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Scheduled Cruises in 2004


Summary of a cruise on margins research (RUS.041)

Location and cruise identifier :   North Atlantic and Western Mediterranean

Research ship :   RV Professor Logachev

Sails :   15 July 2004

Docks :   18 September 2004

Duration :   

Principal Scientist/Investigator :   

Laboratory :   Polar Marine Geosurvey Expedition

Other investigators :   

E-mail contact for further information :   

Nankai
    Fig - Areas visited by the RV Professor Logachev.

Preliminary Scientific Programme :    The forthcoming TTR14 cruise will be carried out in the North Atlantic and Western Mediterranean with the RV Professor Logachev owned and operated by the Polar Marine Geosurvey Expedition (PMGE, St. Petersburg, Russia) from 15 July to 18 September 2004.

     The cruise will start in St. Petersburg (Russia), while the embarkation of non-Russian participants will take place in Porto (Portugal) on 24 July. The expedition will terminate in Naples (Italy) on 17 September. Intermediate port calls are planned to Cadiz (Spain) on 10 - 11 August, Cartagena (Spain) on 19 - 20 August and Barcelona (Spain) on 1 - 2 September. The cruise programme will be divided into 4 Legs with the total of 8 study areas.

Leg 1 - Area 1

Location :   Gulf of Cadiz - Porto to Cadiz

Dates :   25 July 2004 - 10 August 2004

Scientific objectives :    The area of the Gulf of Cadiz has been intensively studied during several recent TTR expeditions, focussed mainly on mud volcanism, fluid venting and related phenomena. About 20 mud volcanoes have been discovered and confirmed by sampling. Gas hydrates, carbonate crust and nodules, as well as benthic chemosynthetic communities were sampled from some of these structures. Large carbonate chimneys, related to fluid escape were sampled and recorded by a deep-towed video system. Within the TTR14 Cruise, further detailed geological and geophysical investigations of known mud volcanoes, fluid escape features, gas hydrate accumulations and other related phenomena will be conducted, together with searching for yet unknown structures of similar origin.

Leg 2 - Area 2

Location :   West Alboran Basin - Cadiz to Cartagena

Dates :   11 August 2004 - 19 August 2004

Scientific objectives :    The notable mud-diapir province recognized in the West Alboran Basin is formed of over-pressed shales of the early Miocene (Burdigalian) age. The mud diapirism is related to the middle Miocene extensional processes, but diapirism resumed at post-Messinian time and continuated till the Holocene then reaching the sea floor. The planned survey will continue the previous studies of mud volcanoes in the Alboran Mud Diapiric Province (Northern and Southern Sectors). The aims are: to enlarge and complete former surveys conducted by TTR- 9 (1999) and TTR-12 (2002) on the mud volcano fields in the Spain and Moroccan margins of the West Alboran Basin; to enlarge the seismic profiling survey across mud volcanoes; to collect information around new mud volcanoes; to image from high-resolution MAK new mud volcanoes; and to sample mud volcano material and related rocks. The tectonic framework of the area as well as the volcanic basemen will also be investigated.

Leg 2 - Area 3

Location :    Almeria-Palomares Margin and core transect from the East Alboran to the South Balearic Basins

Dates :   11 August 2004 - 19 August 2004

Scientific objectives :    Investigation of the SE Iberian continental margin and its wide-spread deep-sea depositional systems will be performed with the use of single-channel seismics, long-range and deep-towed side-scan sonars, and bottom sampling. To be studied are the expressions of active faults on the sea bottom, recent tectonics and turbidite systems in the Palomares margin.

     Self-temperate carbonate Holocene deposits or mounds on the Almeria Margin are among important tasks of this leg as well.

     Among other important objectives, it is planned to continue the studies of Holocene pelagic sedimentation in the area with the view to develop paleoclimate reconstruction in the Western Mediterranean during the last 20,000 years. Core transect will be performed with the use of heavy, 6 m long gravity corer of large diameter.

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