Intrasediment gypsum in subtidal offshore carbonates as a witness of basin-wide evaporitic precipitation. The case of the southern Variscan foreland basin (mid-Carboniferous)

Author:

Díaz-García Iván,Merino-Tomé Óscar,Quijada I. Emma,Bahamonde Juan R.,Fernández Luis P.,Della Porta Giovanna,Samankassou Elias,Kulagina Elena I.,Borrego Ángeles G.,Martín-Llaneza Jaime,Del Pozo José Federico

Funder

Gobierno del Principado de Asturias

Gobierno de España Ministerio de Ciencia Innovación y Universidades

Swiss National Science Foundation

Russian Academy of Sciences

Universidad de Oviedo

Gobierno de España Ministerio de Economía y Competitividad

Publisher

Elsevier BV

Reference169 articles.

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3. Kinetics and morphology of formed gypsum;Alimi;Desalination,2004

4. Sequences of thrusts and displacement transfer in the superposed duplexes of the Esla Nappe Region (Cantabrian Zone, NW Spain);Alonso;Journal of Structural Geology,1987

5. Paleogeographic inversion resulting from large out of sequence breaching thrusts: the León Fault (Cantabrian zone, NW Iberia). A new picture of the external Variscan thrust belt in the Ibero-Armorican arc;Alonso;Geologica Acta,2009

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