Blum, Peter; Mix, Alan C; Tiedemann, Ralf; Shipboard Scientific Party (2005): Smear slide investigation on ODP Hole 202-1232A [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.257761
Always quote citation above when using data! You can download the citation in several formats below.
Related to:
Mix, Alan C; Tiedemann, Ralf; Blum, Peter; et al. (2003): Proceedings of the Ocean Drilling Program, 202 Initial Reports. Proceedings of the Ocean Drilling Program, Ocean Drilling Program, 202, online, https://doi.org/10.2973/odp.proc.ir.202.2003
ODP/TAMU (2005): JANUS Database. Ocean Drilling Program, Texas A&M University, College Station TX 77845-9547, USA; (data copied from Janus 2005-02 to 2005-06), http://www-odp.tamu.edu/database/
Project(s):
Ocean Drilling Program (ODP)
Coverage:
Latitude: -39.891160 * Longitude: -75.901360
Date/Time Start: 2002-04-07T11:00:00 * Date/Time End: 2002-04-10T16:25:00
Minimum DEPTH, sediment/rock: 0.750 m * Maximum DEPTH, sediment/rock: 354.670 m
Event(s):
202-1232A * Latitude: -39.891160 * Longitude: -75.901360 * Date/Time Start: 2002-04-07T11:00:00 * Date/Time End: 2002-04-10T16:25:00 * Elevation: -4078.6 m * Penetration: 371.3 m * Recovery: 288.77 m * Location: South Pacific Ocean * Campaign: Leg202 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 39 cores; 371.3 m cored; 0 m drilled; 77.8 % recovery
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
| 2 | Depth, composite | Depth comp | mcd | Shipboard Scientific Party | ||
| 3 | Sample code/label | Sample label | Shipboard Scientific Party | DSDP/ODP/IODP sample designation | ||
| 4 | Lithology/composition/facies | Lithology | Shipboard Scientific Party | Smear slide analysis | ||
| 5 | Sand | Sand | Shipboard Scientific Party | Smear slide analysis | ||
| 6 | Silt | Silt | Shipboard Scientific Party | Smear slide analysis | ||
| 7 | Clay | Clay | Shipboard Scientific Party | Smear slide analysis | ||
| 8 | Diatom abundance | Diatom abund | Shipboard Scientific Party | Smear slide analysis | ||
| 9 | Foraminifera | Foram | Shipboard Scientific Party | Smear slide analysis | ||
| 10 | Nannofossil abundance | Nannos abund | Shipboard Scientific Party | Smear slide analysis | ||
| 11 | Pollen | Pollen | Shipboard Scientific Party | Smear slide analysis | ||
| 12 | Radiolarians abundance | Rad abund | Shipboard Scientific Party | Smear slide analysis | ||
| 13 | Silicoflagellate abundance | Silicoflag abund | Shipboard Scientific Party | Smear slide analysis | ||
| 14 | Amphibole | Amp | Shipboard Scientific Party | Smear slide analysis | ||
| 15 | Clay minerals | Clay min | Shipboard Scientific Party | Smear slide analysis | ||
| 16 | Clinopyroxene | Cpx | Shipboard Scientific Party | Smear slide analysis | ||
| 17 | Feldspar | Fsp | Shipboard Scientific Party | Smear slide analysis | ||
