Takai, Ken; Mottl, Michael J; Nielsen, Simon Harder Holm; Expedition 331 Scientists (2012): Visual core description (VCD) from IODP Hole 331-C0016B [dataset]. SIO7 Data Center, J-CORES Database; Ocean Drilling Program, Center for Deep Earth Exploration (JAMSTEC), PANGAEA, https://doi.org/10.1594/PANGAEA.776857
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-C0016B, snapshot taken on 2011-10-03, J-CORES, SIO7 Data Center [dataset]. https://www.jamstec.go.jp/sio7/j-cores.data/331/C0016B/
Project(s):
Coverage:
Latitude: 27.790897 * Longitude: 126.896433
Minimum DEPTH, sediment/rock: 0.00 m * Maximum DEPTH, sediment/rock: 27.59 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 | Lithology/composition/facies | Lithology | Expedition 331 Scientists | Visual description | Continued | |
| 11 | Lithology/composition/facies | Lithology | Expedition 331 Scientists | Visual description | Continued | |
| 12 | Lithology/composition/facies | Lithology | Expedition 331 Scientists | Visual description | Continued | |
| 13 | Time Stamp | Time Stamp | Expedition 331 Scientists | Of petrological comment |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
55 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 Lithology (Continued, Visual description) | 11 Lithology (Continued, Visual description) | 12 Lithology (Continued, Visual description) | 13 Time Stamp (Of petrological comment) |
|---|---|---|---|---|---|---|---|---|---|---|---|---|
| 331-C0016B-1L-1,0.0 | 0.00 | 0.00 | 331-C0016B-1L-1,64.0 | 0.640 | 0.640 | 0.0-27.0 cm: Hard black massive sulfide. Clastic textured black ore comprising rounded 1-5mm fragments of ~10% soft clay altered and ~10% hard siliceous volcanic rock cemented in a hard matrix of ~60% sphalerite, 15% pyrite, and quartz. | Coarser grained (2-3mm) sphalerite, pyrite, galena and possible chalcopyrite is associated with a late anhydrite vein down one side of section. 27.0-31.0 cm: WR sample (MB). Massive sulfide from XCT. 31.0-34.0 cm: Seimi-massive sulfide. | Hard, gray, strongly silicified interval with clastic texture almost obliterated by silificification. ~15% sphalerite, 10% pyrite. 34.0-64.0 cm: Hard black massive sulfide. | Similar to upper interval of section, with less abundant altered clasts (5%) and scattered irregular 2-4cm patches of pale clay with sugary quartz (possible late void fill?). Sulfide is more abundant: ~85% of total, with ~ half of this being pyrite. | 2010-09-30T23:35:59 | ||
| 331-C0016B-1L-CC,0.0 | 0.64 | 0.64 | 331-C0016B-1L-CC,15.0 | 0.790 | 0.790 | 0.0-15.0 cm: Hard gray strongly silicifed volcanic rock with ~5% coarsely disseminated 1mm pyrite and sphalerite throughout the body of the rock. | Coarser 2-3mm sulfide (pyrite-sphalerite-minor galena) is associated with a quartz-anhydrite-10% sulfide vein that runs from the top of the section to ~10cm (see core photo). | Fine 1-2mm wide irregular anastomosing veinlets of quartz with 10% sulfide also cut the rock. | 2010-09-30T23:49:47 | |||
| 331-C0016B-2L-CC,0.0 | 9.00 | 9.00 | 331-C0016B-2L-CC,31.0 | 9.310 | 9.310 | 0.0-7.0 cm: Hard gray strongly silicified volcanic rock with faint remnant clastic texture. ~5% pyrite and trace sphalerite disseminated as very fine crystals and scattered coarser 0.1mm euhdra throughout the rock. | 7.0-18.0 cm: Snow white coarsely crystalline anhydrite aggregate composed of 1-2cm tightly intergrown acicular crystals. Rough aligment of crystals in part of sample (orientation relative to core is meaningless, due to distruption). | Most of material is sulfide-free, except for a dark vein of 1-2mm euhedral spahlerite-minor pyrite which lies along one edge of the interval. 18.0-19.0 cm: WR sample (MB). Similar to overlying material. 19.0-20.0 cm: NO CORE. | 20.0-20.5 cm: WR sample (MB) Similar to underlying material. 20.5-31.0 cm: Subangular 2mm to 3cm (dominantly 5 - 10mm) soft gray clay altered and slighly harder white sugary silica-clay altered volcanic clasts are hosted in a dark hard siliceous matrix. | Fine grained pyrite is disseminated throughout the matrix, averaging ~3%, although the distribution is uneven. The clasts are also unevenly pyritic, containing up to 5% fine grained pyrite as disseminations and occasional vesicle fill. | The edge of an anhydrite-sphalerite-pyrite-trace galena vein runs along the top of the fragment - clearly trucnated by drilling, up to 1cm wide as exposed. | 2010-10-01T21:25:14 |
| 331-C0016B-3L-1,0.0 | 27.00 | 27.00 | 331-C0016B-3L-1,59.0 | 27.590 | 27.590 | 0.0-59.0 cm: Dark green to gray hard quartz-chlorite altered volcanic rock with abundant veining - stockwork mineralisation. Possible faintly defined fragments up to ~1cm in size, may be clasts, or fracture/veining generated. | Very fine grained pyrite is disseminated throughout the rock at trace levels. Including the veins, the interval contains ~ 5% sulfide. | Two generations of veining: Earlier sugary quartz-chlorite-pyrite veins form a network of 2-3cm wide veins, including a dark diffuse quartz- fine pyrite halo. | They contain euhedral pyrite up to 5mm in size in their cores, associated with green chlorite and sugary quartz. Later pyrite-anhydrite veins crosscut the quartz-chlorite-pyrite veins and lack halos. | They can be vuggy and comprise very coarse pyrite crystals (plus possible chalcopyrite - needs to be confirmed petrographically)) up to 0.5-1cm in size, with a sharply defined selvedge of anhydrite. | They vary from hairline (anhydrite only) to 1cm in thickness. | 2010-10-02T21:11:43 |
| 331-C0016B-3L-CC,0.0 | 27.59 | 27.59 | 331-C0016B-3L-CC,40.5 | 27.995 | 27.995 | 0.0-39.5 cm: Dark green to gray hard quartz-chlorite altered volcanic rock with abundant veining - stockwork mineralisation. Possible faintly defined fragments up to ~1cm in size, may be clasts, or fracture/veining generated. | Very fine grained pyrite is disseminated throughout the rock at trace levels. Including the veins, the interval contains ~ 5% sulfide. | Two generations of veining: Earlier sugary quartz-chlorite-pyrite veins form a network of 2-3cm wide veins, including a dark diffuse quartz- fine pyrite halo. | They contain euhedral pyrite up to 5mm in size in their cores, associated with green chlorite and sugary quartz. Later pyrite-anhydrite veins crosscut the quartz-chlorite-pyrite veins and lack halos. | They can be vuggy and comprise very coarse pyrite crystals (plus possible chalcopyrite - needs to be confirmed petrographically)) up to 0.5-1cm in size, with a sharply defined selvedge of anhydrite. | They vary from hairline (anhydrite only) to 1cm in thickness. 39.5-40.5 cm: WR sample (PAL). Not imaged by XCT, but visual inspection indicates that it is the same material as the rest of the core. | 2010-10-02T21:14:46 |