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The deposition of diatom mats, and associated diluted magnetic mineral concentrations, leads to weak magnetizations and susceptibilities in these intervals. Bulk density measurements taken at Site U show a similar trend among holes and are variable, ranging from 1. There appears to be a slight correlation between thermal conductivity and magnetic susceptibility, GRA, and NGR data sets, but low resolution of the thermal conductivity data does not allow further conclusions. The discontinuity is characterized by higher values and higher-frequency variability below the discontinuity and lower values and lower-frequency variability above. We use cookies to ensure that we give you the best experience on our website. The magnetic susceptibility record shows two main trends at Site U Fig. Moisture and density MAD properties were also measured on two discrete samples per core, usually at the bottom of Section 1 and the top of Section 6.

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The bulk density record shows a very similar trend to that of magnetic u1304. The discontinuity is characterized by higher values and higher-frequency variability below the discontinuity and lower values and lower-frequency variability above. Moisture and density MAD u1304 were also measured on two discrete samples per core, usually at the bottom of Section 1 and the top of U11304 6.

As expected, porosity shows an inverse relationship to u134. Planktonic foraminifers, Hole UB. Other digital versions may also be u1304 to download e.

The discrete measurements match the values produced by the MST Fig. Xuan, U1304Channell, James E.

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The age model for Site U was established by matching? Thermal conductivity Discrete thermal conductivity measurements were made usually on Section 4 uu1304 each core at Site U Table T Download statistics Downloads from ePrints over the past year.

Thermal conductivity was measured on whole cores in Hole UA with a frequency of one per section for each core. This trend may be u1304 to the presence of diatom layers causing the interval density u1304 to be reduced to a value lower than that of the surrounding silty clay layers. Planktonic foraminifers, Hole UC. Bulk density u1304 taken at Site I1304 show a similar trend among holes and are variable, y1304 from 1.

These mats had highly variable thickness from centimeter to meter scale. NGR counts range from 0 to u1304 cps with the majority of the values between 7 and 21 cps Fig.

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Porosity decreases only slightly with depth at Site U The magnetic susceptibility record shows two main trends at Site U U1304. We use cookies to ensure that we give you the best experience on our website. Library staff additional information. The deposition of diatom mats, and associated diluted magnetic mineral concentrations, leads to weak magnetizations and susceptibilities in u1304 intervals. Nannofossil y1304 smear slides. Laminated diatom ooze split with wire.

GRA density Bulk density measurements u1304 at Site K1304 show a similar trend among holes and are variable, ranging from 1.

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If you continue without changing your settings, we will assume u1304 you are happy to receive cookies on the University of Southampton website. Planktonic foraminifers, Hole UA. Prominent intervals of diatom mats at Site U are associated with the latter stages of interglacial marine isotope stages MIS 9, 11, 13, 15, 21, 27 and 35, and with the weak glacial of MIS Discrete thermal conductivity measurements were made usually on Section 4 of u1304 core u1304 Site U Table T Planktonic foraminifers, Hole UD.

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This repository has been built using U1304 softwaredeveloped at the University of Southampton, but available to everyone to use. There appears to be a slight correlation between thermal u1304 and magnetic susceptibility, GRA, and NGR data sets, but u1304 resolution of the thermal conductivity data does not allow further conclusions. Thermal conductivity is highly variable ranging from 0. Comparison of histograms of paleomagnetic directions and RPI from diatom-rich sediments and from surrounding silty clays indicates that, although results from diatom-rich sediments are more scattered, the occurrence of diatom mats does not appreciably distort the paleomagnetic directional and RPI records.

Laminated diatom ooze split with saw. Natural gamma radiation NGR counts range from 0 to 35 cps with the majority of the values between 7 and 21 cps Fig.