| 18 | Garnet | Grt | Shipboard Scientific Party | Smear slide analysis | ||
| 19 | Glauconite | Glt | Shipboard Scientific Party | Smear slide analysis | ||
| 20 | Heavy minerals | HM | Shipboard Scientific Party | Smear slide analysis | ||
| 21 | Calcite, inorganic | Cal inorg | Shipboard Scientific Party | Smear slide analysis | ||
| 22 | Mica | Mica | Shipboard Scientific Party | Smear slide analysis | ||
| 23 | Opaque minerals | Opaque | Shipboard Scientific Party | Smear slide analysis | ||
| 24 | Orthopyroxene | Opx | Shipboard Scientific Party | Smear slide analysis | ||
| 25 | Palagonite | Palagonite | Shipboard Scientific Party | Smear slide analysis | ||
| 26 | Quartz | Qz | Shipboard Scientific Party | Smear slide analysis | ||
| 27 | Rutile | Rt | Shipboard Scientific Party | Smear slide analysis | ||
| 28 | Titanite | Ttn | Shipboard Scientific Party | Smear slide analysis | ||
| 29 | Volcanic glass | Volc glass | Shipboard Scientific Party | Smear slide analysis | ||
| 30 | Zircon | Zrn | Shipboard Scientific Party | Smear slide analysis | ||
| 31 | Micrite | Micrite | Shipboard Scientific Party | Smear slide analysis | ||
| 32 | Volcanic fragments | Volc fragm | Shipboard Scientific Party | Smear slide analysis | volcanic fragm | |
| 33 | Comment | Comment | Shipboard Scientific Party |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
1680 data points
Data
| 1 Depth sed [m] | 2 Depth comp [mcd] | 3 Sample label | 4 Lithology | 5 Sand | 6 Silt | 7 Clay | 8 Diatom abund | 9 Foram | 10 Nannos abund | 11 Pollen | 12 Rad abund | 13 Silicoflag abund | 14 Amp | 15 Clay min | 16 Cpx | 17 Fsp | 18 Grt | 19 Glt | 20 HM | 21 Cal inorg | 22 Mica | 23 Opaque | 24 Opx | 25 Palagonite | 26 Qz | 27 Rt | 28 Ttn | 29 Volc glass | 30 Zrn | 31 Micrite | 32 Volc fragm | 33 Comment |
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| 0.750 | 6.690 | 202-1232A-1H-1,75 | D | 35 | 0 | 65 | R | R | R | 23 | 54 | 8 | R | 15 | R | |||||||||||||||||
| 3.760 | 9.700 | 202-1232A-1H-3,75 | D | 85 | 15 | 2 | R | 2 | R | 82 | 10 | R | R | 2 | R | |||||||||||||||||
| 5.360 | 11.300 | 202-1232A-1H-4,84 | D | 83 | 17 | 3 | R | 1 | R | R | 69 | 21 | R | 1 | R | 4 | R | R | ||||||||||||||
| 5.460 | 11.400 | 202-1232A-1H-4,94 | D | 91 | 9 | 2 | R | R | R | 82 | 16 | R | R | R | R | R | R | |||||||||||||||
| 7.020 | 12.960 | 202-1232A-1H-5,100 | M | 72 | 28 | 2 | R | 67 | R | 26 | R | 2 | 2 | R | R | |||||||||||||||||
| 7.160 | 13.100 | 202-1232A-1H-5,114 | M | 14 | 3 | 83 | R | R | R | 58 | R | 19 | 4 | 8 | R | 12 | ||||||||||||||||
| 7.240 | 13.180 | 202-1232A-1H-5,122 | M | 8 | 17 | 75 | R | R | R | 80 | R | 12 | R | R | 8 | R | R | R | R | Plagioclase=Andesine | ||||||||||||
| 19.250 | 23.530 | 202-1232A-3H-1,75 | D | 67 | 33 | 3 | R | 1 | R | R | 67 | 20 | 4 | 1 | 4 | R | ||||||||||||||||
