1. https://terra-vocabulary.org/ncl
  2. DataTerraRepositoryFairIncubator
  3. motsClefs
  4. _c_89f33bb7
experimental

Entrée : Faille

URI: https://terra-vocabulary.org/ncl/DataTerraRepositoryFairIncubator/motsClefs/c_89f33bb7

Fracture ou zone de rupture dans le sol, le long de laquelle les blocs rocheux se déplacent l’un par rapport à l’autre

Métadonnées principales

est un Concept | feature of interest
modifié le 18 Sep 2024 09:58:26.150
soumis parHélène Bressan
accepté le 20 May 2022 09:42:08.331

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date accepted 20 May 2022 09:42:08.331
date submitted 20 May 2022 09:41:39.041
definition
entity Faille
source graph graph

description
fr Fracture ou zone de rupture dans le sol, le long de laquelle les blocs rocheux se déplacent l’un par rapport à l’autre
en A fracture along which the blocks of crust on either side have moved relative to one another parallel to the fracture.
en A fracture or fracture zone in the Earth along which the two sides have been displaced relative to one another parallel to the fracture. The accumulated displacement across a fault may range from a fraction of a meter to many tens or hundreds of kilometers. The type of fault is specified according to the orientation and sense of slip and the inclination (dip) of the fault plane (Aki and Richards, 1980; Yeats et al., 1997). If the block opposite an observer looking across the fault moves to the right, the slip style is termed right lateral (dextral), if the block moves to the left, the motion is termed left lateral (sinistral). Dip-slip faults are inclined fractures along which rock masses have mostly shifted vertically. If the rock mass above an inclined fault moves down (due to lateral extension) the fault is termed normal, whereas if the rock above the fault moves up (due to lateral compression), the fault is termed reverse (or thrust). Oblique-slip faults have significant compon...
en Fracture or fracture zone in the ground, along which the two rocky blocks move relative to each other.
item class Concept | feature of interest
label
fr Faille
en Fault
modified 18 Sep 2024 09:58:26.150
notation c_89f33bb7
register mots clefs
status status experimental
submitter
account name h.bressan@brgm.fr
name Hélène Bressan

type register item
version info 8
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Définition

description
fr Fracture ou zone de rupture dans le sol, le long de laquelle les blocs rocheux se déplacent l’un par rapport à l’autre
en A fracture or fracture zone in the Earth along which the two sides have been displaced relative to one another parallel to the fracture. The accumulated displacement across a fault may range from a fraction of a meter to many tens or hundreds of kilometers. The type of fault is specified according to the orientation and sense of slip and the inclination (dip) of the fault plane (Aki and Richards, 1980; Yeats et al., 1997). If the block opposite an observer looking across the fault moves to the right, the slip style is termed right lateral (dextral), if the block moves to the left, the motion is termed left lateral (sinistral). Dip-slip faults are inclined fractures along which rock masses have mostly shifted vertically. If the rock mass above an inclined fault moves down (due to lateral extension) the fault is termed normal, whereas if the rock above the fault moves up (due to lateral compression), the fault is termed reverse (or thrust). Oblique-slip faults have significant compon...
en Fracture or fracture zone in the ground, along which the two rocky blocks move relative to each other.
en A fracture along which the blocks of crust on either side have moved relative to one another parallel to the fracture.
exact match c fbb472a4
in scheme Vocabulaire des mots clefs
label
fr Faille
en Fault
narrow match Faille active
pref label
fr Faille
en Fault
same as c fbb472a4
source wats
top concept of Vocabulaire des mots clefs
type Concept | feature of interest
was attributed to Pôle FormaTerre