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| Main Author: | Pavlova, Galina A |
|---|---|
| Format: | Dataset Open Access |
| Language: | en |
| Published: |
PANGAEA
2005
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| Subjects: | |
| Online Access: | https://doi.org/10.1594/PANGAEA.763559 |
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(Table A) Chemical composition of interstitial waters from sediments and deposits within and outside the Haakon Mosby submarine mud volcano in the Norwegian Sea
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Chemical composition of bottom waters and interstitial waters from sediments and deposits within and outside the Haakon Mosby submarine mud volcano in the Norwegian Sea
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(Table 8.3.10) Chemical composition of interstitial waters from surface layer bottom sediments of the Haakon Mosby mud volcano, Norwegian Sea
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Chemical and isotopic compositions of samples from the Haakon Mosby mud volcano and nearby
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(Table 8.3.14) Rates of microbial processes in deposits covered by bacterial mats in the caldera of the Haakon Mosby mud volcano, Norwegian Sea
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(Table 8.3.12) Abundance of microorganisms in surface layer bottom sediments of the Haakon Mosby mud volcano, Norwegian Sea
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(Table 8.3.15) Chemical composition and rates of microbial processes in bottom water in caldera of the Haakon Mosby mud volcano, Norwegian Sea
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Chemical and isotopic compositions and age of carbonates from the Lost City hydrothermal field, Mid-Atlantic Ridge
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(Table 8.3.18) Contents of calcium carbonate and organic carbon and carbon isotopic compositions in surface deposits from the caldera of the Haakon Mosby mud volcano, Norwegian Sea
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(Table 1) Brief description, main minerals, and hydrocarbon and n-alkane contents in samples from the Rainbow Hydrothermal Field
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(Table 8.3.21) Isotopic composition of carbon and oxygen of dipersed and authigenic carbonates from the Haakon Mosby mud volcano, Norwegian Sea
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(Table 8.3.9a) Chemical and isotopic compositions of bottom sea water from the Haakon Mosby mud volcano, Norwegian Sea
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(Table 4) Radiocarbon datings and 87Sr/86Sr ratios in samples from carbonate mounds of the Lost City hydrothermal field
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(Table 6) Isotopic composition of carbon in tissues of mollusks from hydrothermal fields at the axis of the East Pacific Rise near 9°50'N
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(Table 8.3.22) Radiocarbon ages of authigenic carbonates of an carbonaceous edifice from the Haakon Mosby mud volcano, Norwegian Sea
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(Table 8.3.17) Chemical compositions of surface deposits in the caldera of the Haakon Mosby mud volcano, Norwegian Sea
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(Table 1) Chemical composition of carbonate bodies from the caldera of the Haakon Mosby mud volcano
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(Table 9) Isotopic compositions of sulfur from hydrothermal deposits of the Lucky Strike hydrothermal field
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(Table 4) Isotopic composition of sulfur and organic carbon in sulfide ores from hydrothermal fields at the axis of the East Pacific Rise near 9°50'N
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(Table 3) Isotopic composition of oxygen and hydrogen in seawater, interstitial water, and gas hydrate, area of the Haakon Mosby mud volcano
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(Table 10.4.3) Chemical composition, bacteria adundance, and rates of microbial processes in samples of hydrothermal fluids collected within the Rainbow hydrothermal field
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(Table 4) Radiocarbon datings of the authigenic carbonate buildup from Site AMK40-3745-M1-7
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(Table 7) Rates of microbiological processes in hot and warm solutions within hydrothermal fields at the axis of the East Pacific Rise near 9°50'N
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(Table 8.3.20) Chemical composition of carbonaceous samples from the caldera of the Haakon Mosby mud volcano, Norwegian Sea
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