Barrett, T J; Friedrichsen, Hans (1982): 87Sr/86Sr ratios, Sr and Rb concentrations and stable oxygen isotope values for some basalts from ODP Hole 504B (Table 1) [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.711004, Supplement to: Barrett, TJ; Friedrichsen, H (1982): Strontium and oxygen isotopic composition of some basalts from Hole 504B, Costa Rica Rift, DSDP Legs 69 and 70. Earth and Planetary Science Letters, 60(1), 27-38, https://doi.org/10.1016/0012-821X(82)90017-6
Always quote citation above when using data! You can download the citation in several formats below.
Abstract:
Seventeen whole-rock samples, generally taken at 25-50 m intervals from 5 to 560 m sub-basement in Hole 504B, drilled in 6.2 m.y. old crust, were analysed for 87Sr/86Sr ratios, Sr and Rb concentrations, and 18O/16O ratios. Sr isotope ratios for 8 samples from the upper 260 m of the hole range from 0.70287 to 0.70377, with a mean of 0.70320. In the 330-560 m interval, 5 samples have a restricted range of 0.70255-0.70279, with a mean of 0.70266, the average value for fresh mid-ocean ridge basalts (MORB). In the 260-330 m interval, approximately intermediate Sr isotopic ratios are found.
Delta18O values (‰) range from 6.4 to 7.8 in the upper 260 m, 6.2-6.4 in the 270-320 m interval, and 5.8-6.2 in the 320-560 m interval. The values in the upper 260 m are typical for basalts which have undergone low-temperature seawater alteration, whereas the values for the 320-560 m interval correspond to MORB which have experienced essentially no oxygen isotopic alteration.
The higher 87Sr/86Sr and 18O/16O ratios in the upper part of the hole can be interpreted as the result of a greater overall water/rock ratio in the upper part of the Hole 504B crust than in the lower part. Interaction of basalt with seawater (87Sr/86Sr = 0.7091) increased basalt 87Sr/86Sr ratios and produced smectitic alteration products which raised whole-rock delta18O values. Seawater circulation in the lower basalts may have been partly restricted by the greater number of relatively impermeable massive lava flows below about 230 m sub-basement. These flows may have helped to seal off lower basalts from through-flowing seawater.
Project(s):
Deep Sea Drilling Project (DSDP)
Coverage:
Median Latitude: 1.227100 * Median Longitude: -83.730100 * South-bound Latitude: 1.227000 * West-bound Longitude: -83.730200 * North-bound Latitude: 1.227200 * East-bound Longitude: -83.730000
Date/Time Start: 1979-10-07T00:00:00 * Date/Time End: 1979-12-04T00:00:00
Minimum ORDINAL NUMBER: 1 * Maximum ORDINAL NUMBER: 17
Event(s):
69-504B * Latitude: 1.227200 * Longitude: -83.730200 * Date/Time: 1979-10-07T00:00:00 * Elevation: -3460.0 m * Penetration: 489 m * Recovery: 262 m * Campaign: Leg69 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL)
70-504B * Latitude: 1.227000 * Longitude: -83.730000 * Date/Time: 1979-12-04T00:00:00 * Elevation: -3460.0 m * Penetration: 836.1 m * Recovery: 91.6 m * Campaign: Leg70 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 40 cores; 328.6 m cored; 18.5 m drilled; 27.9 % recovery
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | Event label | Event | ||||
| 2 | ORDINAL NUMBER | Ord No | Geocode | |||
| 3 | Sample code/label | Sample label | Barrett, T J | DSDP/ODP/IODP sample designation | ||
| 4 | Sample code/label 2 | Sample label 2 | Barrett, T J | |||
| 5 | Lithology/composition/facies | Lithology | Barrett, T J | |||
| 6 | Alteration | Alteration | Barrett, T J | G = colourless to green smectites occurring as alteration products of olivine and glass, and as vesicle fillings. R = reddish-brown alteration minerals indicative of relatively oxidizing conditions (hematite, Fe hydroxide, iddingsite), occurring as alteration products of olivine and glass, and as vesicle fillings. P = pyrite, indicative of relatively reducing conditions. Where pyrite is indicated, it is not present in the actual sample, but in veins within 30 cm above or below it | ||