| 20.940 | 25.220 | 202-1232A-3H-2,95 | D | 82 | 2 | 16 | 1 | R | R | 72 | 22 | 3 | R | 1 | R | R | ||||||||||||||||
| 22.250 | 26.530 | 202-1232A-3H-3,75 | D | 73 | 27 | R | R | 60 | 30 | 3 | 2 | 5 | R | R | ||||||||||||||||||
| 27.750 | 33.130 | 202-1232A-4H-1,75 | D | 62 | 38 | 2 | R | 61 | R | 30 | 1 | 1 | 4 | R | R | |||||||||||||||||
| 30.770 | 36.150 | 202-1232A-4H-3,75 | D | 62 | 0 | 38 | 1 | 1 | 1 | R | 58 | R | 29 | R | 3 | R | 6 | R | R | |||||||||||||
| 32.450 | 37.830 | 202-1232A-4H-4,90 | M | 77 | 0 | 23 | 3 | R | 4 | 3 | R | R | 66 | R | 13 | R | 7 | R | 4 | R | ||||||||||||
| 33.560 | 38.940 | 202-1232A-4H-5,50 | D | 71 | 0 | 29 | 2 | R | 4 | 2 | R | R | 60 | R | 18 | R | 6 | R | 6 | R | ||||||||||||
| 45.280 | 50.710 | 202-1232A-5H-6,119 | M | 20 | 40 | 40 | 1 | 20 | R | 68 | 4 | 3 | R | 4 | Plagioclase=Andesine | |||||||||||||||||
| 45.860 | 51.290 | 202-1232A-5H-7,26 | D | 77 | 0 | 23 | R | R | 3 | R | R | 74 | R | 15 | R | 4 | R | 4 | R | |||||||||||||
| 46.750 | 60.400 | 202-1232A-6H-1,75 | D | 71 | 0 | 29 | R | 1 | R | 1 | 67 | R | 20 | 3 | 4 | R | 4 | |||||||||||||||
| 49.780 | 63.430 | 202-1232A-6H-3,75 | D | 67 | 0 | 33 | R | 1 | R | 2 | 60 | R | 24 | 4 | 2 | R | 6 | R | ||||||||||||||
| 56.250 | 71.860 | 202-1232A-7H-1,75 | D | 77 | 0 | 23 | R | R | R | 1 | 71 | R | 19 | 1 | 3 | R | 3 | 1 | ||||||||||||||
| 59.720 | 75.330 | 202-1232A-7H-3,121 | M | 81 | 19 | R | R | 35 | R | 23 | R | R | 7 | R | 35 | Plagioclase=Labradorite | ||||||||||||||||
| 60.780 | 76.390 | 202-1232A-7H-4,75 | D | 83 | 0 | 17 | 4 | 2 | 2 | 75 | R | 7 | 2 | 3 | R | 3 | 2 | 3 | 2 | |||||||||||||
| 62.360 | 77.970 | 202-1232A-7H-5,82 | M | 57 | 43 | R | R | 60 | 24 | R | R | 16 | R | R | Plagioclase=Labradorite | |||||||||||||||||
| 65.750 | 82.050 | 202-1232A-8H-1,75 | D | 70 | 7 | 23 | 4 | 4 | R | R | 63 | R | 15 | 6 | R | 2 | 4 | R | 2 | |||||||||||||
| 68.770 | 85.070 | 202-1232A-8H-3,75 | D | 84 | 16 | 5 | R | R | 77 | R | 11 | R | R | 3 | R | 2 | 3 | R | R | |||||||||||||
| 69.020 | 85.320 | 202-1232A-8H-3,100 | D | 67 | 33 | 1 | 1 | R | R | 65 | R | 26 | 1 | 1 | 4 | R | R | R | ||||||||||||||
| 69.880 | 86.180 | 202-1232A-8H-4,35 | D | 94 | 6 | 7 | R | R | R | 72 | R | 7 | R | R | 4 | R | 2 | 3 | R | R | ||||||||||||
| 72.520 | 88.820 | 202-1232A-8H-5,147 | M | 86 | 14 | R | R | R | R | 57 | R | 23 | R | 5 | 16 | R | R | Plagioclase=Labradorite | ||||||||||||||
| 75.250 | 91.730 | 202-1232A-9H-1,75 | D | 100 | R | 7 | 57 | R | 36 | R | R | |||||||||||||||||||||
| 78.260 | 94.740 | 202-1232A-9H-3,75 | D | 83 | 17 | 2 | R | R | R | 78 | R | 11 | 2 | R | 3 | 3 | R | R | ||||||||||||||
| 81.670 | 98.150 | 202-1232A-9H-5,114 | M | 0 | 40 | 60 | R | 2 | 71 | 17 | R | 5 | 5 | R | R | R | ||||||||||||||||
