Tamborrino, Leonardo; Gualtieri, Alessandro F (2019): X-ray diffraction (XRD) measurements of rock-sediment sample GeoB11319-1 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.902242, In supplement to: Tamborrino, Leonardo; Himmler, Tobias; Elvert, Marcus; Conti, Daniel; Gualtieri, Alessandro F; Fontana, Daniela; Bohrmann, Gerhard (2019): Formation of tubular carbonate conduits at Athina mud volcano, eastern Mediterranean Sea. Marine and Petroleum Geology, 107, 20-31, https://doi.org/10.1016/j.marpetgeo.2019.05.003
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Project(s):
Coverage:
Latitude: 35.387983 * Longitude: 30.210733
Date/Time Start: 2006-12-04T00:00:00 * Date/Time End: 2006-12-04T13:52:00
Event(s):
GeoB11319-1 * Latitude: 35.387983 * Longitude: 30.210733 * Date/Time Start: 2006-12-04T00:00:00 * Date/Time End: 2006-12-04T13:52:00 * Location: Athina Mud Volcano * Campaign: M70/3 * Basis: Meteor (1986) * Method/Device: Rock sample (ROCK) * Comment: The sample was collected with an arm of the ROV MARUM QUEST.
Comment:
Sample powders for X-ray diffraction (XRD) and for stable isotope measurements were obtained from surfaces of the polished slabs, using a handheld microdrill. The XRD measurements were performed on a X'PERT PRO diffractometer equipped with a copper anode λ=1.54 Å at 40 mA and 40 kV current. Qualitative and quantitative analyses were carried out applying the Rietveld method using EXPGUI-GSAS (Rietveld, 1969; Larson and von Dreele, 1994; Toby, 2001). The accuracy was estimated±1 wt.-%. The Mg-content in calcite was determined using the method of Titschack et al. (2011).Values in parentheses represent the deviation in units of last digits. Rp, Rwp and χ2 are agreement factors indicative of the goodness of the Rietweld analyses (Toby, 2006)
Parameter(s):
License:
Creative Commons Attribution 4.0 International (CC-BY-4.0)
Size:
204 data points
Data
| 1 Sample ID | 2 Lithology | 3 Arg [%] | 4 Arg std dev [±] | 5 Cal [%] | 6 Cal std dev [±] | 7 Kut [%] | 8 Kut std dev [±] | 9 Mg-Cal [%] | 10 Mg-Cal std dev [±] | 11 Qz [%] | 12 Qz std dev [±] | 13 Pl [%] | 14 Pl std dev [±] | 15 Hl [%] | 16 Hl std dev [±] | 17 Kln [%] | 18 Kln std dev [±] | 19 Mica [%] (Mica e/o Illite) | 20 Mica std dev [±] | 21 Clc [%] | 22 Clc std dev [±] | 23 Crs [%] | 24 Mg [%] (Mg content (mol%)) | 25 Mg std dev [±] | 26 factor (wRp) | 27 factor (X^2) | 28 factor (Rp) |
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| A1 | Detrital infilling | 6.6 | 0.1 | 10.4 | 0.1 | 1.6 | 0.1 | 76.6 | 0.1 | 2.9 | 0.1 | 1.8 | 0.2 | 0.1 | 10.1 | 0.7 | 0.0570 | 2.602 | 0.0423 | ||||||||
| 0-A1 | Detrital infilling | 12.9 | 0.2 | 25.7 | 0.2 | 4.6 | 0.1 | 28.5 | 0.3 | 7.8 | 0.1 | 4 | 0.2 | 0.5 | 0.1 | 8.4 | 0.2 | 7.5 | 0.3 | 5.2 | 2.2 | 0.0439 | 2.747 | 0.0325 | |||
| 0-A2 | Micrite | 4.1 | 0.1 | 6.1 | 0.1 | 12.9 | 0.1 | 72.6 | 0.1 | 2.1 | 0.1 | 2.2 | 0.2 | 17.1 | 0.7 | 0.0642 | 3.595 | 0.0488 | |||||||||
| 0-A3 | Micrite | 9.1 | 0.1 | 6.8 | 0.2 | 18.4 | 0.2 | 63.7 | 0.2 | 1.9 | 0.1 | 14.8 | 1.0 | 0.0585 | 4.036 | 0.0418 | |||||||||||
| 0-A4 | Micrite | 3.2 | 0.1 | 6.8 | 0.2 | 16.3 | 0.2 | 72.6 | 0.1 | 1.1 | 0.1 | 12.2 | 9.0 | 0.0642 | 5.311 | 0.4450 | |||||||||||
| 0-A5 | Micrite | 2.4 | 0.1 | 8.1 | 0.2 | 25.2 | 0.2 | 63.5 | 0.3 | 0.7 | 0.1 | 15.6 | 1.2 | 0.0515 | 2.637 | 0.0374 | |||||||||||
| 0-A6 | Micrite | 3.6 | 0.1 | 6.1 | 0.2 | 22.2 | 0.2 | 66.7 | 0.2 | 1.4 | 0.1 | 11.8 | 1.1 | 0.0694 | 5.422 | 0.0494 | |||||||||||
| B1 | Micrite | 11.4 | 0.1 | 6.3 | 0.2 | 24.6 | 0.2 | 56.7 | 0.2 | 0.9 | 0.1 | 20.9 | 1.2 | 0.0662 | 5.773 | 0.0474 | |||||||||||
| F1 | Micrite | 31.5 | 0.1 | 7.3 | 0.2 | 13.9 | 0.2 | 45.4 | 0.3 | 1.0 | 0.1 | 0.9 | 0.2 | 11.1 | 1.6 | 0.0654 | 5.291 | 0.0433 | |||||||||
| F2 | Micrite | 16.5 | 0.1 | 8.2 | 0.1 | 12.4 | 0.1 | 58.5 | 0.1 | 1.9 | 0.1 | 2.4 | 0.2 | 15.0 | 0.8 | 0.0626 | 3.430 | 0.0466 | |||||||||
| F3 | Micrite | 11.1 | 0.1 | 6.9 | 0.2 | 17.7 | 0.2 | 63.2 | 0.2 | 1.1 | 0.1 | 17.9 | 1.0 | 0.0568 | 3.896 | 0.0405 |