Not logged in
PANGAEA.
Data Publisher for Earth & Environmental Science

Fretzdorff, Susanne; Haase, Karsten M; Leat, Philip; Livermore, Roy A; Garbe-Schönberg, Dieter; Fietzke, Jan; Stoffers, Peter (2003): (Table 1) Composition of volcanic glasses from the East Scotia Ridge [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.847689, Supplement to: Fretzdorff, S et al. (2003): 230Th-238U disequilibrium in East Scotia backarc basalts: Implications for slab contributions. Geology, 31(8), 693, https://doi.org/10.1130/G19469.1

Always quote citation above when using data! You can download the citation in several formats below.

RIS CitationBibTeX CitationShow MapGoogle Earth

Abstract:
New U-series isotope data for lavas from the East Scotia backarc spreading center span a large range in (230Th/232Th) and (238U/232Th). Most of the backarc lavas have (238U/230Th) < 1, similar to the composition of mid-oceanic-ridge basalts (MORB). Lavas from two segments have (238U/230Th) > 1 and are enriched in fluid-mobile elements, implying a recent addition of a U-rich slab-derived component. The data from one segment suggest an influence from an aqueous fluid from altered MORB, whereas samples from the other slab-influenced segment show addition of a sediment melt. The slab-influenced samples form a distinct trend in the equiline diagram between aqueous fluid and sediment melt that is suggested to be a mixing line rather than an isochron.
Funding:
German Research Foundation (DFG), grant/award no. 5472008: Priority Programme 1158 Antarctic Research with Comparable Investigations in Arctic Sea Ice Areas
Coverage:
Latitude: -58.000000 * Longitude: -25.000000
Event(s):
EastScotiaRidge * Latitude: -58.000000 * Longitude: -25.000000 * Location: Southern Ocean * Method/Device: Rock sample (ROCK)
Comment:
The quoted errors are 2 sigma errors.
Size:
265 data points

Data

Download dataset as tab-delimited text — use the following character encoding:


Sect
(segment)

Sample ID

MgO [%]

Th [mg/kg]

U [mg/kg]

238U/232Th

Error a [±]
(238U/232Th)

(234U/238U)

Error a [±]
(234U/238U)
10 
230Th/232Th
11 
Error a [±]
(230Th/232Th)
12 
230Th/238U
13 
Error a [±]
(230Th/238U)
E396DS-18.160.1780.05901.0060.0041.1640.0201.1580.015
E397DS-16.940.3230.10000.9440.0041.0460.0161.1080.014
E398DS-16.830.4990.14200.8640.0040.9530.0111.1030.011
E4wx476.350.6660.19000.8650.0051.0000.0060.8410.0110.9720.014
E499DS-15.851.3720.32600.7200.0041.0130.0050.7380.0071.0250.011
E499DS-45.971.4080.33000.7110.0040.7600.0061.0690.009
E4100DS-17.420.2630.09101.0570.0030.9990.0051.0010.0110.9470.012
E5wx488.130.1030.04441.3080.0041.4690.0201.1230.012
E5104DS-17.020.2250.08911.2000.0061.2030.0191.0030.016
E5104DS-1 (rpt)7.020.2250.08791.1920.0031.2030.0191.0030.017
E6106DS-17.820.1280.04991.1820.0051.2030.0281.0180.023
E6107DS-17.930.1520.06301.2570.0041.3140.0221.0450.016
E6107DS-38.100.2000.07131.0790.0031.1660.0141.0810.011
E6108DS-17.680.2170.08051.1260.0031.1640.0171.0330.014
E7109DS-17.750.1280.04981.1830.0041.2140.0211.0260.017
E7110DS-36.810.3090.11301.1080.0031.2140.0121.0960.009
E8wx565.040.2160.08261.1600.0050.9960.0121.0070.0160.8680.019
E8wx603.580.1780.06081.0350.0050.9950.0110.8850.0200.8550.027
E8wx626.650.1200.03830.9700.0030.9930.0140.9000.0230.9280.028
E9wx636.200.2980.10401.0600.0041.1590.0151.0930.013
E9wx676.610.6140.21601.0690.0061.1240.0131.0510.012
E9wx686.660.3820.13201.0470.0051.2300.0101.1750.008
E9wx697.220.4470.15801.0760.0051.1590.0081.0780.008