Takai, Ken; Mottl, Michael J; Nielsen, Simon Harder Holm; Expedition 331 Scientists (2012): Visual core description (VCD) from IODP Hole 331-C0014F [dataset]. SIO7 Data Center, J-CORES Database; Ocean Drilling Program, Center for Deep Earth Exploration (JAMSTEC), PANGAEA, https://doi.org/10.1594/PANGAEA.776810
Always quote citation above when using data! You can download the citation in several formats below.
Related to:
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/
Takai, Ken; Mottl, Michael J; Nielsen, Simon Harder Holm; Expedition 331 Scientists (2010): Integrated Ocean Drilling Program Expedition 331 Preliminary Report. Deep Hot Biosphere. Washington, DC (Integrated Ocean Drilling Program Management International, Inc.), 331, https://doi.org/10.2204/iodp.pr.331.2010
Other version:
IODP Hole 331-C0014F, snapshot taken on 2011-10-03, J-CORES, SIO7 Data Center [dataset]. https://www.jamstec.go.jp/sio7/j-cores.data/331/C0014F/
Project(s):
Coverage:
Latitude: 27.790308 * Longitude: 126.900738
Minimum DEPTH, sediment/rock: 0.000 m * Maximum DEPTH, sediment/rock: 3.225 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 331 Scientists | DSDP/ODP/IODP sample designation | Sample top | |
2 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
3 | Depth, top/min | Depth top | m | Expedition 331 Scientists | [m CSF-B] Top Core depth (below sea floor) | |
4 | Sample code/label 2 | Sample label 2 | Expedition 331 Scientists | DSDP/ODP/IODP sample designation | Sample bottom | |
5 | Depth, bottom/max | Depth bot | m | Expedition 331 Scientists | [m CSF-A] Bottom Core depth (below sea floor) | |
6 | Depth, bottom/max | Depth bot | m | Expedition 331 Scientists | [m CSF-B] Bottom Core depth (below sea floor) | |
7 | Lithology/composition/facies | Lithology | Expedition 331 Scientists | Visual description | Petrological comment on Section | |
8 | Lithology/composition/facies | Lithology | Expedition 331 Scientists | Visual description | Continued | |
9 | Lithology/composition/facies | Lithology | Expedition 331 Scientists | Visual description | Continued | |
10 | Time Stamp | Time Stamp | Expedition 331 Scientists | Of petrological comment |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
43 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 Lithology (Petrological comment on Secti...) | 8 Lithology (Continued, Visual description) | 9 Lithology (Continued, Visual description) | 10 Time Stamp (Of petrological comment) |
---|---|---|---|---|---|---|---|---|---|
331-C0014F-1H-1,0.0 | 0.000 | 0.000 | 331-C0014F-1H-1,21.0 | 0.210 | 0.208 | 0.0-12.5 cm: Dark brown silty oxidised clay with rare 0.5cm pumice fragments. Silt fraction comprises pumice, volcanic glass and abundant foraminifera. | 12.5-21.0 cm: Dark olive green reduced silty clay with rare 0.5cm pumice fragments. Silt fraction comprises pumice, volcanic glass and rare foraminifera. Shavings of Al liner also seen. | 2010-09-21T02:20:51 | |
331-C0014F-1H-2,0.0 | 0.210 | 0.208 | 331-C0014F-1H-2,100.5 | 1.215 | 1.206 | 0.0-101.0 cm: Dark olive green reduced plastic clay. Rare pale green mineral seen under binocular microscope (glauconite?). Rare narrow (3-5 mm) silt bands occur in the core (2 or 3 in the section). Silt bands contain abundant foraminifera. | Trace disseminated framboidal pyrite. | 2010-09-21T02:17:56 | |
331-C0014F-1H-3,0.0 | 1.215 | 1.206 | 331-C0014F-1H-3,100.5 | 2.220 | 2.204 | 0.0-82.0 cm: Dark olive green reduced plastic clay. Rare narrow (3-5 mm) silt bands occur in the core (2 or 3 in the section). Silt bands contain abundant foraminifera. Trace disseminated framboidal pyrite. | 82.0-84.0 cm: Distinct silt band, with abundant foraminifera. Rare pale green mineral seen under binocular microscope (glauconite?). dark olive green clay matrix. Trace disseminated framboidal pyrite. | 84.0-101.0 cm: Dark olive green reduced plastic clay. Rare narrow (3-5 mm) silt bands occur in the core (2 or 3 in the section). Silt bands contain abundant foraminifera. Trace disseminated framboidal pyrite. | 2010-09-21T02:25:16 |
331-C0014F-1H-4,0.0 | 2.220 | 2.204 | 331-C0014F-1H-4,100.5 | 3.225 | 3.202 | 0.0-74.0 cm: General gradation from dark olive green reduced silty clay at top of interval to matrix supported pumiceous grit with a dark olive green clay matrix at base. | More sulfidic than previous intervals in this hole, but still << 1% fine grained pyrite framboids and rare pyritized foraminifera. Fragmental component is pumice and glass, with <5% shell fragments and foraminifera. Green glauconite (?) present. | 42.0-100.5 cm:Matrix supported pumiceous grit with a dark olive green sandy clay matrix.Fragmental component is pumice and glass, with minor shell fragments and foraminifera.Green glauconite (?) present. Trace fine grained disseminated framboidal pyrite. | 2010-09-21T02:42:33 |
331-C0014F-1H-5,0.0 | 3.225 | 3.202 | 331-C0014F-1H-5,100.0 | 4.225 | 4.195 | 0.0-52.0 cm:Matrix supported pumiceous grit with a dark olive green sandy clay matrix.Fragmental component is pumice and glass,with minor shell fragments and foraminifera.Green glauconite(?) present.Trace fine grained disseminated framboidal pyrite. | 52.0-99.0 cm:Clast supported pumiceous grit with a dark olive green sandy clay matrix. Fragmental component is pumice and glass, with minor shell fragments and foraminifera. Green glauconite (?) present.Trace fine grained disseminated framboidal pyrite. | 99.0-100.0cm: WR sample (PAL). Not imaged by XCT. | 2010-09-21T02:44:25 |