© 2015 Elsevier Ltd.Investigations carried out on surface sediments collected from the Anaximander mud volcanoes in the Eastern Mediterranean Sea to determine sedimentary and geochemical properties. The sediment grain size distribution and geochemical contents were determined by grain size analysis, organic carbon, carbonate contents and element analysis. The results of element contents were compared to background levels of Earth's crust. The factors that affect element distribution in sediments were calculated by the nine push core samples taken from the surface of mud volcanoes by the E/V Nautilus. The grain size of the samples varies from sand to sandy silt. Enrichment and Contamination factor analysis showed that these analyses can also...
Mud volcanism on the Mediterranean Ridge is caused by extrusion of overpressured sediments, with con...
Copyright © 2009 Elsevier B.V. All rights reserved. ScienceDirect® is a registered trademark of Else...
The Eastern Mediterranean Sea (EMS) is the last remnant of the Tethys Ocean that has been subducted ...
© 2015 Elsevier Ltd.Investigations carried out on surface sediments collected from the Anaximander m...
The pore water chemistry of mud volcanoes from the Olimpi Mud Volcano Field and the Anaximander Moun...
Submersible observations and seafloor mapping over areas of mud volcanism in the eastern Mediterrane...
Recent field observations have identified the widespread occurrence of fluid seepage through the eas...
The pore water chemistry of mud volcanoes from the Olimpi Mud Volcano Field and the Anaximander Moun...
Recent field observations have identified the widespread occurrence of fluid seepage through the eas...
Copyright © 2013 Semal Yemenicioglu, Sakir Cagan Tunc. This is an open access article distributed un...
A mud volcano field was recently discovered within the Malta Plateau in the Strait of Sicily (Centra...
A mud volcano field was recently discovered within the Malta Plateau in the Strait of Sicily (Centra...
Based on the analysis of geochemical and mineralogical compositions, deep sea clay sediment characte...
Clay mineralogy is an important characteristic of mud volcano sediments. This study determined the c...
Detailed geophysical, geochemical and petrological data over a cluster of large mud volcanoes at the...
Mud volcanism on the Mediterranean Ridge is caused by extrusion of overpressured sediments, with con...
Copyright © 2009 Elsevier B.V. All rights reserved. ScienceDirect® is a registered trademark of Else...
The Eastern Mediterranean Sea (EMS) is the last remnant of the Tethys Ocean that has been subducted ...
© 2015 Elsevier Ltd.Investigations carried out on surface sediments collected from the Anaximander m...
The pore water chemistry of mud volcanoes from the Olimpi Mud Volcano Field and the Anaximander Moun...
Submersible observations and seafloor mapping over areas of mud volcanism in the eastern Mediterrane...
Recent field observations have identified the widespread occurrence of fluid seepage through the eas...
The pore water chemistry of mud volcanoes from the Olimpi Mud Volcano Field and the Anaximander Moun...
Recent field observations have identified the widespread occurrence of fluid seepage through the eas...
Copyright © 2013 Semal Yemenicioglu, Sakir Cagan Tunc. This is an open access article distributed un...
A mud volcano field was recently discovered within the Malta Plateau in the Strait of Sicily (Centra...
A mud volcano field was recently discovered within the Malta Plateau in the Strait of Sicily (Centra...
Based on the analysis of geochemical and mineralogical compositions, deep sea clay sediment characte...
Clay mineralogy is an important characteristic of mud volcano sediments. This study determined the c...
Detailed geophysical, geochemical and petrological data over a cluster of large mud volcanoes at the...
Mud volcanism on the Mediterranean Ridge is caused by extrusion of overpressured sediments, with con...
Copyright © 2009 Elsevier B.V. All rights reserved. ScienceDirect® is a registered trademark of Else...
The Eastern Mediterranean Sea (EMS) is the last remnant of the Tethys Ocean that has been subducted ...