Meijer, Arend (1976): (Tables 1-3) Pb and Sr isotopic data for sediments and rocks from DSDP holes in the Mariana island-arc system [dataset]. Department of Earth Sciences, University of California, Santa Barbara, PANGAEA, https://doi.org/10.1594/PANGAEA.719615
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Abstract:
Analyses of the isotopic composition of Pb in (1) western Pacific Ocean sediments [Jurassic(?) to Pleistocene in age, including clays and biogenic oozes], (2) Pacific Ocean basaltic rocks, (3) Mariana frontal arc volcanic rocks (Eocene to Miocene), and (4) Mariana active arc volcanic rocks [Pliocene (?) to Holocene] indicate that Pacific Ocean sediments could not have been a significant component of the source material for the Mariana arc volcanic rocks. Calculations involving the average concentrations and isotopic compositions of Pb in oceanic sediments, sea-floor basaltic rocks, and the Mariana arc volcanic rocks suggest that the sediment component must have been less than 1 percent of this source material.
The Pb isotopic compositions of the Mariana arc volcanic rocks lie, within experimental error, along the trend of available Pacific Ocean basalt analyses in versus 207Pb/204Pb versus 206Pb/204Pb and 208Pb/204Pb versus 206Pb/204Pb diagrams. Isotopic analyses of Pb in Pacific Ocean sediments do not lie along this trend; they have higher 207Pb/204Pb and 208Pb/204Pb values for comparable 206Pb/204Pb ratios. Clayey sediments generally have higher 208Pb/204Pb and 207Pb/204Pb ratios than biogenic oozes regardless of the age of the sediment.
Comparison of combined Sr and Pb isotopic analyses for (1) mantle-derived materials erupted through oceanic crust, (2) altered ocean-floor basaltic rocks, and (3) volcanic rocks from oceanic island arcs suggests that the Mariana arc volcanic rocks were derived, at least in part, from altered Pacific lithosphere subducted beneath the Mariana arc.
Unaltered basalts from the Mariana inter-arc basin (Mariana Trough) have Pb and Sr isotopic compositions that are very similar to those reported for some Hawaiian volcanic rocks but distinct from Mariana active and frontal arc compositions. These observations, in addition to existing major-and trace-element data, support a mantle origin for the interarc basin volcanic rocks. Dacites dredged from the Mariana remnant arc (South Honshu Ridge) have Pb isotopic compositions that are within experimental error of the active-arc analyses, consistent with a genetic relation.
Related to:
Meijer, Arend (1976): Pb and Sr isotopic data bearing on the origin of volcanic rocks from the Mariana island-arc system. Geological Society of America Bulletin, 87(9), 1358-1369, https://doi.org/10.1130/0016-7606(1976)87%3C1358:PASIDB%3E2.0.CO;2
Project(s):
Deep Sea Drilling Project (DSDP)
Coverage:
Median Latitude: 20.527213 * Median Longitude: 150.695212 * South-bound Latitude: 11.780000 * West-bound Longitude: 147.061700 * North-bound Latitude: 30.290700 * East-bound Longitude: 156.782700
Date/Time Start: 1969-07-09T00:00:00 * Date/Time End: 1971-10-26T00:00:00
Minimum Elevation: -6194.0 m * Maximum Elevation: -1479.0 m
Event(s):
6-52 * Latitude: 27.771700 * Longitude: 147.130000 * Date/Time: 1969-07-09T00:00:00 * Elevation: -5744.0 m * Penetration: 68.9 m * Recovery: 44.9 m * Location: North Pacific/PLAIN * Campaign: Leg6 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 10 cores; 68.9 m cored; 0 m drilled; 65.2 % recovery
6-59B * Latitude: 11.780000 * Longitude: 147.581700 * Date/Time: 1969-07-31T00:00:00 * Elevation: -5547.0 m * Penetration: 135.3 m * Recovery: 18.2 m * Location: North Pacific * Campaign: Leg6 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 6 cores; 46 m cored; 0 m drilled; 39.6 % recovery
