Graben

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Diagram illustrating the structural relationship between grabens and horsts
Infrared-enhanced satellite image of a graben in the Afar Depression

In geology, a graben (Template:IPAc-en) is a depressed block of the crust of a planet or moon, bordered by parallel normal faults.

Etymology

Graben is a loan word from German, meaning 'ditch' or 'trench', up to large valley like Upper Rhine Graben. The first known usage of the word in the geologic context was by Eduard Suess in 1883.<ref>Template:Oed</ref> The plural form, in German, is "Gräben", in English either graben<ref>Schlumberger Oilfield Glossary</ref> or grabens.<ref name = "horst-and-graben">Template:Cite encyclopedia</ref>

Formation

Template:Unreferenced section A graben is a valley with a distinct escarpment on each side caused by the displacement of a block of land downward. Graben often occur side by side with horsts. Horst and graben structures indicate tensional forces and crustal stretching.

Graben are produced by sets of normal faults that have parallel fault traces, where the displacement of the hanging wall is downward, while that of the footwall is upward. The faults typically dip toward the center of the graben from both sides. Horsts are parallel blocks that remain between graben; the bounding faults of a horst typically dip away from the center line of the horst. Single or multiple graben can produce a rift valley.

Half-graben

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The Newark Basin, an early Mesozoic half-graben

In many rifts, the graben are asymmetric, with a major fault along only one of the boundaries, and these are known as half-graben. The polarity (throw direction) of the main bounding faults typically alternates along the length of the rift. The asymmetry of a half-graben strongly affects syntectonic deposition. Comparatively little sediment enters the half-graben across the main bounding fault because of footwall uplift on the drainage systems. The exception is at any major offset in the bounding fault, where a relay ramp may provide an important sediment input point. Most of the sediment will enter the half-graben down the unfaulted hanging wall side (e.g., Lake Baikal).<ref>Template:Cite journal</ref>

Rima Ariadaeus on the Moon is thought to be a graben. The lack of erosion on the Moon makes its structure with two parallel faults and the sunken block in between particularly obvious.

Examples

Africa

Antarctica

Asia

Europe

North America

Canada

Guatemala

United States

Multi-national

Oceania

South America

See also

Notes

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References

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