Storey, Michael; Kent, R W; Saunders, Andrew D; Salters, Vincent J M; Hergt, Janet M; Whitechurch, Hubert; Sevigny, James H; Thirlwall, Matthew F; Leat, Philip; Ghose, N C; Gifford, M (1992): Major and trace element analyses of ODP Leg 120 volcanic rocks (Table 1) [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.759908, Supplement to: Storey, M et al. (1992): Lower Cretaceous volcanic rocks on continental margins and their relationship to the Kerguelen Plateau. In: Wise, SW; Schlich, R; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 120, 33-53, https://doi.org/10.2973/odp.proc.sr.120.118.1992
Always quote citation above when using data! You can download the citation in several formats below.
Abstract:
Widespread Lower Cretaceous magmatism occurred along the Indian-Australian/Antarctic margins, and in the juvenile Indian Ocean, during the rifting of eastern Gondwana. The formation of this magmatic province probably began around 120-130 Ma with the eruption of basalts on the Naturaliste Plateau and at Bunbury, western Australia. On the northeast margin of India, activity began around 117 Ma with the Rajmahal continental basalts and associated lamprophyre intrusions. The formation of the Kerguelen Plateau in the Indian Ocean began no later than 114 Ma. Ultramafic lamprophyres (alnoites) were emplaced in the Prince Charles Mountains near the Antarctic continental margin at ~ 110 Ma. These events are considered to be related to a major mantle plume, the remnant of which is situated beneath the region of Kerguelen and Heard islands at the present day.
Geochemical data are presented for each of these volcanic suites and are indicative of complex interactions between asthenosphere-derived magmas and the continental lithosphere. Kerguelen Plateau basalts have Sr and Nd isotopic compositions lying outside the field for Indian Ocean mid-ocean ridge basalts (MORB) but, with the exception of Site 738 at the southern end of the plateau, within the range of more recent hotspot basalts from Kerguelen and Heard Islands. However, a number of the plateau tholeiites are characterized by lower 206Pb/204Pb ratios than are basalts from Kerguelen Island, and many also have anomalously high La/Nb ratios. These features suggest that the source of the Kerguelen Plateau basalts suffered contamination by components derived from the Gondwana continental lithosphere. An extreme expression of this lithospheric signature is shown by a tholeiite from Site 738, suggesting that the southernmost part of the Kerguelen Plateau may be underlain by continental crust.
The Rajmahal tholeiites mostly fall into two distinct geochemical groups. Some Group I tholeiites have Sr and Nd isotopic compositions and incompatible element abundances, similar to Kerguelen Plateau tholeiites from Sites 749 and 750, indicating that the Kerguelen-Heard mantle plume may have directly furnished Rajmahal volcanism. However, their elevated 207Pb/204Pb ratios indicate that these magmas did not totally escape contamination by continental lithosphere. In contrast to the Group I tholeiites, significant contamination is suggested for Group II Rajmahal tholeiites, on the basis of incompatible element abundances and isotopic compositions.
The Naturaliste Plateau and the Bunbury Basalt samples show varying degrees of enrichment in incompatible elements over normal MORB. The Naturaliste Plateau samples (and Bunbury Basalt) have high La/Nb ratios, a feature not inconsistent with the notion that the plateau may consist of stretched continental lithosphere, near the ocean-continent divide.
Project(s):
Ocean Drilling Program (ODP)
Coverage:
Median Latitude: -57.390250 * Median Longitude: 78.359775 * South-bound Latitude: -58.717000 * West-bound Longitude: 76.407500 * North-bound Latitude: -54.811000 * East-bound Longitude: 81.239500
Date/Time Start: 1988-03-09T06:45:00 * Date/Time End: 1988-04-23T04:00:00
Minimum Elevation: -2041.0 m * Maximum Elevation: -1080.0 m
Event(s):
120-747C * Latitude: -54.811000 * Longitude: 76.794000 * Date/Time Start: 1988-03-09T06:45:00 * Date/Time End: 1988-03-12T17:00:00 * Elevation: -1706.0 m * Penetration: 350.5 m * Recovery: 49.5 m * Location: South Indian Ridge, South Indian Ocean * Campaign: Leg120 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 16 cores; 144.5 m cored; 0 m drilled; 34.3 % recovery
120-748C * Latitude: -58.441000 * Longitude: 78.998100 * Date/Time Start: 1988-03-15T11:00:00 * Date/Time End: 1988-03-23T22:54:00 * Elevation: -1301.0 m * Penetration: 935 m * Recovery: 185.88 m * Location: South Indian Ridge, South Indian Ocean * Campaign: Leg120 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 87 cores; 760 m cored; 0 m drilled; 24.5 % recovery
