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Pernambuco Fault, the Glossary

Index Pernambuco Fault

The Pernambuco Fault or Pernambuco Shear Zone in northeastern Brazil is a fault radiating from the Trans Brazilian Lineament eastwards to the coast, a major geological feature.[1]

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Table of Contents

  1. 8 relations: Africa, Brazil, Cameroon, Central African Shear Zone, Fault (geology), Foumban Shear Zone, South America, Trans Brazilian Lineament.

  2. Geology of Brazil
  3. Seismic faults of Brazil

Africa

Africa is the world's second-largest and second-most populous continent after Asia.

See Pernambuco Fault and Africa

Brazil

Brazil, officially the Federative Republic of Brazil, is the largest and easternmost country in South America and Latin America.

See Pernambuco Fault and Brazil

Cameroon

Cameroon, officially the Republic of Cameroon, is a country in Central Africa.

See Pernambuco Fault and Cameroon

Central African Shear Zone

The Central African Shear Zone (CASZ) (or Shear System) is a wrench fault system extending in an ENE direction from the Gulf of Guinea through Cameroon into Sudan.

See Pernambuco Fault and Central African Shear Zone

Fault (geology)

In geology, a fault is a planar fracture or discontinuity in a volume of rock across which there has been significant displacement as a result of rock-mass movements.

See Pernambuco Fault and Fault (geology)

Foumban Shear Zone

The Foumban Shear Zone, or Central Cameroon Shear Zone (CCSZ), is a fault zone in Cameroon that has been correlated with the Pernambuco fault in northeastern Brazil, which splays from the Trans-Brazilian Lineament. Pernambuco Fault and Foumban Shear Zone are Palaeogeography stubs.

See Pernambuco Fault and Foumban Shear Zone

South America

South America is a continent entirely in the Western Hemisphere and mostly in the Southern Hemisphere, with a considerably smaller portion in the Northern Hemisphere.

See Pernambuco Fault and South America

Trans Brazilian Lineament

The Trans Brazilian Lineament (TBL), or Transbrasiliano Lineament, is a major shear zone that developed in the Precambrian period, and that has been reactivated several times since then, mostly recently during the Mesozoic. Pernambuco Fault and Trans Brazilian Lineament are Seismic faults of Brazil.

See Pernambuco Fault and Trans Brazilian Lineament

See also

Geology of Brazil

Seismic faults of Brazil

References

[1] https://en.wikipedia.org/wiki/Pernambuco_Fault