Investigating deep earthquake mechanisms of the M6.6 Java Sea earthquake, 2016
Devastating earthquakes in the brittle shallow earth occur due to frictional sliding between the plates. However, at the depth between 100 and 600km, where brittle deformation is inaccessible, deep earthquakes occur frequently. Therefore, deep earthquakes require a different mechanism. The M6.6 Jav...
| প্রধান লেখক: | |
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| অন্যান্য লেখক: | |
| বিন্যাস: | Final Year Project (FYP) |
| ভাষা: | English |
| প্রকাশিত: |
2019
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| বিষয়গুলি: | |
| অনলাইন ব্যবহার করুন: | http://hdl.handle.net/10356/76436 |