120-749C * Latitude: -58.717000 * Longitude: 76.407500 * Date/Time Start: 1988-03-25T09:45:00 * Date/Time End: 1988-03-28T01:00:00 * Elevation: -1080.0 m * Penetration: 249.5 m * Recovery: 29.92 m * Location: South Indian Ridge, South Indian Ocean * Campaign: Leg120 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 16 cores; 147.5 m cored; 0 m drilled; 20.3 % recovery
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | Event label | Event | ||||
| 2 | Sample code/label | Sample label | Storey, Michael | DSDP/ODP/IODP sample designation | ||
| 3 | Silicon dioxide | SiO2 | % | Storey, Michael | X-ray fluorescence (XRF) | |
| 4 | Titanium dioxide | TiO2 | % | Storey, Michael | X-ray fluorescence (XRF) | |
| 5 | Aluminium oxide | Al2O3 | % | Storey, Michael | X-ray fluorescence (XRF) | |
| 6 | Iron oxide, Fe2O3 | Fe2O3 | % | Storey, Michael | X-ray fluorescence (XRF) | |
| 7 | Manganese oxide | MnO | % | Storey, Michael | X-ray fluorescence (XRF) | |
| 8 | Magnesium oxide | MgO | % | Storey, Michael | X-ray fluorescence (XRF) | |
| 9 | Calcium oxide | CaO | % | Storey, Michael | X-ray fluorescence (XRF) | |
| 10 | Sodium oxide | Na2O | % | Storey, Michael | X-ray fluorescence (XRF) | |
| 11 | Potassium oxide | K2O | % | Storey, Michael | X-ray fluorescence (XRF) | |
| 12 | Phosphorus pentoxide | P2O5 | % | Storey, Michael | X-ray fluorescence (XRF) | |
| 13 | Elements, total | Total | % | Storey, Michael | X-ray fluorescence (XRF) | |
| 14 | Loss on ignition | LOI | % | Storey, Michael | X-ray fluorescence (XRF) | |
| 15 | Quartz | Qz | % | Storey, Michael | CIPW Norm | |
| 16 | Corundum | Crn | % | Storey, Michael | CIPW Norm | |
| 17 | Orthoclase | Or | % | Storey, Michael | CIPW Norm | |
| 18 | Albite | Ab | % | Storey, Michael | CIPW Norm | |
| 19 | Anorthite | An | % | Storey, Michael | CIPW Norm | |
| 20 | Nepheline | Ne | % | Storey, Michael | CIPW Norm | |
| 21 | Diopside | Di | % | Storey, Michael | CIPW Norm | |
| 22 | Hypersthene | Hyp | % | Storey, Michael | CIPW Norm | |
| 23 | Olivine | Ol | % | Storey, Michael | CIPW Norm | |
| 24 | Montmorillonite | Mnt | % | Storey, Michael | CIPW Norm | |
| 25 | Ilmenite | Ilm | % | Storey, Michael | CIPW Norm | |
| 26 | Apatite | Ap | % | Storey, Michael | CIPW Norm | |
| 27 | Niobium | Nb | mg/kg | Storey, Michael | X-ray fluorescence (XRF) | |
| 28 | Zirconium | Zr | mg/kg | Storey, Michael | X-ray fluorescence (XRF) | |
| 29 | Yttrium | Y | mg/kg | Storey, Michael | X-ray fluorescence (XRF) | |
| 30 | Strontium | Sr | mg/kg | Storey, Michael | X-ray fluorescence (XRF) | |
| 31 | Rubidium | Rb | mg/kg | Storey, Michael | X-ray fluorescence (XRF) | |
| 32 | Gallium | Ga | mg/kg | Storey, Michael | X-ray fluorescence (XRF) | |
| 33 | Zinc | Zn | mg/kg | Storey, Michael | X-ray fluorescence (XRF) | |
| 34 | Nickel | Ni | mg/kg | Storey, Michael | X-ray fluorescence (XRF) | |
| 35 | Vanadium | V | mg/kg | Storey, Michael | X-ray fluorescence (XRF) | |
| 36 | Chromium | Cr | mg/kg | Storey, Michael | X-ray fluorescence (XRF) | |
| 37 | Barium | Ba | mg/kg | Storey, Michael | X-ray fluorescence (XRF) | |
| 38 | Lanthanum | La | mg/kg | Storey, Michael | X-ray fluorescence (XRF) | |
| 39 | Cerium | Ce | mg/kg | Storey, Michael | X-ray fluorescence (XRF) | |
| 40 | Neodymium | Nd | mg/kg | Storey, Michael | X-ray fluorescence (XRF) | |
| 41 | Lanthanum | La | mg/kg | Storey, Michael | Instrumental neutron activation analysis (INAA) (Reimann et al., 1998) | |
| 42 | Cerium | Ce | mg/kg | Storey, Michael | Instrumental neutron activation analysis (INAA) (Reimann et al., 1998) | |
| 43 | Neodymium | Nd | mg/kg | Storey, Michael | Instrumental neutron activation analysis (INAA) (Reimann et al., 1998) | |
| 44 | Samarium | Sm | mg/kg | Storey, Michael | Instrumental neutron activation analysis (INAA) (Reimann et al., 1998) | |
| 45 | Europium | Eu | mg/kg | Storey, Michael | Instrumental neutron activation analysis (INAA) (Reimann et al., 1998) | |
| 46 | Terbium | Tb | mg/kg | Storey, Michael | Instrumental neutron activation analysis (INAA) (Reimann et al., 1998) | |
| 47 | Ytterbium | Yb | mg/kg | Storey, Michael | Instrumental neutron activation analysis (INAA) (Reimann et al., 1998) | |
| 48 | Lutetium | Lu | mg/kg | Storey, Michael | Instrumental neutron activation analysis (INAA) (Reimann et al., 1998) | |
| 49 | Tantalum | Ta | mg/kg | Storey, Michael | Instrumental neutron activation analysis (INAA) (Reimann et al., 1998) | |
| 50 | Hafnium | Hf | mg/kg | Storey, Michael | Instrumental neutron activation analysis (INAA) (Reimann et al., 1998) | |
| 51 | Thorium | Th | mg/kg | Storey, Michael | Instrumental neutron activation analysis (INAA) (Reimann et al., 1998) | |
| 52 | Tungsten | W | mg/kg | Storey, Michael | Instrumental neutron activation analysis (INAA) (Reimann et al., 1998) | |
| 53 | Scandium | Sc | mg/kg | Storey, Michael | Instrumental neutron activation analysis (INAA) (Reimann et al., 1998) |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
1209 data points