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Coogan, Laurence A; Kempton, Pamela D; Saunders, Andrew D; Norry, Michael J (2000): Element concentrations of plagioclase and clinopyroxene in poikilitic olivine gabbros from ODP Hole 153-923A (Table 4) [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.711293, Supplement to: Coogan, LA et al. (2000): Melt aggregation within the crust beneath the Mid-Atlantic Ridge: evidence from plagioclase and clinopyroxene major and trace element compositions. Earth and Planetary Science Letters, 176(2), 245-257, https://doi.org/10.1016/S0012-821X(00)00006-6

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Abstract:
Ocean Drilling Program Hole 923A, located on the western flank of the Mid-Atlantic Ridge south of the Kane Fracture Zone, recovered primitive gabbros that have mineral trace element compositions inconsistent with growth from a single parental melt. Plagioclase crystals commonly show embayed anorthitic cores overgrown by more albitic rims. Ion probe analyses of plagioclase cores and rims show consistent differences in trace element ratios, indicating variation in the trace element characteristics of their respective parental melts. This requires the existence of at least two distinct melt compositions within the crust during the generation of these gabbros. Melt compositions calculated to be parental to plagioclase cores are depleted in light rare earth elements, but enriched in yttrium, compared to basalts from this region of the Mid-Atlantic Ridge, which are normal mid-ocean ridge basalt (N-MORB). Clinopyroxene trace element compositions are similar to those predicted to be in equilibrium with N-MORB. However, primitive clinopyroxene crystals are much more magnesian than those produced in one-atmosphere experiments on N-MORB, suggesting that the major element composition of the melt was unlike N-MORB. These data require that the diverse array of melt compositions generated within the mantle beneath mid-ocean ridges are not always fully homogenised during melt extraction from the mantle and that the final stage of mixing can occur efficiently within crustal magma chambers. This has implications for the process of melt extraction from the mantle and the liquid line of descent of MORB
Project(s):
Coverage:
Latitude: 23.542600 * Longitude: -45.031600
Date/Time Start: 1994-01-07T17:27:00 * Date/Time End: 1994-01-13T02:45:00
Minimum ORDINAL NUMBER: 1 * Maximum ORDINAL NUMBER: 17
Event(s):
153-923A * Latitude: 23.542600 * Longitude: -45.031600 * Date/Time Start: 1994-01-07T17:27:00 * Date/Time End: 1994-01-13T02:45:00 * Elevation: -2440.0 m * Penetration: 70 m * Recovery: 40.03 m * Location: South Atlantic Ocean * Campaign: Leg153 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 15 cores; 53.6 m cored; 0 m drilled; 74.7 % recovery
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
1ORDINAL NUMBEROrd NoGeocode
2Sample code/labelSample labelCoogan, Laurence ADSDP/ODP/IODP sample designation
3PlagioclasePl%Coogan, Laurence A
4ClinopyroxeneCpx%Coogan, Laurence A
5OlivineOl%Coogan, Laurence A
6Sample commentSample commentCoogan, Laurence Aanalysis
7MineralsMineralsCoogan, Laurence Aphase
8CommentCommentCoogan, Laurence Alocation
9Silicon dioxideSiO2%Coogan, Laurence AElectron Probe Microanalysis (EPMA)
10Titanium dioxideTiO2%Coogan, Laurence AElectron Probe Microanalysis (EPMA)
11Aluminium oxideAl2O3%Coogan, Laurence AElectron Probe Microanalysis (EPMA)
12Chromium(III) oxideCr2O3%Coogan, Laurence AElectron Probe Microanalysis (EPMA)
13Iron oxide, FeOFeO%Coogan, Laurence AElectron Probe Microanalysis (EPMA)total iron
14Manganese oxideMnO%Coogan, Laurence AElectron Probe Microanalysis (EPMA)
15Magnesium oxideMgO%Coogan, Laurence AElectron Probe Microanalysis (EPMA)
16Calcium oxideCaO%Coogan, Laurence AElectron Probe Microanalysis (EPMA)
17Sodium oxideNa2O%Coogan, Laurence AElectron Probe Microanalysis (EPMA)
18Calcium/(Calcium+Sodium+Potassium) ratioCa/(Ca+Na+K)Coogan, Laurence ACalculated
19Magnesium numberMg#Coogan, Laurence ACalculated
20TitaniumTimg/kgCoogan, Laurence AIon probe analysis
21StrontiumSrmg/kgCoogan, Laurence AIon probe analysis
22YttriumYmg/kgCoogan, Laurence AIon probe analysis
23ZirconiumZrmg/kgCoogan, Laurence AIon probe analysis
24LanthanumLamg/kgCoogan, Laurence AIon probe analysis
25CeriumCemg/kgCoogan, Laurence AIon probe analysis
26PraseodymiumPrmg/kgCoogan, Laurence AIon probe analysis
27NeodymiumNdmg/kgCoogan, Laurence AIon probe analysis
28SamariumSmmg/kgCoogan, Laurence AIon probe analysis
29EuropiumEumg/kgCoogan, Laurence AIon probe analysis
30GadoliniumGdmg/kgCoogan, Laurence AIon probe analysis1
31GadoliniumGdmg/kgCoogan, Laurence AIon probe analysis2
32TerbiumTbmg/kgCoogan, Laurence AIon probe analysis
33DysprosiumDymg/kgCoogan, Laurence AIon probe analysis
34HolmiumHomg/kgCoogan, Laurence AIon probe analysis
35ErbiumErmg/kgCoogan, Laurence AIon probe analysis
36YtterbiumYbmg/kgCoogan, Laurence AIon probe analysis
Size:
401 data points

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