Grimes, Craig B; John, Barbara E; Cheadle, Michael J; Mazdab, Frank K; Wooden, Joseph L; Swapp, Susan; Schwartz, Joshua J (2010): (Table S2) Trace element analyses of porous zircon and luminescent rims on zircon from ocean crust [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.772868, In supplement to: Grimes, CB et al. (2009): On the occurrence, trace element geochemistry, and crystallization history of zircon from in situ ocean lithosphere. Contributions to Mineralogy and Petrology, 158(6), 757-783, https://doi.org/10.1007/s00410-009-0409-2
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Project(s):
Coverage:
Median Latitude: 30.056772 * Median Longitude: -42.039667 * South-bound Latitude: 30.000000 * West-bound Longitude: -42.119000 * North-bound Latitude: 30.168650 * East-bound Longitude: -42.000000
Minimum DEPTH, sediment/rock: 0 m * Maximum DEPTH, sediment/rock: 0 m
Event(s):
304-U1309D * Latitude: 30.168650 * Longitude: -42.119000 * Elevation: -1644.9 m * Recovery: 243.69 m * Campaign: Exp304 (Oceanic Core Complex Formation, Atlantis Massive 1) * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 77 cores; 380.7 m cored; 64 % recovered; 20.5 m drilled; 401.3 m penetrated
305-U1309D * Latitude: 30.001667 * Longitude: -42.000000 * Elevation: -1644.9 m * Recovery: 799.65 m * Campaign: Exp305 (Oceanic Core Complex Formation, Atlantis Massive 2) * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 216 cores; 1014.2 m cored; 78.8 % recovered; 0 m drilled; 1415.5 m penetrated
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | Event label | Event | ||||
| 2 | Sample code/label | Sample label | Grimes, Craig B | |||
| 3 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
| 4 | Sample comment | Sample comment | Grimes, Craig B | |||
| 5 | Sample code/label 2 | Sample label 2 | Grimes, Craig B | spot | ||
| 6 | Sulfur | S | relative units | Grimes, Craig B | Sensitive high-resolution ion microprobe-reverse geometry (SHRIMP-RG) | |
| 7 | Chlorine | Cl | relative units | Grimes, Craig B | Sensitive high-resolution ion microprobe-reverse geometry (SHRIMP-RG) | |
| 8 | Fluorine | F | mg/kg | Grimes, Craig B | Sensitive high-resolution ion microprobe-reverse geometry (SHRIMP-RG) | |
| 9 | Aluminium | Al | mg/kg | Grimes, Craig B | Sensitive high-resolution ion microprobe-reverse geometry (SHRIMP-RG) | |
| 10 | Calcium | Ca2+ | mg/kg | Grimes, Craig B | Sensitive high-resolution ion microprobe-reverse geometry (SHRIMP-RG) | |
| 11 | Iron | Fe | mg/kg | Grimes, Craig B | Sensitive high-resolution ion microprobe-reverse geometry (SHRIMP-RG) | |
| 12 | Scandium | Sc | mg/kg | Grimes, Craig B | Sensitive high-resolution ion microprobe-reverse geometry (SHRIMP-RG) | |
| 13 | Titanium | Ti | mg/kg | Grimes, Craig B | Sensitive high-resolution ion microprobe-reverse geometry (SHRIMP-RG) | |
| 14 | Phosphorus | P | mg/kg | Grimes, Craig B | Sensitive high-resolution ion microprobe-reverse geometry (SHRIMP-RG) | |
| 15 | Yttrium | Y | mg/kg | Grimes, Craig B | Sensitive high-resolution ion microprobe-reverse geometry (SHRIMP-RG) | |
| 16 | Niobium | Nb | mg/kg | Grimes, Craig B | Sensitive high-resolution ion microprobe-reverse geometry (SHRIMP-RG) | |
