The evolution of fault networks during multiphase deformation: An analogue modeling approach Article Swipe
Jun Liu
,
Matthias Rosenau
,
Ehsan Kosari
,
Sascha Brune
,
Frank Zwaan
,
Onno Oncken
·
YOU?
·
· 2024
· Open Access
·
· DOI: https://doi.org/10.5194/egusphere-egu24-15107
YOU?
·
· 2024
· Open Access
·
· DOI: https://doi.org/10.5194/egusphere-egu24-15107
It is well known that triaxial deformation is a common feature of continental tectonics, and is accommodated by complex polymodal fault networks. Field investigations confirm that multiple phases involving time-dependent three-dimensional strain conditions (e.g. constriction, plane, and flattening strain) affect the spatial and temporal interaction of polymodal fault systems. However, a key question remains: How do changing strain conditions affect the reactivation of fault systems that formed during a previous deformation phase? Here, we conduct scaled analogue models with time-dependent boundary conditions to investigate how fault networks evolve under changing boundary conditions, including reactivation and formation of new faults.We have developed a setup in which a basal rubber sheet is stretched in one direction, so that longitudinal extension and layer thinning are accompanied by lateral shortening, hence producing triaxial deformation (Liu et al. in revision). According to previous brittle-viscous experiments with this set-up, an increase in longitudinal extension velocity results in a higher coupling between the rubber base and brittle layer, generating increasing transmission of lateral shortening from the base into the brittle layer. We thus induce constriction-to-plane strain conditions in the brittle layer as a function of longitudinal extension velocity by varying the magnitude of lateral contraction. In a new set of experiments, by varying extension velocity either stepwise or continuously, we realize time-dependent kinematic boundary conditions including deformation phases and secular changes, respectively. Digital image correlation (DIC) and photogrammetry (structure from motion, SFM) are employed to track the 3D kinematic surface and topography evolution, respectively.Preliminary observations show both the formation of new faults and the reactivation of early phase faults through a change from plane to constriction strain. Conversely, a change from constriction to plane strain conditions results in the abandonment of the early phase fault network as it becomes overprinted by fault systems of the subsequent phase. Moreover, early-phase fault systems influence the propagation and linkage of fault populations in subsequent phases. Our analogue models highlight the impact of strain conditions on the overall plan-view geometry of fault populations, providing alternative explanations for complex fault patterns and interactions (e.g. the Jeanne d’Arc basin, the North Træna Basin, and the Beagle Platform).
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Metadata
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- Language
- en
- Landing Page
- https://doi.org/10.5194/egusphere-egu24-15107
- OA Status
- gold
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- OpenAlex ID
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All OpenAlex metadata
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https://openalex.org/W4392758761Canonical identifier for this work in OpenAlex
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https://doi.org/10.5194/egusphere-egu24-15107Digital Object Identifier
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The evolution of fault networks during multiphase deformation: An analogue modeling approachWork title
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preprintOpenAlex work type
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enPrimary language
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2024Year of publication
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2024-03-09Full publication date if available
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Jun Liu, Matthias Rosenau, Ehsan Kosari, Sascha Brune, Frank Zwaan, Onno OnckenList of authors in order
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https://doi.org/10.5194/egusphere-egu24-15107Publisher landing page
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goldOpen access status per OpenAlex
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https://doi.org/10.5194/egusphere-egu24-15107Direct OA link when available
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Fault (geology), Deformation (meteorology), Computer science, Materials science, Geology, Seismology, Composite materialTop concepts (fields/topics) attached by OpenAlex
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0Total citation count in OpenAlex
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| abstract_inverted_index.conditions | 32, 58, 81, 179, 217, 278, 323 |
| abstract_inverted_index.direction, | 113 |
| abstract_inverted_index.evolution, | 245 |
| abstract_inverted_index.flattening | 37 |
| abstract_inverted_index.generating | 161 |
| abstract_inverted_index.increasing | 162 |
| abstract_inverted_index.revision). | 134 |
| abstract_inverted_index.shortening | 166 |
| abstract_inverted_index.subsequent | 298, 313 |
| abstract_inverted_index.tectonics, | 13 |
| abstract_inverted_index.topography | 244 |
| abstract_inverted_index.Conversely, | 270 |
| abstract_inverted_index.abandonment | 282 |
| abstract_inverted_index.accompanied | 122 |
| abstract_inverted_index.alternative | 333 |
| abstract_inverted_index.conditions, | 91 |
| abstract_inverted_index.continental | 12 |
| abstract_inverted_index.correlation | 227 |
| abstract_inverted_index.deformation | 6, 70, 129, 219 |
| abstract_inverted_index.early-phase | 301 |
| abstract_inverted_index.experiments | 139 |
| abstract_inverted_index.interaction | 44 |
| abstract_inverted_index.investigate | 83 |
| abstract_inverted_index.overprinted | 292 |
| abstract_inverted_index.populations | 311 |
| abstract_inverted_index.propagation | 306 |
| abstract_inverted_index.shortening, | 125 |
| abstract_inverted_index.accommodated | 16 |
| abstract_inverted_index.constriction | 268, 274 |
| abstract_inverted_index.contraction. | 197 |
| abstract_inverted_index.experiments, | 203 |
| abstract_inverted_index.explanations | 334 |
| abstract_inverted_index.interactions | 340 |
| abstract_inverted_index.longitudinal | 116, 146, 188 |
| abstract_inverted_index.observations | 247 |
| abstract_inverted_index.populations, | 331 |
| abstract_inverted_index.reactivation | 61, 93, 257 |
| abstract_inverted_index.transmission | 163 |
| abstract_inverted_index.constriction, | 34 |
| abstract_inverted_index.continuously, | 211 |
| abstract_inverted_index.respectively. | 224 |
| abstract_inverted_index.Træna | 348 |
| abstract_inverted_index.investigations | 23 |
| abstract_inverted_index.photogrammetry | 230 |
| abstract_inverted_index.time-dependent | 29, 79, 214 |
| abstract_inverted_index.brittle-viscous | 138 |
| abstract_inverted_index.d’Arc | 344 |
| abstract_inverted_index.three-dimensional | 30 |
| abstract_inverted_index.including  | 92 |
| abstract_inverted_index.constriction-to-plane | 177 |
| abstract_inverted_index.respectively.Preliminary | 246 |
| cited_by_percentile_year | |
| corresponding_author_ids | https://openalex.org/A5016678837, https://openalex.org/A5089281652 |
| countries_distinct_count | 2 |
| institutions_distinct_count | 6 |
| corresponding_institution_ids | https://openalex.org/I154338468, https://openalex.org/I176453806 |
| citation_normalized_percentile.value | 0.03273621 |
| citation_normalized_percentile.is_in_top_1_percent | False |
| citation_normalized_percentile.is_in_top_10_percent | False |