Henry, Pierre; Kanamatsu, Toshiya; Moe, Kyaw Thu; Expedition 333 Scientists (2012): Visual core description (VCD) from IODP Hole 333-C0011C [dataset]. SIO7 Data Center, J-CORES Database; Ocean Drilling Program, Center for Deep Earth Exploration (JAMSTEC), PANGAEA, https://doi.org/10.1594/PANGAEA.784665
Always quote citation above when using data! You can download the citation in several formats below.
Related to:
Henry, Pierre; Kanamatsu, Toshiya; Moe, Kyaw Thu; Expedition 333 Scientists (2011): NanTroSEIZE Stage 2: subduction inputs 2 and heat flow. Washington, DC (Integrated Ocean Drilling Program Management International, Inc.), 333, https://doi.org/10.2204/iodp.pr.333.2011
IODP/CDEX (2012): SIO7 Data Center, J-CORES Database. Ocean Drilling Program, Center for Deep Earth Exploration, Japan Agency for Marine-Earth Science and Technology, Yokohama Kanagawa 236-0001, JAPAN, https://www.jamstec.go.jp/sio7/j-cores.data/315/C0001H/
Other version:
IODP Hole 333-C0011C, snapshot taken on 2012-05-08, J-CORES, SIO7 Data Center [dataset]. https://www.jamstec.go.jp/sio7/j-cores.data/333/C0011C/
Project(s):
Coverage:
Latitude: 32.829060 * Longitude: 136.882083
Minimum DEPTH, sediment/rock: 0.000 m * Maximum DEPTH, sediment/rock: 13.000 m
Event(s):
Comment:
Geocode = [m CSF-A] Top Core depth (below sea floor)
Parameter(s):
# | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
---|---|---|---|---|---|---|
1 | Sample code/label | Sample label | Expedition 333 Scientists | DSDP/ODP/IODP sample designation | Sample top | |
2 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
3 | Depth, top/min | Depth top | m | Expedition 333 Scientists | [m CSF-B] Top Core depth (below sea floor) | |
4 | Sample code/label 2 | Sample label 2 | Expedition 333 Scientists | DSDP/ODP/IODP sample designation | Sample bottom | |
5 | Depth, bottom/max | Depth bot | m | Expedition 333 Scientists | [m CSF-A] Bottom Core depth (below sea floor) | |
6 | Depth, bottom/max | Depth bot | m | Expedition 333 Scientists | [m CSF-B] Bottom Core depth (below sea floor) | |
7 | Main Lithology | Main lith | Expedition 333 Scientists | Visual description | Sedimentological comment on Core | |
8 | Lithology/composition/facies | Lithology | Expedition 333 Scientists | Visual description | Sedimentological comment on Section | |
9 | Lithology/composition/facies | Lithology | Expedition 333 Scientists | Visual description | Continued | |
10 | Time Stamp | Time Stamp | Expedition 333 Scientists |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
101 data points
Data
1 Sample label (Sample top, DSDP/ODP/IODP sam...) | 2 Depth sed [m] | 3 Depth top [m] ([m CSF-B] Top Core depth (bel...) | 4 Sample label 2 (Sample bottom, DSDP/ODP/IODP ...) | 5 Depth bot [m] ([m CSF-A] Bottom Core depth (...) | 6 Depth bot [m] ([m CSF-B] Bottom Core depth (...) | 7 Main lith (Sedimentological comment on C...) | 8 Lithology (Sedimentological comment on S...) | 9 Lithology (Continued, Visual description) | 10 Time Stamp |
---|---|---|---|---|---|---|---|---|---|
333-C0011C-1H-1,0.0 | 0.000 | 0.000 | 333-C0011C-1H-CC,31.5 | 3.645 | 3.495 | A succession of hemipelagic sediments on top (in the first Section), then mixed sediments inferred to be five MTDs to the lower part of section 5, beneath which is hemipelagic clay. | 2011-01-06T13:13:16 | ||
333-C0011C-1H-1,0.0 | 0.000 | 0.000 | 333-C0011C-1H-1,62.5 | 0.625 | 0.599 | Hemipelagic sediments, olice brown sandy clay (youngest), dark grayish yellow clay and green sandy clay at the base. | 2010-12-20T20:33:41 | ||
