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Regional Occurrence of Large-Scale Sand Injectites in the North Sea: Event Stratigraphy and Implications for Hydrocarbon Exploration

Huuse, Mads 1; Jackson, Christopher 2; Cartwright, Joe 3; Hurst, Andrew 1
1 Geology and Petroleum Geology, University of Aberdeen, Aberdeen, United Kingdom.
2 Imperial College, London, United Kingdom.
3 Cardiff University, Cardiff, United Kingdom.

Large-scale sandstone intrusions are common in deepwater depositional systems, with excellent outcrop examples in California, Patagonia, France, Antarctica, Sakhalin and Greenland. The largest subsurface examples constitute entire oil fields, particularly common in the Paleogene of the central and northern North Sea. Recent studies have documented their occurrence in the North Sea from the Upper Cretaceous to the Neogene from the Norwegian-Danish Basin through the northern Central Graben, the Outer Moray Firth, the South Viking Graben, to the North Viking Graben, and in the Faroe-Shetland Basin.

This paper reviews the tectono-stratigraphy of large-scale sandstone intrusions, and their implications for hydrocarbon systems in the North Sea. The origin of the intrusions in the North Sea and in many basins worldwide remains largely unconstrained. In particular, the 1) timing, 2) sand and fluid source, 3) source of overpressure, 4) role of hydrocarbons, and 5) triggering mechanisms remain unresolved. Proposed mechanisms and drivers include liquefaction by earthquakes or meteorite impacts, diagenetic and hydrocarbon fluids, disequilibrium compaction, lateral transfer of pressure. In terms of hydrocarbon exploration, large-scale intrusions are important reservoirs with intricate geometries usually characterised by excellent intra- and inter-reservoir connectivity. Some intrusions may act as long-term fluid conduits and may thus be implicated in hydrocarbon migration and act as long-term fluid conduits (valves), increasing cross-stratal fluid flow over hundreds of metres of section, assisting pressure bleed off and compaction. In other areas, sandstone intrusions may act as fluid sinks when penetrated during drilling. Sandstone intrusions may connect isolated reservoir bodies over tens of kilometres laterally and over several hundreds of metres vertically. The sizes of individual completely injected sandbodies range up to 0.5-1 km3 in volume. Only a few such large-scale intrusions have been targeted deliberately, but several have been drilled before their true origin were realized, causing much confusion in the initial appraisal and production of oil in these bodies. Intrusions associated with in situ remobilized sandbodies are extremely common in the North Sea Paleogene and currently constitute important infill drilling targets on the Gryphon and Alba Fields and several smaller oil fields in the North Sea whilst frontier examples include deepwater West Africa.


AAPG Search and Discovery Article #90090©2009 AAPG Annual Convention and Exhibition, Denver, Colorado, June 7-10, 2009