At the research frontiers of plate tectonics: Microearthquakes along the Knipovich Ridge help understanding ultraslow seafloor spreading
At mid-ocean spreading ridges, tectonic plates drift apart and upwelling magma builds new seafloor and tectonic plates. Spreading ridges are grouped according to their spreading velocity. The slowest ridges among them work entirely different than their faster counterparts. They do not receive enough...
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| Format: | Conference Object |
| Language: | unknown |
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2020
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| Online Access: | https://epic.awi.de/id/eprint/53399/ https://hdl.handle.net/10013/epic.b7c7d7f3-2c8e-4201-a8b5-ea8acc696149 |