Density distribution across the Alpine lithosphere constrained by 3-D gravity modelling and relation to seismicity and deformation
<p>The Alpine orogen formed as a result of the collision between the Adriatic and European plates. Significant crustal heterogeneity exists within the region due to the long history of interplay between these plates, other continental and oceanic blocks in the region, and inherited crustal features...
Gorde:
| Egile Nagusiak: | , , , , , |
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| Formatua: | Artigo |
| Hizkuntza: | Inglês |
| Argitaratua: |
Copernicus Publications
2019-11-01
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| Saila: | Solid Earth |
| Sarrera elektronikoa: | https://www.solid-earth.net/10/2073/2019/se-10-2073-2019.pdf |
| Etiketak: |
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