| 7 | Rubidium | Rb | mg/kg | Barrett, T J | X-ray fluorescence (XRF) | |
| 8 | Strontium | Sr | mg/kg | Barrett, T J | X-ray fluorescence (XRF) | |
| 9 | Strontium-87/Strontium-86 ratio | 87Sr/86Sr | Barrett, T J | Isotope ratio mass spectrometry | ||
| 10 | Strontium-87/Strontium-86 ratio, error | 87Sr/86Sr e | ± | Barrett, T J | Isotope ratio mass spectrometry | |
| 11 | δ18O | δ18O | ‰ | Barrett, T J | Isotope ratio mass spectrometry | |
| 12 | Water in rock | H2O | % | Barrett, T J |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
153 data points
Data
| 1 Event | 2 Ord No | 3 Sample label | 4 Sample label 2 | 5 Lithology | 6 Alteration | 7 Rb [mg/kg] | 8 Sr [mg/kg] | 9 87Sr/86Sr | 10 87Sr/86Sr e [±] | 11 δ18O [‰] | 12 H2O [%] |
|---|---|---|---|---|---|---|---|---|---|---|---|
| 69-504B | 1 | 69-504B-3-1,102-105 | 253 | Fine-grained aphyric basalt. Pillow or thin flow (80 cm thick): sample from middle | g, r | 3.6 | 68.8 | 0.70377 | 0.00006 | 7.40 | 0.90 |
| 69-504B | 2 | 69-504B-8-3,75-80 | 540 | Medium-grained, subaphyric basalt. Massive flow (at least 1.5 m thick); sample from middle | g | 2.5 | 69.4 | 0.70316 | 0.00006 | 7.00 | 0.72 |
| 69-504B | 3 | 69-504B-13-2,86-89 | 779 | Fine-grained aphyric basalt. Pillow or thin flow; sample from middle | g, r | 9.5 | 74.0 | 0.70337 | 0.00005 | 7.70 | |
| 69-504B | 4 | 69-504B-19-2,82-85 | 1145 | Fine-grained moderately pl-ol-cpx phyric basalt. Pillow; sample from middle | g | 2.0 | 64.6 | 0.70318 | 0.00004 | 6.55 | |
| 69-504B | 5 | 69-504B-25-2,97-101 | 1434 | Fine-grained aphyric basalt. Pillow or thin flow (55 cm thick); sample from middle | g | 6.2 | 74.1 | 0.70287 | 0.00005 | 6.60 | |
| 69-504B | 6 | 69-504B-29-1,50-52 | 1569 | Fine-grained aphyric basalt, probably pillow material | g | 0.70291 | 0.00005 | 6.90 | |||
| 70-504B | 7 | 70-504B,33-1,28-30 | 184 | Medium-grained highly ol-pl phyric basalt. Massive unit (c. 3 m thick); sample from c. 70 cm below top | g, r | 1.3 | 78.5 | 0.70291 | 0.00004 | 6.80 | 1.56 |
| 70-504B | 8 | 70-504B-34-2,32-37 | 242 | Fine-grained moderately pl-ol phyric basalt. Pillow; sample from margin | g,r | 1.4 | 67.4 | 0.70340 | 0.00006 | 7.40 | 0.79 |
| 70-504B | 9 | 70-504B-36-2,44-46 | 307 | Medium-grained moderately pl phyric basalt. Massive unit sample from c. 2 m below top | g, p | 0.0 | 58.2 | 0.70262 | 0.00007 | 6.30 | |
| 70-504B | 10 | 70-524B-38-1,90-92 | 420 | Medium-grained moderately ol-pl-cpx phyric basalt. Pillow interior | f, r, p | 0.70306 | 0.00005 | 6.20 | 0.67 | ||
| 70-504B | 11 | 70-504B-41-2,17-19 | 599 | Medium-grained moderately pl-ol phyric basalt. Massive flow (c. 14 m thick); sample from c. 3 m above base | g | 0.70296 | 0.00005 | 6.40 | |||
| 70-504B | 12 | 70-504B-46-1,112-116 | 778 | Fine-grained sparsely pl phyric basalt. Pillow; sample from margin | g | 0.1 | 60.8 | 0.70259 | 0.00007 | 6.20 | 5.84 |
| 70-504B | 13 | 70-504B-52-3,62-65 | 1030 | Medium-grained sparsely ol-pl phyric basalt. Massive unit (at least 4 m thick); sample from middle | g, p | 0.5 | 60.2 | 0.70269 | 0.00005 | 6.00 | 0.78 |
| 70-504B | 14 | 70-504B-51-1,83-88 | 1139 | Fine-grained moderately pl- ol phyric basalt. Pillow; sample from margin | g | 0.2 | 73.2 | 0.70279 | 0.00004 | 6.10 | |
| 70-504B | 15 | 70-504B-63-4,5-8 | 1393 | Glassy pillow rim; glass partly altered to green smectite | g | 2.8 | 62.5 | 0.70465 | 0.00007 | ||
| 70-504B | 16 | 70-504B-64-2,125-130 | 1436 | Medium-grained aphyric basalt. Massive flow (c. 1.5 m thick); sample from lower portion | g, p | 0.3 | 53.3 | 0.70268 | 0.00007 | 6.00 | |
| 70-504B | 17 | 70-504B-70-2,3-7 | 1563 | Coarse-grained ophitic basalt. Massive flow (or sill) of unknown thickness; sample from c. 25 cm below top | g | 0.1 | 59.8 | 0.70255 | 0.00006 | 5.80 |