The link between lithospheric scale deformations and deep fluid emanations: Inferences from the Southeastern Carpathians, Romania

Author:

Lange T.P.ORCID,Palcsu L.,Szakács A.,Kővágó Á.,Gelencsér O.,Gál Á.,Gyila S.,M. Tóth T.,Mațenco L.,Krézsek Cs.,Lenkey L.,Szabó Cs.,Kovács I.J.

Funder

Magyar Tudományos Akadémia

NKFIH

Ministry for Innovation and Technology

Nemzeti Kutatási Fejlesztési és Innovációs Hivatal

Innovációs és Technológiai Minisztérium

Eötvös Loránd Research Network

Publisher

Elsevier BV

Reference146 articles.

1. Some geological connections between the mineral carbonic and thermal waters and the post-vulcanic manifestations correlated with the deep geological structure of the East Carpathians territory–Romania;Airinei;Institutul de Geologie și Geofizică, Studii Tehnice și Economice, Seria E, Hidrogeologie,1975

2. Noble gas studies of fluids and gas exhalations in the East Carpathians, Romania;Althaus;Chem. Erde-Geochem.,2000

3. Rheological implications of the thermal structure of the lithosphere in the convergence zone of the Eastern Carpathians;Andreescu;J. Geodyn.,2001

4. Thermal budget of the Transylvanian lithosphere. Reasons for a low surface heat-flux anomaly in a Neogene intra-Carpathian basin;Andreescu;Geophys. J. Int.,2002

5. Origins of cratonic mantle discontinuities: a view from petrology, geochemistry and thermodynamic models;Aulbach;Lithos,2017

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