| 84.750 | 101.230 | 202-1232A-10H-1,75 | D | 77 | 0 | 23 | 2 | R | 77 | R | 15 | R | 3 | R | R | 3 | ||||||||||||||||
| 87.780 | 104.260 | 202-1232A-10H-3,75 | M | 55 | 9 | 36 | 2 | 58 | R | 19 | 2 | 6 | R | 6 | 6 | 2 | ||||||||||||||||
| 90.660 | 107.140 | 202-1232A-10H-5,60 | D | 83 | 0 | 17 | R | R | R | 79 | R | 16 | R | 2 | R | 2 | 2 | R | ||||||||||||||
| 94.250 | 110.730 | 202-1232A-11H-1,75 | D | 77 | 0 | 23 | R | R | R | R | 77 | R | 15 | R | 3 | R | 2 | 3 | R | |||||||||||||
| 97.260 | 113.740 | 202-1232A-11H-3,75 | D | 77 | 0 | 23 | R | R | R | R | 77 | R | 15 | R | 3 | R | 3 | 2 | ||||||||||||||
| 97.730 | 114.210 | 202-1232A-11H-3,122 | M | 0 | 14 | 86 | 3 | R | 63 | 3 | 9 | R | 6 | 9 | 6 | ´From brownish ´´turbidite´´´ | ||||||||||||||||
| 100.265 | 116.745 | 202-1232A-11H-5,73.5 | M | 80 | 0 | 20 | 60 | R | 30 | R | 6 | 1 | R | R | 1 | 1 | Sample comes from a nodule | |||||||||||||||
| 103.750 | 120.510 | 202-1232A-12H-1,75 | D | 77 | 0 | 23 | R | R | R | 75 | R | 15 | R | 3 | R | 1 | 4 | 1 | Plagioclase=Labradorita | |||||||||||||
| 106.780 | 123.540 | 202-1232A-12H-3,75 | D | 77 | 0 | 23 | R | 4 | R | R | 74 | R | 15 | R | 3 | R | R | 3 | 1 | |||||||||||||
| 108.760 | 125.520 | 202-1232A-12H-4,121 | D | 57 | 0 | 43 | R | R | R | 1 | 55 | R | 27 | 1 | 4 | R | 1 | 7 | 3 | |||||||||||||
| 109.520 | 126.280 | 202-1232A-12H-5,45 | M | 80 | 0 | 20 | 3 | 63 | 3 | R | 25 | R | 4 | R | 1 | R | R | 1 | 1 | Sample comes from brownish nodule | ||||||||||||
| 113.250 | 130.460 | 202-1232A-13X-1,75 | D | 80 | 2 | 18 | 3 | 2 | R | 70 | R | 20 | 1 | 1 | R | 2 | 1 | Fixed sample | ||||||||||||||
| 114.480 | 131.690 | 202-1232A-13X-2,48 | D | 80 | 0 | 20 | 1 | 75 | 18 | 1 | 1 | 2 | R | |||||||||||||||||||
| 116.250 | 133.460 | 202-1232A-13X-3,75 | D | 65 | 5 | 30 | 3 | R | 2 | 1 | 60 | R | 27 | R | 1 | 1 | R | 3 | 1 | Fixed sample | ||||||||||||
| 116.460 | 133.670 | 202-1232A-13X-3,96 | M | 60 | 10 | 30 | R | 60 | 25 | 10 | R | 1 | R | taken in diffuse mottled light brown sediment | ||||||||||||||||||
| 119.670 | 136.880 | 202-1232A-13X-5,114 | M | 15 | 25 | 60 | 3 | 15 | 1 | 65 | R | R | 3 | 5 | 1 | R | 5 | 5 | Very base of graded layer | |||||||||||||
| 131.650 | 148.860 | 202-1232A-15X-1,75 | D | 83 | 17 | R | R | 27 | R | 36 | 9 | R | 18 | |||||||||||||||||||
| 141.350 | 158.560 | 202-1232A-16X-1,75 | D | 77 | 23 | 1 | R | R | 66 | R | 26 | R | R | R | 3 | R | 1 | 1 | R | 1 | ||||||||||||
| 141.350 | 158.560 | 202-1232A-16X-1,75 | D | 77 | 23 | 1 | R | R | 66 | R | 26 | R | R | R | 3 | R | 1 | 1 | R | 1 | ||||||||||||
| 142.990 | 160.200 | 202-1232A-16X-2,89 | D | 97 | 3 | 8 | R | R | R | R | R | 77 | R | 5 | R | R | 5 | R | 3 | R | 3 | |||||||||||
| 160.650 | 177.860 | 202-1232A-18X-1,75 | D | 71 | 1 | 28 | R | R | 1 | 68 | 1 | 20 | R | R | R | R | 3 | 4 | R | 3 | ||||||||||||