333-C0011C-1H-3,0.0 | 0.845 | 0.810 | 333-C0011C-1H-3,101.5 | 1.860 | 1.784 | A succession of sandy clay which can be separated into three intervalls based on differences in color. Irregular lower boundaries, color mottling and banding indicates that this may be reworked sediments, i.e. MTDs, later affected by bioturbation. | 2010-12-20T20:40:30 | ||
333-C0011C-1H-5,0.0 | 2.075 | 1.990 | 333-C0011C-1H-5,125.5 | 3.330 | 3.193 | A succession of clay which can be separated into three intervalls based on differences in color. Irregular lower boundaries of the upper two intervalls indicates that these sediments may have been reworked (MTDs) and later affected by bioturbation. | Both do comprise seemingly undisturbed ash layers. Lower interval is probably hemipelagic sediments. | 2010-12-20T21:15:14 | |
333-C0011C-1H-CC,0.0 | 3.330 | 3.193 | 333-C0011C-1H-CC,31.5 | 3.645 | 3.495 | Yellow gray hemipelagic clay affected by slight - moderate bioturbation. | 2010-12-20T21:17:40 | ||
333-C0011C-2H-1,0.0 | 3.500 | 3.500 | 333-C0011C-2H-CC,41.0 | 13.390 | 13.390 | Dark greenish gray clay with a number of thin sand and/or silt layers, frequent color mottling, patches of ash and a few ash layers. Hemipelagic clay, moderately bioturbated, with a number of thin turbiditic sand/silt layers and a few ash layers. | 2011-01-06T13:13:40 | ||
333-C0011C-2H-1,0.0 | 3.500 | 3.500 | 333-C0011C-2H-1,118.0 | 4.680 | 4.680 | Dark greenish gray clay with a number of thin sand/silt layers and a pink ash layer. Hemipelagic sediments, normally bioturbated, with a numer of thin turbiditic sands. Smear slides at 30 and 80 cm. | 2010-12-21T02:42:05 | ||
333-C0011C-2H-3,0.0 | 4.890 | 4.835 | 333-C0011C-2H-3,142.0 | 6.310 | 6.310 | Dominantly dark greenish gray clay with a number of thin sand/silt layers and a yellowish -gray interval from 16 - 48 cm depth. Frequent color mottling. Hemipelagic sediments with a number of this turbiditic sands. | 2010-12-21T02:41:44 | ||
333-C0011C-2H-4,0.0 | 6.310 | 6.199 | 333-C0011C-2H-4,121.0 | 7.520 | 7.520 | Dark greenish gray clay with a number of thin sand/silt layers and frequent color mottling and some outsized clasts. Hemipelagic sediments, moderately bioturbated, with a number of thin, turbiditic sand layers. | 2010-12-21T02:41:32 | ||
333-C0011C-2H-7,0.0 | 9.145 | 8.922 | 333-C0011C-2H-7,120.0 | 10.345 | 10.345 | Dark greenish gray clay - sandy clay with a number of thin sand/silt layers, frequent color mottling, patches of ash and an ash layer at 44.5 - 47.5 cm. | Hemipelagic sediments, moderately bioturbated, with a number of thin turbiditic sands and an ash layer. | 2010-12-21T02:40:51 | |
333-C0011C-2H-9,0.0 | 10.555 | 10.277 | 333-C0011C-2H-9,120.0 | 11.755 | 11.755 | Dark greenish gray clay with a number of thin sand/silt layers, frequent color mottling and a ash layer at 99-102 cm.Hemipelagic clay, moderately bioturbated, with a number of thin turbiditic sands and a black ash layer. | Smear slide at 48 cm and 101 cm. | 2010-12-21T02:40:30 | |
333-C0011C-2H-11,0.0 | 11.975 | 11.641 | 333-C0011C-2H-11,100.5 | 12.980 | 12.980 | Dark greenish gray clay with a number of thin sand/silt layers, frequent color mottling and patches of ash. hemipelagic sediments, moderately bioturbated with a number of thin turbiditic sands. | 2010-12-21T02:40:11 | ||
333-C0011C-2H-CC,0.0 | 12.980 | 12.606 | 333-C0011C-2H-CC,41.0 | 13.390 | 13.390 | Hemipelagic sediments, moderately bioturbated. | 2010-12-21T00:15:11 | ||
333-C0011C-3H-1,0.0 | 13.000 | 13.000 | 333-C0011C-3H-CC,40.0 | 23.110 | 23.110 | Succession of clay and silty clasy with intercalated volcanic ash and sand. Some significant bioturbation at places. Scattered pumice and isolated mud clasts. | 2010-12-21T07:50:53 |