Estructura en forma de ceja
Una línea sísmica a través de un arrecife enterrado podría mostrar dos eventos convexos hacia arriba (los lados opuestos del arrecife) separados por una laguna central baja o un colapso de arrecife.
This website uses cookies. If you continue without changing your browser settings, you consent to our use of cookies in accordance with our cookie policy. You can disable cookies at any time. Learn more
We also use partner advertising cookies to deliver targeted, geophysics-related advertising to you; these cookies are not added without your direct consent.