| 162.660 | 179.870 | 202-1232A-18X-2,126 | M | 7 | 58 | 35 | R | 7 | R | R | R | 2 | 91 | |||||||||||||||||||
| 163.660 | 180.870 | 202-1232A-18X-3,75 | D | 81 | 19 | 6 | R | 6 | R | R | 60 | 10 | R | 4 | R | 4 | 4 | R | 2 | |||||||||||||
| 165.350 | 182.560 | 202-1232A-18X-4,94 | D | 83 | 17 | R | R | 3 | 88 | 6 | 3 | R | 3 | |||||||||||||||||||
| 170.250 | 187.460 | 202-1232A-19X-1,75 | D | 67 | 33 | R | R | 63 | R | 21 | R | 4 | R | 4 | 4 | R | 4 | |||||||||||||||
| 171.760 | 188.970 | 202-1232A-19X-2,75 | D | 88 | 12 | 4 | 4 | R | 58 | 12 | R | 8 | 4 | 4 | R | 8 | ||||||||||||||||
| 182.860 | 200.070 | 202-1232A-20X-3,66 | M | 67 | 33 | R | R | 39 | R | R | 17 | 17 | 28 | R | R | R | ||||||||||||||||
| 182.950 | 200.160 | 202-1232A-20X-3,75 | D | 76 | 3 | 21 | R | R | R | R | R | 63 | R | 21 | R | R | 4 | 4 | 8 | R | ||||||||||||
| 182.950 | 200.160 | 202-1232A-20X-3,75 | D | 71 | 5 | 24 | 3 | R | 56 | R | 28 | R | 3 | R | 3 | 6 | 3 | R | ||||||||||||||
| 189.550 | 206.760 | 202-1232A-21X-1,75 | D | 43 | 57 | R | R | 43 | R | 29 | R | R | 9 | R | 3 | 14 | R | 3 | R | |||||||||||||
| 192.540 | 209.750 | 202-1232A-21X-3,75 | M | 45 | 10 | 45 | R | R | R | R | 40 | 4 | 28 | R | 12 | 4 | 8 | R | 4 | R | ||||||||||||
| 198.600 | 215.810 | 202-1232A-22X-1,50 | D | 98 | 2 | 1 | R | 48 | R | R | R | 48 | R | 1 | R | 1 | R | R | R | R | R | |||||||||||
| 198.850 | 216.060 | 202-1232A-22X-1,75 | D | 87 | 2 | 11 | 1 | R | 63 | R | R | R | 30 | R | 3 | 2 | R | R | ||||||||||||||
| 201.860 | 219.070 | 202-1232A-22X-3,75 | D | 67 | 33 | 2 | R | 60 | R | 14 | R | R | 4 | R | 2 | 10 | R | 6 | R | |||||||||||||
| 208.450 | 225.660 | 202-1232A-23X-1,75 | D | 75 | 25 | R | R | R | 77 | R | 13 | R | R | R | R | 3 | R | 3 | ||||||||||||||
| 211.450 | 228.660 | 202-1232A-23X-3,75 | D | 88 | 0 | 12 | 5 | R | R | R | R | 79 | R | 8 | R | R | 3 | R | 3 | R | R | |||||||||||
| 218.050 | 235.260 | 202-1232A-24X-1,75 | D | 81 | 0 | 19 | 2 | R | 2 | R | R | 73 | R | 7 | R | 5 | 5 | 2 | R | 2 | ||||||||||||
| 227.650 | 244.860 | 202-1232A-25X-1,75 | D | 67 | 0 | 33 | R | 31 | R | 1 | 46 | R | 15 | R | R | 3 | 3 | R | ||||||||||||||
| 230.620 | 247.830 | 202-1232A-25X-3,75 | D | 60 | 0 | 40 | 4 | R | R | 58 | R | 29 | R | R | 4 | R | 2 | 4 | R | |||||||||||||
| 237.250 | 254.680 | 202-1232A-26X-1,75 | D | 71 | 0 | 29 | 4 | R | R | 68 | 20 | R | 3 | R | R | 3 | 1 | |||||||||||||||
| 240.220 | 257.650 | 202-1232A-26X-3,75 | D | 77 | 0 | 23 | 3 | R | R | 77 | 15 | R | R | 3 | R | R | 4 | R | ||||||||||||||
| 242.660 | 260.090 | 202-1232A-26X-5,19 | M | 80 | 0 | 20 | R | 65 | 3 | R | 26 | 4 | 1 | R | R | R | some aggregates of nanno-ooze | |||||||||||||||
| 246.850 | 264.510 | 202-1232A-27X-1,75 | D | 75 | 0 | 25 | R | R | 75 | R | 20 | R | R | R | R | R | ||||||||||||||||
