Strong heat flow variability in an active shallow gas environment, Dnepr palaeo-delta, Black Sea

Author:

Poort J.,Kutas R. I.,Klerkx J.,Beaubien S. E.,Lombardi S.,Dimitrov L.,Vassilev A.,Naudts L.

Publisher

Springer Science and Business Media LLC

Subject

Earth and Planetary Sciences (miscellaneous),Geotechnical Engineering and Engineering Geology,Environmental Science (miscellaneous),Oceanography

Reference37 articles.

1. Beaubien SE, Haeckel M, Lombardi S (2004) Chemical analysis of sea water and sediment pore water. In: Naudts L, De Batist M (eds) Crimea 2004 Expedition Report. RCMG UGent, Gent, pp 80–92

2. Bodri L (1994) Hydrological disturbances of the conductive heat flow in stable continental crust. Tectonophysics 234:291–304

3. Cermak V, Balling N, Kukkonen I, Zui VI (1993) Heat flow in the Baltic shield: results of the lithospheric geothermal modelling. Precambrian Res 64:54–65

4. De Batist M, Klerkx J, Van Rensbergen P, Vanneste M, Poort J, Golmshtok AY, Kremlev AA, Khlystov O, Krinitsky P (2002) Active hydrate destabilization in Lake Baikal, Siberia? Terra Nova 14:436–442

5. Egorov VN, Luth U, Luth C, Gulin MB (1998) Gas seeps in the submarine Dniepr paleo-delta, Black Sea: acoustic video and trawl data. Ber ZMK Reihe E14:11–22

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