Binns, Raymond A; Barriga, Fernando J A S; Miller, D Jay (2007): (Tables T1, T2) Major element content in alteration categories of ODP Site 193-1188 and Hole 193-1189A, PACMANUS field [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.778790, Supplement to: Binns, RA et al. (2007): Leg 193 synthesis: Anatomy of an active felsic-hosted hydrothermal system, eastern Manus Basin, Papua New Guinea. In: Barriga, FJAS; Binns, RA; Miller, DJ; Herzig, PM (eds.) Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 193, 1-71, https://doi.org/10.2973/odp.proc.sr.193.201.2007
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Abstract:
In the Ocean Drilling Program's only foray to an active seafloor hydrothermal system hosted by felsic volcanic rocks at a convergent plate margin, deep penetrations were achieved at two contrasted sites within the PACMANUS field (Manus backarc basin, Papua New Guinea). Just 1.0 km apart, these sites are characterized, respectively, by diffuse low-temperature venting at the seabed (Site 1188, Snowcap site; 1650 meters below sea level [mbsl]) and focused high-temperature venting (Site 1189, Roman Ruins; 1700 mbsl). Shallow holes at a background location remote from known hydrothermal activity (Site 1190) and at a second high-temperature chimney field (Site 1191, Satanic Mills) failed to drill beyond unaltered felsic lavas which at Sites 1188 and 1189 form an impervious cap (as thick as 35 m) to an underlying, pervasively altered lava sequence with occasional volcaniclastic horizons.
To the maximum depth drilled (387 meters below seafloor [mbsf]), alteration assemblages are characterized by clay minerals and ubiquitous disseminated pyrite. Hydrothermal K-feldspar at Site 1189 differentiates it from Site 1188 where, by contrast, several intervals of pyrophyllite-bearing acid sulfate alteration suggest input from magmatic volatiles. At both deeply penetrated sites the dominant silica phase in alteration assemblages changes downhole from opal-A at the transition from overlying unaltered lava to cristobalite and then to quartz. The boundary between the cristobalite and quartz domains is gradational between 60 and 110 mbsf in Hole 1188A under Snowcap but is sharper and shallower (~25 mbsf) in Hole 1189A on the fringes of the Roman Ruins field. Hole 1189B, higher on the Roman Ruins mound, intersected a "Stockwork Zone" with abundant quartz ± pyrite ± anhydrite veins and breccia infills, from base of casing (31 mbsf) to ~110 mbsf, below which an abrupt change occurred to a "Lower Sequence" with interleaved cristobalite- and quartz-bearing assemblages and common preservation of igneous plagioclase. Only two thin intervals of sulfide-rich mineralization were encountered, both below the Roman Ruins chimney field.
Project(s):
Ocean Drilling Program (ODP)
Coverage:
Median Latitude: -3.725700 * Median Longitude: 151.671533 * South-bound Latitude: -3.728300 * West-bound Longitude: 151.669800 * North-bound Latitude: -3.720700 * East-bound Longitude: 151.674900
Date/Time Start: 2000-11-18T17:30:00 * Date/Time End: 2000-12-30T04:00:00
Minimum DEPTH, sediment/rock: 31.20 m * Maximum DEPTH, sediment/rock: 300.72 m
Event(s):
193-1188A * Latitude: -3.728300 * Longitude: 151.669900 * Date/Time Start: 2000-11-18T17:30:00 * Date/Time End: 2000-11-22T08:30:00 * Elevation: -1640.2 m * Penetration: 211.6 m * Recovery: 21.93 m * Location: Bismarck Sea * Campaign: Leg193 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 23 cores; 211.6 m cored; 0 m drilled; 10.4 % recovery
193-1188F * Latitude: -3.728100 * Longitude: 151.669800 * Date/Time Start: 2000-12-29T15:15:00 * Date/Time End: 2000-12-30T04:00:00 * Elevation: -1641.7 m * Penetration: 386.7 m * Recovery: 30.89 m * Location: Bismarck Sea * Campaign: Leg193 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 45 cores; 168.7 m cored; 218 m drilled; 18.3 % recovery
193-1189A * Latitude: -3.720700 * Longitude: 151.674900 * Date/Time Start: 2000-11-22T08:30:00 * Date/Time End: 2000-11-23T20:45:00 * Elevation: -1690.2 m * Penetration: 125.8 m * Recovery: 8.58 m * Location: Bismarck Sea * Campaign: Leg193 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 13 cores; 125.8 m cored; 0 m drilled; 6.8 % recovery
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | Event label | Event | ||||
| 2 | Sample code/label | Sample label | Binns, Raymond A | DSDP/ODP/IODP sample designation | ||
| 3 | Piece | Piece | Binns, Raymond A | |||
| 4 | DEPTH, sediment/rock | Depth sed | m | Geocode – mbsf | ||
| 5 | Sample ID | Sample ID | Binns, Raymond A | of Commonwealth Scientific and Industrial Research Organisation (CSIRO) | ||
| 6 | Description | Description | Binns, Raymond A | |||
| 7 | Alteration | Alteration | Binns, Raymond A | category | ||
| 8 | Silicon dioxide | SiO2 | % | Binns, Raymond A | ||
| 9 | Titanium dioxide | TiO2 | % | Binns, Raymond A | ||
| 10 | Aluminium oxide | Al2O3 | % | Binns, Raymond A | ||
| 11 | Iron oxide, FeO | FeO | % | Binns, Raymond A | FeO(t) | |
| 12 | Manganese oxide | MnO | % | Binns, Raymond A | ||
| 13 | Magnesium oxide | MgO | % | Binns, Raymond A | ||
| 14 | Calcium oxide | CaO | % | Binns, Raymond A | ||
| 15 | Sodium oxide | Na2O | % | Binns, Raymond A | ||
| 16 | Potassium oxide | K2O | % | Binns, Raymond A | ||
| 17 | Phosphorus pentoxide | P2O5 | % | Binns, Raymond A | ||
| 18 | Sulfur, total | TS | % | Binns, Raymond A | ||
| 19 | Loss on ignition | LOI | % | Binns, Raymond A | includes loss on drying (105°C) | |
| 20 | Elements, total | Total | % | Binns, Raymond A | uncorrected for oxygen in sulfides allocated to FeO(t) or not allocated to TS for sulfates | |
| 21 | Zirconium/Titanium ratio | Zr/Ti | Binns, Raymond A | Zr in mg/kg and Ti in wt % TiO2 |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
133 data points