| 249.840 | 267.500 | 202-1232A-27X-3,75 | D | 78 | 0 | 22 | 2 | 75 | 18 | R | 1 | R | 1 | greenish silt mineral ~5% euhedral mod relief | ||||||||||||||||||
| 251.550 | 269.210 | 202-1232A-27X-4,96 | M | 10 | 5 | 85 | 5 | 10 | R | 70 | R | 2 | 8 | R | 2 | 1 | well sorted 40-50 cm silt | |||||||||||||||
| 256.450 | 274.260 | 202-1232A-28X-1,75 | D | 73 | 27 | R | 8 | 68 | R | 17 | R | R | R | R | R | 3 | 2 | R | 2 | |||||||||||||
| 259.420 | 277.230 | 202-1232A-28X-3,75 | D | 100 | 42 | R | R | R | 2 | R | 52 | R | R | R | R | R | R | R | 2 | |||||||||||||
| 260.360 | 278.170 | 202-1232A-28X-4,20 | D | 90 | 5 | 5 | 5 | 3 | 50 | R | R | R | 33 | R | R | R | 2 | 5 | R | R | R | |||||||||||
| 266.050 | 284.170 | 202-1232A-29X-1,75 | D | 10 | 13 | 77 | R | 8 | R | R | 15 | R | 38 | R | R | 8 | 15 | R | R | 15 | R | R | R | R | ||||||||
| 269.040 | 287.160 | 202-1232A-29X-3,75 | D | 78 | 2 | 20 | R | R | R | 2 | 80 | R | 10 | R | R | 4 | R | R | 6 | R | R | R | ||||||||||
| 275.750 | 294.050 | 202-1232A-30X-1,75 | D | 75 | 2 | 23 | R | R | 72 | R | 14 | R | 3 | R | 3 | 7 | R | R | R | R | ||||||||||||
| 278.750 | 297.050 | 202-1232A-30X-3,75 | D | 67 | 33 | 3 | R | 60 | R | 22 | R | R | 4 | R | 1 | 7 | R | R | 1 | R | ||||||||||||
| 285.450 | 303.880 | 202-1232A-31X-1,75 | D | 75 | 0 | 25 | 7 | 70 | 15 | R | R | 5 | R | R | R | |||||||||||||||||
| 288.440 | 306.870 | 202-1232A-31X-3,75 | M | 81 | 19 | R | 14 | R | 41 | R | R | 14 | R | 5 | 27 | R | R | R | R | Plagioclase= Andesine | ||||||||||||
| 295.050 | 313.800 | 202-1232A-32X-1,75 | D | 83 | 0 | 17 | R | 2 | 85 | R | 8 | R | R | 2 | R | R | 2 | 2 | ||||||||||||||
| 298.040 | 316.790 | 202-1232A-32X-3,75 | D | 60 | 0 | 40 | R | R | R | 2 | 61 | R | 31 | R | R | 2 | R | R | 4 | R | ||||||||||||
| 304.650 | 323.600 | 202-1232A-33X-1,75 | D | 74 | 2 | 24 | R | 2 | 3 | R | R | 2 | 63 | R | 16 | R | 5 | R | 3 | 5 | R | R | 2 | R | R | |||||||
| 307.670 | 326.620 | 202-1232A-33X-3,75 | D | 71 | 0 | 29 | 1 | R | R | 71 | R | 21 | R | R | 1 | R | R | 3 | 1 | |||||||||||||
| 314.250 | 333.200 | 202-1232A-34X-1,75 | D | 55 | 9 | 36 | R | 2 | 3 | 2 | 50 | R | 25 | 2 | 5 | R | 2 | 8 | 2 | |||||||||||||
| 317.250 | 336.200 | 202-1232A-34X-3,75 | D | 35 | 12 | 53 | R | R | R | 2 | 42 | R | 32 | R | 2 | 4 | R | 2 | 15 | R | ||||||||||||
| 317.665 | 336.615 | 202-1232A-34X-3,116.5 | M | 50 | 0 | 50 | 1 | R | R | 14 | R | 10 | 1 | R | 1 | 71 | Mainly sand-sized volcanic glass | |||||||||||||||
| 317.840 | 336.790 | 202-1232A-34X-3,134 | M | 91 | 0 | 9 | R | R | R | R | 91 | R | 5 | R | 2 | R | R | 2 | R | Aggregates of clayey material | ||||||||||||
| 320.170 | 339.120 | 202-1232A-34X-5,66 | M | 91 | 0 | 9 | R | 4 | R | R | 88 | R | 5 | R | 2 | R | R | 2 | R | Aggregates of clayey material | ||||||||||||
| 354.670 | 374.290 | 202-1232A-38X-2,116 | M | 82 | 0 | 18 | R | 80 | 17 | R | 2 |