Formación de sulfuros de hierro en estuarios actuales:algunas consideraciones genéticas.

1. Borrego Flores, José
2. Morales González, Juan Antonio
3. Pendón Martín, José Gabriel

Export

Export

×

MLA

modern-language-association

APA

apa

Chicago

chicago-fullnote-bibliography

Harvard

harvard-cite-them-right

Vancouver

vancouver-author-date

---

RIS BibTex

Export

×

This document cannot be exported because it belongs to another portal.

Full text

lock_openArias Montano externo

DIALNET GOOGLE SCHOLAR lock_openArias Montano editor

More publications in: Geogaceta

Abstract

Iron sulfides found in estuaries located along the mesotidal coast of Huelva (SW Iberia) show various kinds of occurrence and allow to infer their genesis as an early diagenetic process. Sediment burial produces the alteration of organic matter and the reduction of ferric iron which reacts with amorfous iron grains supplied by Plio-Pleistocene sediments from the substrate. Sulfates supplied by marine waters can produce reduction of sulfur. Iron sulfides precipitation is then taken into account

Data source: Dialnet