulrooney, Mark & Lecomte, Isabelle (2015). State of-the-art of digital outcrop mapping methods: application to the Triassic of Edgeøya, Svalbard.
• Osmundsen, Per Terje; Smyrak-Sikora, Aleksandra Anna; Braathen, Alvar; Olaussen, Snorre; Ogata, Kei & Anell, Ingrid Margareta (2015). Growth basins at Edgeøya: sedimentary architecture and facies relationships.
• Lecomte, Isabelle; Buckley, Simon John & Anell, Ingrid Margareta (2015). Seismic modelling: Edgeøya and other illustration cases.
• Anell, Ingrid Margareta; Braathen, Alvar & Faleide, Jan Inge (2015). Shifting stress regimes and deep structural control on Triassic sedimentation.
• Anell, Ingrid Margareta & Midtkandal, Ivar (2015). Quantifiable clinothems and missing clinoforms : How studies down under can help our understanding of the Triassic of the Barents Shelf.
• Osmundsen, Per Terje; Smyrak-Sikora, Aleksandra Anna; Braathen, Alvar; Olaussen, Snorre; Ogata, Kei & Anell, Ingrid Margareta (2015). Sedimentary architecture and facies distribution in Late Triassic, reservoir-scale half-graben, De Geerdalen Formation, East Svalbard.
• Anell, Ingrid Margareta (2015). Edgeøya - en saga i sten. Geologiskt forum : Geologiska Föreningens populärvetenskapliga tidskrift. ISSN 1104-4721. 22(87), s. 23–27.
• Braathen, Alvar; Anell, Ingrid Margareta; Smyrak-Sikora, Aleksandra Anna; Mulrooney, Mark; Haile, Beyene Girma & Ogata, Kei [Vis alle 11 forfattere av denne artikkelen] (2015). Tectonic influence on platform infill patterns in the mid-late Triassic, Southern Edgeøya, Svalbard.
• Smyrak-Sikora, Aleksandra Anna; Osmundsen, Per Terje; Braathen, Alvar; Ogata, Kei; Anell, Ingrid Margareta & Husteli, Berit [Vis alle 7 forfattere av denne artikkelen] (2015). Depositional setting and internal architecture of syn-tectonic, siliciclastic half-graben fill, Edgeøya, Svalbard.
• Braathen, Alvar; Mulrooney, Mark; Ogata, Kei; Anell, Ingrid Margareta; Smyrak-Sikora, Aleksandra Anna & Lecomte, Isabelle [Vis alle 8 forfattere av denne artikkelen] (2015). Trias North: Late Triassic shallow faulting in Edgeøya, Svalbard; structural style, deformation mechanisms and seismic expression.
• Anell, Ingrid Margareta; Braathen, Alvar; Faleide, Jan Inge & Olaussen, Snorre (2015). Bridging the gaps of our understanding of the Triassic of the northern Barents Shelf.
• Anell, Ingrid Margareta; Braathen, Alvar; Midtkandal, Ivar; Smyrak-Sikora, Aleksandra Anna; Husteli, Berit & Ogata, Kei [Vis alle 7 forfattere av denne artikkelen] (2015). Tracking the Triassic platform-edge: Inferences on onshore clinoform geometries upon reaching the Edgeøya platform.
• Anell, Ingrid Margareta (2014). The Regional Triassic Puzzle - Origins of the Longyearbyen CO2 reservoir.
• Ogata, Kei; Anell, Ingrid Margareta; Braathen, Alvar; Osmundsen, Per Terje; Smyrak-Sikora, Aleksandra Anna & Husteli, Berit [Vis alle 8 forfattere av denne artikkelen] (2014). Syndepositional faulting in the Late Triassic succession of Kvalpynten, Edgeøya, East Svalbard.
• Anell, Ingrid Margareta; Midtkandal, Ivar & Braathen, Alvar (2013). A detailed trajectory analysis and some new inferences on geometrical relationships in an Early Triassic prograding clinoform succession on the northern Barents Shelf.
• Braathen, Alvar; Anell, Ingrid Margareta; Osmundsen, Per Terje & Olaussen, Snorre (2013). Exploring the Triassic of the Northern Barents Shelf – Sag-basins Interacting with Growth-faults.
• Anell, Ingrid Margareta; Braathen, Alvar & Olaussen, Snorre (2013). Tracking the Triassic – early results of linking the Longyearbyen CO2 reservoir across the northern Barents Shelf.
• Olaussen, Snorre; Braathen, Alvar; Anell, Ingrid Margareta; Johansen, Harald; Johansen, I & Larsen, Leif [Vis alle 13 forfattere av denne artikkelen] (2013). You learn so long as you drill: some unexpected results from the UNIS CO2Lab drilling and testing venture in Adventdalen, Svalbard.
• Olaussen, Snorre; Anell, Ingrid; Braathen, Alvar; Larsen, Leif; Mørk, Mai Britt Engeness & Ogata, Kei [Vis alle 7 forfattere av denne artikkelen] (2012). Fluid flow test of a tight fractured and under-pressured reservoir unit, a case study from Longyearbyen CO2 drilling and test site, Adventdalen, Svalbard. NGF abstracts and proceedings. 2012(3), s. 39–42.
• Anell, Ingrid Margareta; Braathen, Alvar; Husteli, Berit; Larsen, Leif; Ogata, Kei & Olaussen, Snorre [Vis alle 7 forfattere av denne artikkelen] (2012). State of the art fluid flow tests of tight fractured and under-pressured sandstone unit – De-risking of the potential CO2 storage unit in Adventdalen, Svalbard.
• Olaussen, Snorre; Anell, Ingrid Margareta; Braathen, Alvar; Larsen, Leif; Mørk, Mai Britt Engeness & Ogata, Kei [Vis alle 7 forfattere av denne artikkelen] (2012). Fluid flow test of a tight fractured and under-pressured reservoir unit, a case study from Longyearbyen CO2 drilling and test site, Adventdalen, Svalbard.
• Harris, Sharon; Anell, Ingrid Margareta; Sundal, Anja; Braathen, Alvar & Faleide, J I (2019). The tectono-sedimentary development of Smeaheia on the Horda Platform with a focus on the Cretaceous, and implications for CO2 storage. UIO.

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