Autor: |
Barré Guillaume, Elias-Bahnan Alexy, Motte Geoffrey, Ducoux Maxime, Hoareau Guilhem, Laurent Dimitri, Gaucher Eric C. |
Jazyk: |
English<br />French |
Rok vydání: |
2019 |
Předmět: |
|
Zdroj: |
E3S Web of Conferences, Vol 98, p 01001 (2019) |
Druh dokumentu: |
article |
ISSN: |
2267-1242 |
DOI: |
10.1051/e3sconf/20199801001 |
Popis: |
Several fluid circulation events are recorded in the Aquitaine Basin and the Chaînons Béarnais in the Pyrenean belt of southwestern France. Different fluid types are found in all locations studied. The main difference comes from the thermal peak event (rifting), which was more intense in the Chaînons Béarnais close to the exhumed mantle zone. In situ gas analysis associated of fluid inclusions and isotopic (C, O, H, S) analyses show that similar fluids are generated in both systems, although separated by deep structures, e.g. the North Pyrenean Frontal Thrust (NPFT). The Pyrenean tectonic history leads to the compartmentalization of fluid circulations. |
Databáze: |
Directory of Open Access Journals |
Externí odkaz: |
|