Three-dimensional variations of the slab geometry correlate with earthquake distributions at the Cascadia subduction system
Variations in seismicity are observed at subduction zones, but the oceanic sides remain poorly resolved. Here, the author presents tomographic results of the Cascadia subduction system demonstrating that there are significant variations of the oceanic lithosphere along the subduction zone.
| প্রধান লেখক: | |
|---|---|
| বিন্যাস: | প্রবন্ধ |
| ভাষা: | English |
| প্রকাশিত: |
Nature Portfolio
2018-03-01
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| মালা: | Nature Communications |
| অনলাইন ব্যবহার করুন: | https://doi.org/10.1038/s41467-018-03655-5 |