| 17 | Lanthanum | La | mg/kg | Grimes, Craig B | Sensitive high-resolution ion microprobe-reverse geometry (SHRIMP-RG) | |
| 18 | Cerium | Ce | mg/kg | Grimes, Craig B | Sensitive high-resolution ion microprobe-reverse geometry (SHRIMP-RG) | |
| 19 | Praseodymium | Pr | mg/kg | Grimes, Craig B | Sensitive high-resolution ion microprobe-reverse geometry (SHRIMP-RG) | |
| 20 | Neodymium | Nd | mg/kg | Grimes, Craig B | Sensitive high-resolution ion microprobe-reverse geometry (SHRIMP-RG) | |
| 21 | Samarium | Sm | mg/kg | Grimes, Craig B | Sensitive high-resolution ion microprobe-reverse geometry (SHRIMP-RG) | |
| 22 | Europium | Eu | mg/kg | Grimes, Craig B | Sensitive high-resolution ion microprobe-reverse geometry (SHRIMP-RG) | |
| 23 | Gadolinium | Gd | mg/kg | Grimes, Craig B | Sensitive high-resolution ion microprobe-reverse geometry (SHRIMP-RG) | |
| 24 | Terbium | Tb | mg/kg | Grimes, Craig B | Sensitive high-resolution ion microprobe-reverse geometry (SHRIMP-RG) | |
| 25 | Dysprosium | Dy | mg/kg | Grimes, Craig B | Sensitive high-resolution ion microprobe-reverse geometry (SHRIMP-RG) | |
| 26 | Holmium | Ho | mg/kg | Grimes, Craig B | Sensitive high-resolution ion microprobe-reverse geometry (SHRIMP-RG) | |
| 27 | Erbium | Er | mg/kg | Grimes, Craig B | Sensitive high-resolution ion microprobe-reverse geometry (SHRIMP-RG) | |
| 28 | Thulium | Tm | mg/kg | Grimes, Craig B | Sensitive high-resolution ion microprobe-reverse geometry (SHRIMP-RG) | |
| 29 | Ytterbium | Yb | mg/kg | Grimes, Craig B | Sensitive high-resolution ion microprobe-reverse geometry (SHRIMP-RG) | |
| 30 | Lutetium | Lu | mg/kg | Grimes, Craig B | Sensitive high-resolution ion microprobe-reverse geometry (SHRIMP-RG) | |
| 31 | Hafnium | Hf | % | Grimes, Craig B | Sensitive high-resolution ion microprobe-reverse geometry (SHRIMP-RG) | |
| 32 | Thorium | Th | mg/kg | Grimes, Craig B | Sensitive high-resolution ion microprobe-reverse geometry (SHRIMP-RG) | |
| 33 | Uranium | U | mg/kg | Grimes, Craig B | Sensitive high-resolution ion microprobe-reverse geometry (SHRIMP-RG) | |
| 34 | Temperature, calculated | T cal | °C | Grimes, Craig B | Calculated | Uncorrected Ti-in-zircon temperature calculated using the equation of Ferry and Watson (2007) (Ti and Si activities = 1) |
| 35 | Temperature, calculated | T cal | °C | Grimes, Craig B | Calculated | Corrected Ti-in-zircon temperature (after Ferry and Watson, 2007) assuming TiO2 activity = 0.7, SiO2 activity = 1, pressure =2 kbars |
| 36 | Europium anomaly | Eu/Eu* | Grimes, Craig B | Calculated | Eu-anomalies were calculated in the following manner using chondrite-normalized values: Eu/Eu* = EuN/(square-root(GdN*SmN)) | |
| 37 | Cerium anomaly | Ce/Ce* | Grimes, Craig B | Calculated | Ce-anomaly calculated in the following manner using chondrite-normalized values: Ce/Ce* = CeN/(square-root(LaN*PrN)). For samples in which Pr was not measured directly, chondrite normalized Pr values were estimated from smooth chondrite normalized REE patterns: Prest = LaN*(1/3) + NdN*(2/3)). An overestimate of La in zircon will therefore lead to overestimated Pr values. Normalizing values were from Korotev, 1996. | |
| 38 | Comment | Comment | Grimes, Craig B |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
1542 data points