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FAULT BLOCK [4 records]

Record 1 2011-01-06

English

Subject field(s)
  • Tectonics
DEF

A structure formed when the crust is divided into blocks of different elevation by a set of normal fault.

OBS

block fault: term used at Natural Resources Canada - Earth Sciences Sector.

French

Domaine(s)
  • Tectonique
Key term(s)
  • faille en blocs

Spanish

Save record 1

Record 2 2009-03-13

English

Subject field(s)
  • Geomorphology and Geomorphogeny
  • Tectonics
DEF

A fault block that has become tilted.

CONT

structural trap: The structural enclose of a porous unit by folding (e.g., anticline trap) or faulting (e.g., tilted fault block).

CONT

The Teton Range in Wyoming is an example of a tilted-fault block, a range of scenic beauty and rugged relief.

OBS

tilted fault block: term used at Natural Resources Canada - Earth Sciences Sector.

French

Domaine(s)
  • Géomorphologie et géomorphogénie
  • Tectonique
CONT

Le delta du Mackenzie et le centre de la mer de Beaufort recouvrent un régime d'expansion de failles listriques et de blocs faillés inclinés qui y sont reliés lequel régime est typiquement représenté dans la zone faillée Tarsiut-Amauligak.

OBS

bloc-faille incliné : terme en usage à Ressources naturelles Canada - Secteur des sciences de la Terre.

Spanish

Save record 2

Record 3 2009-01-22

English

Subject field(s)
  • Tectonics
DEF

A crustal unit formed by block faulting.

OBS

[This unit] is bounded by faults, either completely or in part. It behaves as a unit during block faulting and tectonic activity.

OBS

fault block: term used at Natural Resources Canada - Earth Sciences Sector.

French

Domaine(s)
  • Tectonique
CONT

Un bloc faillé, relativement soulevé entre deux failles bordières, est un Horst.

OBS

bloc faillé : terme en usage à Ressources naturelles Canada - Secteur des sciences de la Terre.

Spanish

Save record 3

Record 4 1999-11-03

English

Subject field(s)
  • Geomorphology and Geomorphogeny
DEF

A depression separated from the surrounding area by faults.

French

Domaine(s)
  • Géomorphologie et géomorphogénie
CONT

En structure massive faillée, les rivières suivent les bassins d'effondrement (Auvergne, Pyrénées orientales) ou les lignes de failles (Vosges).

Spanish

Save record 4

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