![Bollettino della Geological Society of America. La geologia. Le illustrazioni dei movimenti di traduttori 171. Figura 2.-lo slittamento, lanciare e Heave le superfici superiore ed inferiore del blocco sono orizzontali; le Bollettino della Geological Society of America. La geologia. Le illustrazioni dei movimenti di traduttori 171. Figura 2.-lo slittamento, lanciare e Heave le superfici superiore ed inferiore del blocco sono orizzontali; le](https://c8.alamy.com/compit/rggtxk/bollettino-della-geological-society-of-america-la-geologia-le-illustrazioni-dei-movimenti-di-traduttori-171-figura-2-lo-slittamento-lanciare-e-heave-le-superfici-superiore-ed-inferiore-del-blocco-sono-orizzontali-le-facce-di-estremita-sono-verticali-e-ad-angolo-retto-rispetto-al-guasto-sciopero-a-b-c-e-d-si-trovano-in-fault-piano-nella-faccia-di-estremita-lasciate-che-il-punto-originariamente-adiacente-ad-una-mossa-a-b-quindi-ab-slittamento-o-slittamento-netto-ad-trace-slip-cb-dip-slip-fk-buttare-ac-strike-slip-ek-heave-bd-slittamento-perpendicolare-e-f-e-fc-si-prega-di-notare-che-queste-immagini-vengono-estratte-dalla-pagina-sottoposta-a-scansione-di-immagini-che-possono-essere-state-digital-rggtxk.jpg)
Bollettino della Geological Society of America. La geologia. Le illustrazioni dei movimenti di traduttori 171. Figura 2.-lo slittamento, lanciare e Heave le superfici superiore ed inferiore del blocco sono orizzontali; le
![Vettoriale Stock Fault type vector illustration set (3 dimensions) / Normal, Reverse, Strike-slip etc. | Adobe Stock Vettoriale Stock Fault type vector illustration set (3 dimensions) / Normal, Reverse, Strike-slip etc. | Adobe Stock](https://as2.ftcdn.net/v2/jpg/02/87/96/57/500_F_287965781_vMOhVJWBbTyLLD8pJ9CMtmpT8KhtgzIR.jpg)
Vettoriale Stock Fault type vector illustration set (3 dimensions) / Normal, Reverse, Strike-slip etc. | Adobe Stock
Learning goals - January 16, 2012 You will understand how to: Describe the geometry of a fault (1) orientation of the plane (str
![Rock faults are ruptures along which opposite faces of rock have slid past each other. In Fig. 3-35, points A and B coincided before the rock in the foreground slid down to Rock faults are ruptures along which opposite faces of rock have slid past each other. In Fig. 3-35, points A and B coincided before the rock in the foreground slid down to](https://www.vedantu.com/question-sets/a01d6d59-0fb8-4df3-80d5-825072387556187408460538327319.png)
Rock faults are ruptures along which opposite faces of rock have slid past each other. In Fig. 3-35, points A and B coincided before the rock in the foreground slid down to
![4 A planar fault is defined by the strike and dip of the fault surface... | Download Scientific Diagram 4 A planar fault is defined by the strike and dip of the fault surface... | Download Scientific Diagram](https://www.researchgate.net/publication/269277748/figure/fig2/AS:669526098202629@1536638869613/A-planar-fault-is-defined-by-the-strike-and-dip-of-the-fault-surface-and-the-direction-of.png)
4 A planar fault is defined by the strike and dip of the fault surface... | Download Scientific Diagram
![Block diagram of a generic fault plane, redrawn and modified from both... | Download Scientific Diagram Block diagram of a generic fault plane, redrawn and modified from both... | Download Scientific Diagram](https://www.researchgate.net/publication/266436983/figure/fig9/AS:670314467975190@1536826831289/Block-diagram-of-a-generic-fault-plane-redrawn-and-modified-from-both-Allmendinger-et.png)
Block diagram of a generic fault plane, redrawn and modified from both... | Download Scientific Diagram
![Geosciences | Free Full-Text | Major Strike-Slip Faults Identified Using Satellite Data in Central Borneo, SE Asia Geosciences | Free Full-Text | Major Strike-Slip Faults Identified Using Satellite Data in Central Borneo, SE Asia](https://pub.mdpi-res.com/geosciences/geosciences-08-00156/article_deploy/html/images/geosciences-08-00156-g004.png?1570059765)