Estructuras de deformación en sedimentos del Cuaternario reciente de la cuenca del Bajo Segura (Alicante).Discusión sobre su posible origen sísmico.

1. Alfaro García, Pedro
2. Doménech Morante, César
3. Estévez Rubio, Antonio
4. Soria Mingorance, Jesús Miguel

Exportieren

Exportieren

×

MLA

modern-language-association

APA

apa

Chicago

chicago-fullnote-bibliography

Harvard

harvard-cite-them-right

Vancouver

vancouver-author-date

---

RIS BibTex

Exportieren

×

Das Dokument kann nicht exportiert werden, da es zu einem anderen Portal gehört.

Volltext

lock_openArias Montano externo

DIALNET GOOGLE SCHOLAR lock_openArias Montano editor

Andere Publikationen in: Geogaceta

Zusammenfassung

Aiming at recognizing the prints in the most recent sedimentary record due to earthquakes, able to develop liquefaction and fluidization in sediments (magnitude equal to or more than 5), we have studied eight boreholes, each about 40 m long, located in the Low Segura basin (Alicante, Spain). We have recognized disturbances due to the own boring activity, as well as others due to bioturbation, thixotropy in clayey levels and to what, in our opinion, is the effect of seismic shocks (microfaults, distorted lamination and fluid scape structures)

Fuente de los datos: Dialnet