Hydrothermal massive dolomitization in the Cantabrian Zone (NW Spain): a Permian to Triassic event promoted by extensional tectonics?

Ronald J. Bakker; Marta Gasparrini; Thilo Bechstädt; M. Boni

Hydrothermal massive dolomitization in the Cantabrian Zone (NW Spain): a Permian to Triassic event promoted by extensional tectonics?

Titel in Übersetzung: Hydrothermal massive dolomitization in the Cantabrian Zone (NW Spain): a Permian to Triassic event promoted by extensional tectonics?

Ronald J. Bakker, Marta Gasparrini, Thilo Bechstädt, M. Boni

Lehrstuhl für Rohstoffmineralogie (620)

Publikation: Beitrag in Buch/Bericht/Konferenzband › Beitrag in Konferenzband

Titel in Übersetzung	Hydrothermal massive dolomitization in the Cantabrian Zone (NW Spain): a Permian to Triassic event promoted by extensional tectonics?
Originalsprache	Englisch
Titel	Deformation history, fluid flow reconstruction and reservoir appraisal in foreland fold and thrust
Seiten	1-5
Publikationsstatus	Veröffentlicht - 2002

Dieses zitieren

@inproceedings{fdad49e9e17c48de9736de19f7e00efe,

title = "Hydrothermal massive dolomitization in the Cantabrian Zone (NW Spain): a Permian to Triassic event promoted by extensional tectonics?",

author = "Bakker, {Ronald J.} and Marta Gasparrini and Thilo Bechst{\"a}dt and M. Boni",

year = "2002",

language = "English",

pages = "1--5",

booktitle = "Deformation history, fluid flow reconstruction and reservoir appraisal in foreland fold and thrust",