Abstract
A series of analog modeling experiments were carried out to investigate lateral strike-slip fault propagation vs. attenuation across a discrete rheology boundary, and to gain insight on the mechanics governing the generation of associated characteristic structural patterns. Experiments were conceived to simulate the lateral propagation of a strike-slip fault through a Mohr-Coulomb medium (dry quartz sand), from a zone overlying a rigid basement (where the fault is pre-cut) to another one where the sand lies on top of a viscous (Newtonian) silicone layer. Comparison of the obtained results with the natural example of the Gloria Fault - Tore-Madeira intersection (Eurasia-Nubia plate boundary, NE Atlantic) revealed a striking first-order resemblance, allowing speculation about a compliant tectono-magmatic evolution, and stressing the relevance for future enhanced modeling.
| Original language | English |
|---|---|
| Pages (from-to) | 1429-1432 |
| Number of pages | 4 |
| Journal | Comunicacoes Geologicas |
| Volume | 101 |
| Issue number | Special Issue 3 |
| Publication status | Published - 1 Dec 2014 |
UN SDGs
This output contributes to the following UN Sustainable Development Goals (SDGs)
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SDG 7 Affordable and Clean Energy
Keywords
- Analog modelling
- Gloria fault
- Rheological boundary
- Strike-slip fault propagation
- Tore-madeira rise
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