Results of direct shear experiments on intact and powdered samples from the submarine flank of Kilauea volcano (Hawaii, USA)
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| Auteurs principaux: | , , , |
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| Format: | Dataset Open Access |
| Langue: | en |
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PANGAEA
2025
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| _version_ | 1867169521411817472 |
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| author | Stoepke, Fiene Ikari, Matt J Morgan, Julia K Urlaub, Morelia |
| author_facet | Stoepke, Fiene Ikari, Matt J Morgan, Julia K Urlaub, Morelia |
| collection | Datos científicos de ciencias marinas y ambientales |
| contents | We performed laboratory friction experiments on simulated fault gouges and intact samples from the submarine flank of Kilauea volcano (Hawaii, USA) and measured the velocity-dependence of friction in velocity-step tests. Moreover, we have directly measured cohesion on the fault gouge and intact samples from Kilauea's submarine flank. The experiments were carried out using a single-direct shear device at room temperature. For the shearing tests, the samples simulating fault gouge were crushed and sieved to a grain size of < 125 µm. The intact samples were tested as mini-cores. All experiments were carried out under fluid-saturated conditions (3.5 % NaCl brine) and under an effective normal load of 10 MPa. |
| format | Dataset Open Access |
| id | pangaea_https___doi_org_10_1594_PANGAEA_985068 |
| institution | PANGAEA |
| language | en |
| publishDate | 2025 |
| publisher | PANGAEA |
| record_format | pangaea |
| spellingShingle | Results of direct shear experiments on intact and powdered samples from the submarine flank of Kilauea volcano (Hawaii, USA) Stoepke, Fiene Ikari, Matt J Morgan, Julia K Urlaub, Morelia cohesion; Direct Shear; Kilauea_Volcano; Laboratory experiment; rate-and-state friction; SUB; Submersible We performed laboratory friction experiments on simulated fault gouges and intact samples from the submarine flank of Kilauea volcano (Hawaii, USA) and measured the velocity-dependence of friction in velocity-step tests. Moreover, we have directly measured cohesion on the fault gouge and intact samples from Kilauea's submarine flank. The experiments were carried out using a single-direct shear device at room temperature. For the shearing tests, the samples simulating fault gouge were crushed and sieved to a grain size of < 125 µm. The intact samples were tested as mini-cores. All experiments were carried out under fluid-saturated conditions (3.5 % NaCl brine) and under an effective normal load of 10 MPa. |
| title | Results of direct shear experiments on intact and powdered samples from the submarine flank of Kilauea volcano (Hawaii, USA) |
| topic | cohesion; Direct Shear; Kilauea_Volcano; Laboratory experiment; rate-and-state friction; SUB; Submersible |
| url | https://doi.org/10.1594/PANGAEA.985068 |