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Beachrocks from the Cabo Frio Island: unique geological record of the pleistocene - holocene transition in Rio de Janeiro State
The Cabo Frio Island, Rio de Janeiro State, southeast Brazil shows four bodies of beachrocks, emerged up to +1.5 m and submerged down to - 4.5 m. These bodies are constituted of discontinuous strips, parallel to the coastline. Beachrock is beach sediment that has been cemented within the intertidal...
محفوظ في:
| المؤلفون الرئيسيون: | , , , , , |
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| التنسيق: | Online |
| اللغة: | Português |
| منشور في: |
Universidade Federal do Rio de Janeiro
2012
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| الوصول للمادة أونلاين: | https://revistas.ufrj.br/index.php/aigeo/article/view/6927 |
| الوسوم: |
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