The Lower Jurassic Johansen Formation, northern North Sea - Depositional model and reservoir characterization for CO₂ storage

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• 作者：Anja Sundal^a ; ^{anja.sundal@geo.uio.no" class="auth_mail" title="E-mail the corresponding author} ; Johan Petter Nystuen^a ; Kari-Lise Rø ; rvik^b ; ^{klr@gassnova.no" class="auth_mail" title="E-mail the corresponding author} ; Henning Dypvik^a ; Per Aagaard^a
• 关键词：Reservoir characterization ; Depositional model ; North Sea ; Jurassic ; Sandstone ; CO2 storage ; Sedimentology ; Geological heterogeneity ; Trapping mechanisms
• 刊名：Marine and Petroleum Geology
• 出版年：2016
• 出版时间：November 2016
• 年：2016
• 卷：77
• 期：Complete
• 页码：1376-1401
• 全文大小：11932 K

文摘

The Lower Jurassic, Johansen Formation sandstone, located in the Northern North Sea, has been proposed as a reservoir candidate for CO₂ storage by Norwegian authorities. The objective of this study is to evaluate the reservoir quality of the Johansen Formation, as function of depositional history and architecture.

We propose a depositional model comprising an early phase delta progradation, with clinothems building into deep waters, associated with delta front and pro-delta turbidites sourced from river mouths or/and upper delta front collapse. During a subsequent, aggradational stage, thick spit bar deposits developed in the southern, down-current part, sheltering a brackish lagoon, before rapid transgression caused back-stepping and preservation of sandy deposits encased in mud. Considering the depositional model presented, the inferred high porosity spit bar deposits would provide a suitable injection site and reservoir for CO₂.

Climatic controlling factors, rather than structural, are interpreted to have exerted the major force on the asymmetric sand distributions observed in the Johansen Formation, an architectural style which is repeated in later Jurassic successions on the Horda Platform. On a local scale, accommodation was created by differential compaction above rotated, Permian fault blocks, in addition to regional, post-thermal subsidence and rising sea-level.