Payros, Aitor; Ortiz, Silvia; Alegret, Laia; Orue-Etxebarria, Xabier; Apellaniz, Estibaliz; Molina, Eustoquio (2012): (Table S3) Clay mineral analysis from the Gorrondatxe section hemipelagic deposits [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.826204, In supplement to: Payros, A et al. (2012): An early Lutetian carbon-cycle perturbation: Insights from the Gorrondatxe section (western Pyrenees, Bay of Biscay). Paleoceanography, 27(2), PA2213, https://doi.org/10.1029/2012PA002300
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Coverage:
Latitude: 43.380000 * Longitude: -3.017000
Minimum SECTION, height: 2.0 m * Maximum SECTION, height: 200.0 m
Event(s):
Comment:
Clay minerals of size fraction <2 µm.
Parameter(s):
# | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
---|---|---|---|---|---|---|
1 | Lithologic unit/sequence | Unit | Payros, Aitor | |||
2 | SECTION, height | Section | m | Geocode | ||
3 | Smectite | Sme | % | Payros, Aitor | X-ray diffraction (XRD) | |
4 | Illite | Ill | % | Payros, Aitor | X-ray diffraction (XRD) | |
5 | Kaolinite | Kln | % | Payros, Aitor | X-ray diffraction (XRD) | |
6 | Chlorite | Chl | % | Payros, Aitor | X-ray diffraction (XRD) | |
7 | Weathering Index | W.I. | Payros, Aitor | |||
8 | Humidity index | Humidity index | Payros, Aitor |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
364 data points
Data
1 Unit | 2 Section [m] | 3 Sme [%] | 4 Ill [%] | 5 Kln [%] | 6 Chl [%] | 7 W.I. | 8 Humidity index |
---|---|---|---|---|---|---|---|
A | 2.0 | 58 | 34 | 0 | 8 | 0.72 | 0.00 |
A | 10.0 | 42 | 43 | 0 | 15 | 1.38 | 0.00 |
A | 17.1 | 55 | 39 | 0 | 6 | 0.82 | 0.00 |
A | 18.0 | 69 | 26 | 0 | 5 | 0.45 | 0.00 |
A | 22.1 | 49 | 42 | 6 | 3 | 0.82 | 0.12 |
A | 23.4 | 52 | 38 | 5 | 5 | 0.75 | 0.10 |
A | 27.7 | 50 | 40 | 6 | 4 | 0.76 | 0.12 |
A | 28.3 | 42 | 48 | 7 | 3 | 1.04 | 0.17 |
A | 32.2 | 42 | 49 | 6 | 3 | 1.08 | 0.14 |
A | 33.0 | 49 | 36 | 11 | 4 | 0.67 | 0.23 |
A | 36.0 | 44 | 39 | 13 | 4 | 0.75 | 0.29 |
A | 43.0 | 37 | 42 | 17 | 4 | 0.85 | 0.46 |
A | 52.0 | 36 | 47 | 11 | 6 | 1.13 | 0.31 |
A | 60.0 | 50 | 41 | 5 | 4 | 0.82 | 0.10 |
A | 65.5 | 38 | 46 | 12 | 4 | 1.00 | 0.32 |
A | 70.0 | 43 | 39 | 18 | 0 | 0.64 | 0.42 |
A | 71.0 | 37 | 41 | 14 | 8 | 0.96 | 0.38 |
A | 75.0 | 35 | 42 | 23 | 0 | 0.72 | 0.66 |
A | 76.5 | 34 | 39 | 21 | 6 | 0.82 | 0.62 |
A | 81.0 | 33 | 40 | 24 | 3 | 0.75 | 0.73 |
A | 84.0 | 35 | 41 | 24 | 0 | 0.69 | 0.66 |
A | 87.0 | 45 | 39 | 0 | 16 | 1.22 | 0.00 |
A | 91.0 | 34 | 44 | 20 | 2 | 0.85 | 0.59 |
A | 94.0 | 36 | 40 | 8 | 16 | 1.27 | 0.22 |
A | 100.0 | 43 | 36 | 11 | 10 | 0.85 | 0.26 |
A | 105.0 | 41 | 36 | 12 | 11 | 0.87 | 0.29 |
A | 108.0 | 48 | 36 | 10 | 6 | 0.72 | 0.21 |
A | 110.0 | 39 | 43 | 8 | 10 | 1.13 | 0.21 |
A | 111.0 | 45 | 48 | 4 | 3 | 1.04 | 0.09 |
A | 115.0 | 52 | 38 | 0 | 10 | 0.92 | 0.00 |
B | 119.0 | 27 | 41 | 28 | 4 | 0.82 | 1.04 |
B | 119.2 | 34 | 41 | 22 | 3 | 0.78 | 0.65 |
B | 119.4 | 35 | 42 | 20 | 3 | 0.82 | 0.57 |
B | 120.0 | 29 | 42 | 25 | 4 | 0.85 | 0.86 |
B | 122.0 | 35 | 37 | 25 | 3 | 0.67 | 0.71 |
B | 124.0 | 9 | 56 | 30 | 5 | 1.56 | 3.33 |
B | 124.2 | 18 | 53 | 22 | 7 | 1.50 | 1.22 |
B | 125.0 | 27 | 42 | 26 | 5 | 0.89 | 0.96 |
B | 126.0 | 27 | 42 | 26 | 5 | 0.89 | 0.96 |
B | 129.0 | 18 | 48 | 24 | 10 | 1.38 | 1.33 |
B | 131.0 | 23 | 45 | 23 | 9 | 1.17 | 1.00 |
C | 135.0 | 36 | 48 | 10 | 6 | 1.17 | 0.28 |
C | 138.0 | 32 | 46 | 19 | 3 | 0.96 | 0.59 |
C | 142.0 | 32 | 42 | 19 | 7 | 0.96 | 0.58 |
C | 146.0 | 32 | 44 | 19 | 5 | 0.96 | 0.59 |
D | 150.0 | 46 | 47 | 2 | 5 | 1.08 | 0.04 |
D | 165.0 | 53 | 36 | 4 | 7 | 0.75 | 0.08 |
D | 169.0 | 46 | 52 | 0 | 2 | 1.17 | 0.00 |
D | 174.0 | 49 | 49 | 0 | 2 | 1.04 | 0.00 |
D | 180.0 | 51 | 45 | 0 | 4 | 0.96 | 0.00 |
D | 190.0 | 62 | 37 | 0 | 1 | 0.61 | 0.00 |
D | 200.0 | 54 | 42 | 0 | 4 | 0.85 | 0.00 |