Schlumberger
 
CyberGeologist
Studying Point Bars

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First the coarse grains are deposited near the base of the point bar and then the finer grains as the water flows towards the top of the point bar.


Ripples

Ripples on the surface of a modern point bar.

Underground Eyes

In addition to the arrangement of the layers, there are other signs geologists look for when building a picture of underground point bar formations.

One sign comes from sedimentary structures, such as dunes and ripples deposited on the surface as the point bar grows and preserved as distinctive features over time. These structures are aligned by the current flow in the river and have a distinct relationship to the point bar. Examining the orientation of the structures within wells provides clues geologists can use to determine the orientation of the entire point bar through which an oil well has been drilled.

In many parts of the world, oil and gas can be found trapped in sands that have been deposited as point bars millions of years ago.  In order to efficiently drain these reservoirs, geologists need to predict their location deep beneath the surface of the earth.

Diagonal layers of sediment
Cross-section of a modern point bar showing cross-bedding deposited by large ripples.
 

Another sign is in cross-sections of the point bar, where clearly defined layers are visible: finest particles, the silt and clay, on top and the larger particles, sand and tiny pebbles, on the bottom. This vertical sequence of grain sizes is another characteristic of point bars that enables geologists to recognize these formations in oil and gas wells.

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CyberGeologist
The Formation of Point Bars
Studying Point Bars
Evaluation Tools and Method
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