Pariso, Janet E; Johnson, H Paul (1989): (Table 2) Summary of oxide petrography description of samples from the sheeted dike complex, ODP Hole 111-504B [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.753152, In supplement to: Pariso, JE; Johnson, HP (1989): Magnetic properties and oxide petrography of the sheeted dike complex in Hole 504B. In: Becker, K; Sakai, H; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 111, 159-167, https://doi.org/10.2973/odp.proc.sr.111.132.1989
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Project(s):
Ocean Drilling Program (ODP)
Coverage:
Latitude: 1.226900 * Longitude: -83.730300
Date/Time Start: 1986-10-05T11:45:00 * Date/Time End: 1986-10-16T18:15:00
Minimum DEPTH, sediment/rock: 960.00 m * Maximum DEPTH, sediment/rock: 1548.40 m
Event(s):
111-504B * Latitude: 1.226900 * Longitude: -83.730300 * Date/Time Start: 1986-10-05T11:45:00 * Date/Time End: 1986-10-16T18:15:00 * Elevation: -3474.0 m * Penetration: 1562.1 m * Recovery: 27.36 m * Location: North Pacific Ocean * Campaign: Leg111 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 29 cores; 209 m cored; 0 m drilled; 13.1 % recovery
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
| 2 | Comment | Comment | Pariso, Janet E | oxidation class, describes the average degree of high-temperature, deuteric oxidation of primary oxides observed in the samples | ||
| 3 | Comment 2 (continued) | Comm 2 | Pariso, Janet E | hydrothermal alteration class, describes the average degree of hydrothermal alteration of oxides in the sample | ||
| 4 | Comment 3 (continued) | Comm 3 | Pariso, Janet E |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
96 data points
Data
| 1 Depth sed [m] | 2 Comment | 3 Comm 2 | 4 Comm 3 |
|---|---|---|---|
| 960.00 | C1 | H4 | Titanomagnetite nearly completely granulated to sphene and anatase |
| 1068.00 | C1 | H2 | Titanomagnetite is variably granulated and has low-temperature cracks |
| 1100.00 | C1 | H4 | Titanomagnetite nearly completely granulated to sphene and anatase |
| 1150.00 | C1 | H2 | Magnetite is pervasively, but lightly, granulated; discrete ilmenite grains are unaltered |
| 1152.00 | C1 | H3 | Titanomagnetite is granulated to variable degrees, has low temperature cracks, and rare, very fine ilmenite lamellae |
| 1190.00 | C3 | H2 | Titanomagnetite pervasively, but lightly, granulated; discrete ilmenite is very clean |
| 1261.00 | C3 | H2-H3 | Titanomagnetite granulated to varying degrees; discrete ilmenite is unaltered |
| 1295.00 | C1-C2 | H3-H4 | Titanomagnetite heavily altered to sphene and anatase granules; discrete ilmenite grains unaltered |
| 1327.00 | C1 | 4 | Titanomagnetite is heavily altered to sphene and anatase; discrete ilmenite grains are unaltered |
| 1354.65 | C1 | H2 | Nondeuterically altered titanomagnetites have variable degrees of hydrothermal granulation |
| 1359.36 | C2 | H2 | Ilmenite lamellae generally unaltered; remaining titanomagnetite is granulated |
| 1360.29 | ? | H6 | Titanomagnetite is completely altered to massive anatase ghosts |
| 1361.40 | C2-C3 | H3-H4 | Titanomagnetite is quite variably granulated |
| 1369.02 | C1 | H2 | Titanomagnetite pervasively, but lightly, granulated; discrete ilmenite is very clean |
| 1378.32 | C3 | H4 | Magnetite part of magnetite/ilmenite network is nearly completely altered to sphene; ilmenite in lamellae are only partly altered |
| 1380.34 | C2-C3 | H5 | Magnetite nearly completely altered to anatase; ilmenite only moderately altered |
| 1382.59 | C2-C3 | H5 | Magnetite nearly completely altered to anatase; ilmenite only moderately altered |
| 1398.03 | C2 | H2 | Ilmenite lamellar or podlike, with some altered to sphene; magnetite is lightly granulated |
| 1399.26 | C2-C3 | H2 | Ilmenite lamellar or podlike, with some altered to sphene; magnetite is lightly granulated |
| 1408.82 | C2-C3 | H2 | Very fine ilmenite lamellae; light granulation of magnetite |
| 1417.24 | C2 | H3 | Lamellar and irregular ilmenite are rarely hydrothermally altered; magnetite is granulated |
| 1418.54 | C2 | H3 | Lamellar and irregular ilmenite are rarely hydrothermally altered; magnetite is granulated |
| 1426.67 | C2 | H3 | Ilmenite is both lamellar and podlike and variably altered to sphene; magnetite bears anatase granules |
| 1427.75 | C2-C3 | H2-H3 | Ilmenite is always lamellar and commonly altered to sphene on grain peripheries; magnetite is anatase bearing and has lost iron |
| 1445.94 | C2 | H5 | Ilmenite lamellae are altered to sphene; large iron losses in magnetite |
| 1454.44 | C2 | H2 | Thin and irregular ilmenite are rarely altered to sphene; magnetite bears anatase granules |
| 1455.06 | C1-C2 | H2 | Ilmenite commonly altered to sphene; magnetite bears anatase granules |
| 1504.67 | C3 | H1-H2 | Lamellar and podlike ilmenite is unaltered; magnetite is lightly altered to anatase |
| 1512.59 | C3-C4 | H3 | Magnetite is generally unaltered; ilmenite lamellae and pods altered to sphene |
| 1513.16 | C3-C4 | H3 | Magnetite is generally unaltered; ilmenite lamellae and pods altered to sphene |
| 1529.79 | C3-C4 | H1-H2 | Ilmenite is podlike; magnetite bears small number of secondary anatase granules |
| 1548.40 | C3-C4 | H1-H2 | Abundant ilmenite is irregular in form; small crystals of anatase are the only alteration product of magnetite |