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North Sea Oil - How did it get here?

It may seem surprising that the Oil industry has waited until recently to explore the coast of the British Isles for any oil or gas deposits. A shallow water area such as the North Sea would almost certainly yield some Oil or Gas and it had been a matter of conjecture for some years that oil and gas deposits could be found and exploited. In the mid 1960s real efforts were made to explore the Southern part of the North Sea and in 1965 hydrocarbons were found. A brief history of this exciting time can be found at The History page.

The North West European Geological garden which has been dug over hundreds of millions of years by erosion, deposition, uplifting and then more erosion. At the present time the North Sea is part of the depositional basin collecting the debris brought down by large European rivers. In times past this sea stretched halfway across Britain and Holland whilst at other times the North Sea was itself land.

About 250 million years ago the sea area which was collecting sediment stretched right across the UK Midlands, through the North Sea's present location and far into Holland and Germany.

Although the exact process is complex it was possible for geologists to predict with a reasonable amount of certainty where sedimentary oil-bearing rock was likely to have been laid down at this period.

Most of the large oil-producing areas of the world are in the tropics. Considering first these oil fields contained in recently deposited rocks - say thirty million years old - they are found to lie in the tropical belt. It is only the oil found in the older rocks that is in the higher Northern or Southern latitudes. This observation leads to the assumption that petroleum is not only associated with marine sedimentary rocks, but also with those rocks that were deposited in tropical climates.

So why are we finding oil at these latitudes? The answer is that the continents have moved around in the past hundred million years.    

Some rocks, particularly those with iron in them are magnetised in a certain direction and in many case this is not the same as direction the rocks would be magnetized if it was formed today. By measuring these magnetic anomalies it is possible to make a guess at what latitude the particular rocks were first formed. For example by looking at the magnetism direction of certain rocks in the Dogger Bank we can be reasonably certain that it was situated in the tropics, indeed on the equator, from 250 - 270 million years ago or during the Permian period and Upper Carboniferous period.

 As oil is formed in warm conditions in marine sediments all the geologists need to look for are sedimentary rocks which formed around the Permian period or the Carboniferous Period, which in the case of the North Sea Basin is around the 8000 - 11000 feet level. Any oil will be concentrated in reservoirs at the top of an anticline and held by a Caprock (a layer of rock which is impervious to oil or gas).

In the North Sea the sedimentary basin is 221,000 square miles and there are numerous humps and plugs that are so important to the oil explorer. Evidence from the study of rocks that are similar to those beneath the North Sea suggests a warm depositional environment for rocks more than 150 million years old. Porous rocks such as Carboniferous limestone or the sands of the Coal measures is almost certainly present. There are also adequate impervious rocks which form the Caprock.  

Supplying the Oil Platforms can be particularly hazardous. Here a Supply Vessel rides out the kind of storm which are commonplace in the seas around the latitudes of the British Isles.

The maps on the left show part of the total extent of the British North Sea operations in greater detail.

 

 

East of Shetland

East of Orkney

East of Orkney

East of Aberdeen

East of Aberdeen

Southern Sector Gas Fields

Southern Sector Gas Fields