F. Harmegnies

发表

Campagne FARE: Wireline reentry of DSDP Hole 396B using the NADIA System

Ralph A. Stephen, Gerard Loaec, J. Legrand, 1989 .

Heat flow in the Sea of Marmara Central Basin: Possible implications for the tectonic evolution of the North Anatolian fault,

A. Bécel, C. Grall, P. Henry, 2012 .

Spatial distribution of diverse cold seep communities living on various diapiric structures of the southern Barbados prism

J. Foucher, K. Olu, M. Sibuet, 1996 .

In-situ sediment temperature measurements and geochemical porewater data suggest highly dynamic fluid flow at Isis mud volcano, eastern Mediterranean Sea

Tomas Feseker, J. Foucher, Jean-Paul Foucher, 2009 .

Seafloor geological studies above active gas chimneys off Egypt (Central nile deep sea fan)

Jean-Claude, A. Boetius, H. Niemann, 2007 .

Variations in heat flow across the ocean—continent transition in the Iberia abyssal plain

J. Sibuet, K. Louden, F. Harmegnies, 1997 .

Warm brine lakes in craters of active mud volcanoes, Menes caldera off NW Egypt: evidence for deep-rooted thermogenic processes

J. Foucher, J. Mascle, S. Dupré, 2014, Geo-Marine Letters.

Hydrothermal activity in the Lau Basin: First results from the NAUTILAU Cruise

P. Herzig, J. Erzinger, J. Charlou, 1990 .

18. LONG-TERM OBSERVATIONS OF PRESSURE AND TEMPERATURE IN HOLE 948D, BARBADOS ACCRETIONARY PRISM 1

J. Foucher, P. Henry, Jean-Paul Foucher, 1997 .

Deep‐penetration heat flow probes raise questions about interpretations from shorter probes

E. Michel, Daniel Aslanian, Alain Normand, 2001 .