The influence of geomorphological and hydrologic conditions on travertine deposit formation has been studied in Cogolls Valley (Girona, Spain). Results indicate an evolutive sequence of the Quaternary materials, that is related to instabilities created by progresive changes into the valley systemEl estudio de las formaciones travertfnicas cuaternarias del valle de Cogolls (Girona) se centra fundamentalmente en la influencia del contexto geomorfológico y en las condiciones hidrológicas que motivaron su precipitación. A partir de ello, se propone una secuencia evolutiva del conjunto de los materiales cuaternarios relacionada con las inestabilidades derivadas de los cambios progresivos ocurridos en la cuenc
Abstract. - Tufas and travertines are mainly detritical carbonates deposits coming from karstical sp...
El Barranco de Azuaje está situado en el NE de la isla volcánica de Gran Canaria. El barranco se fo...
Fossil travertine deposits have been recognized in the Aguilar Fm., which are intercalated vyithin t...
The aim of this study, using geomorphologic, sedimentological and geochemical new data, is to presen...
The aim of this study is to present, through the use of new geomorphologic, sedimentological and geo...
Diagenesis of Miocene-Pliocene continental rocks in extensional Teruel Basin related to deposition o...
En este trabajo se presenta un estudio geomorfológico del valle del río Tuéjar (Valencia), en el que...
This work studies a fossil system of perched and fluvial travertines passing distally to fluvial tuf...
In the Tabernas desert there are several sectors with Quaternary travertines not formed in the proxi...
Los Llanos de Cubillas (Sot de Chera, Valencia) es una cuenca intramontañosa que registra una sedime...
The Argens upper watershed, upstream to the Valley Sourn gorges, is rich in remarkable travertine de...
Travertines represent an important deposit in the whole central Apennine: in fact, travertine deposi...
Fossil travertine deposits ha ve been recognlzed in the Aguilar Fm., which are intercalated within t...
A brief description of the Quaternary deposits of the Negro-Guayuriba river valley is presented here...
Holocene and present-day calcareous tufs formations of Central Spain are described and modélized in ...
Abstract. - Tufas and travertines are mainly detritical carbonates deposits coming from karstical sp...
El Barranco de Azuaje está situado en el NE de la isla volcánica de Gran Canaria. El barranco se fo...
Fossil travertine deposits have been recognized in the Aguilar Fm., which are intercalated vyithin t...
The aim of this study, using geomorphologic, sedimentological and geochemical new data, is to presen...
The aim of this study is to present, through the use of new geomorphologic, sedimentological and geo...
Diagenesis of Miocene-Pliocene continental rocks in extensional Teruel Basin related to deposition o...
En este trabajo se presenta un estudio geomorfológico del valle del río Tuéjar (Valencia), en el que...
This work studies a fossil system of perched and fluvial travertines passing distally to fluvial tuf...
In the Tabernas desert there are several sectors with Quaternary travertines not formed in the proxi...
Los Llanos de Cubillas (Sot de Chera, Valencia) es una cuenca intramontañosa que registra una sedime...
The Argens upper watershed, upstream to the Valley Sourn gorges, is rich in remarkable travertine de...
Travertines represent an important deposit in the whole central Apennine: in fact, travertine deposi...
Fossil travertine deposits ha ve been recognlzed in the Aguilar Fm., which are intercalated within t...
A brief description of the Quaternary deposits of the Negro-Guayuriba river valley is presented here...
Holocene and present-day calcareous tufs formations of Central Spain are described and modélized in ...
Abstract. - Tufas and travertines are mainly detritical carbonates deposits coming from karstical sp...
El Barranco de Azuaje está situado en el NE de la isla volcánica de Gran Canaria. El barranco se fo...
Fossil travertine deposits have been recognized in the Aguilar Fm., which are intercalated vyithin t...