7-61 * Latitude: 12.083700 * Longitude: 147.061700 * Date/Time: 1969-08-09T00:00:00 * Elevation: -5570.0 m * Penetration: 97 m * Recovery: 3 m * Location: North Pacific * Campaign: Leg7 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 2 cores; 12 m cored; 0 m drilled; 25 % recovery
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | Event label | Event | ||||
| 2 | Latitude of event | Latitude | ||||
| 3 | Longitude of event | Longitude | ||||
| 4 | Elevation of event | Elevation | m | |||
| 5 | Sample code/label | Sample label | Meijer, Arend | DSDP/ODP/IODP sample designation | ||
| 6 | Epoch | Epoch | Meijer, Arend | |||
| 7 | Lead-206/Lead-204 ratio | 206Pb/204Pb | Meijer, Arend | Isotope ratio mass spectrometry | ||
| 8 | Lead-207/Lead-204 ratio | 207Pb/204Pb | Meijer, Arend | Isotope ratio mass spectrometry | ||
| 9 | Lead-208/Lead-204 ratio | 208Pb/204Pb | Meijer, Arend | Isotope ratio mass spectrometry | ||
| 10 | Strontium-87/Strontium-86 ratio | 87Sr/86Sr | Meijer, Arend | Isotope ratio mass spectrometry | ||
| 11 | Lead | Pb | mg/kg | Meijer, Arend | ||
| 12 | Sample type | Samp type | Meijer, Arend | |||
| 13 | Description | Description | Meijer, Arend |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
121 data points
Data
| 1 Event | 2 Latitude | 3 Longitude | 4 Elevation [m] | 5 Sample label | 6 Epoch | 7 206Pb/204Pb | 8 207Pb/204Pb | 9 208Pb/204Pb | 10 87Sr/86Sr | 11 Pb [mg/kg] | 12 Samp type | 13 Description |
|---|---|---|---|---|---|---|---|---|---|---|---|---|
| 6-52 | 27.7717 | 147.1300 | -5744 | 6-52-1-1,90-92 | Miocene - Middle Pleistocene | 18.855 | 15.661 | 38.915 | clay | brown clay with ash (clay abundant, glass abundant, limonite and feldspar common, diatom rare) | ||
| 6-52 | 27.7717 | 147.1300 | -5744 | 6-52-3-1,130-132 | Miocene - Middle Pleistocene | 18.679 | 15.643 | 38.818 | clay | clay, silty clay, clayey silt (clay dominant, glass rare-common, zeolite rare) | ||
| 6-52 | 27.7717 | 147.1300 | -5744 | 6-52-7-2,90-92 | Cretaceous (?) | 18.543 | 15.598 | 38.710 | clay | clay (clay dominant, zeolite rare, glass, including palagonite, rare) | ||
| 6-52 | 27.7717 | 147.1300 | -5744 | 6-52-8-6,140-142 | Cretaceous (?) | 18.556 | 15.602 | 38.727 | clay | clay (clay dominant, zeolite common) | ||
| 6-59B | 11.7800 | 147.5817 | -5547 | 6-59B-2-3,110-112 | Early Miocene | 18.664 | 15.603 | 38.581 | ooze | radiolarian ooze (radiolarians abundant, diatom common, glass common, clay abundant, limonite, hematite and plagioclase rare-common) | ||
| 6-59B | 11.7800 | 147.5817 | -5547 | 6-59B-5-1,110-112 | Late Eocene - Early Oligocene | 18.666 | 15.620 | 38.791 | clay | zeolite clay (zeolite dominant, clay common, glass and palagonite common, plagioclase common) | ||
| 7-61 | 12.0837 | 147.0617 | -5570 | 7-61-1-1,33-34, piece 4 | Cretaceous (?) | 18.460 | 15.511 | 38.300 | 0.70432 | 0.95 | sea-floor basalt | basalt, coarse grained, ophitic texture (augite 40%, plagioclase 40%, olivine pseudomorphs 5%, opaques 4%, interstitial material 11%); olivine and some groundmass altered to clays |
| 20-196 | 30.1162 | 148.5748 | -6194 | 20-196-3-1,102-103 | Early Cretaceous | 18.845 | 15.683 | 38.955 | chert | chert, with clay | ||
| 20-197 | 30.2907 | 147.6743 | -6153 | 20-197-1-1,90-92, piece 22 | Cretaceous - Jurassic (?) | 18.515 | 15.429 | 37.690 | 0.70369 | 0.37 | sea-floor basalt | basalt, fine grained, intersertal texture (plagioclase 30%, augite 20%, opaques 15%, olivine pseudomorphs 1%), 34% glass with quench texture; alteration limited to olivine and some glass |
| 20-198A | 25.8257 | 154.5842 | -5958 | 20-198A-1-3,4-5 | Late Cretaceous | 18.586 | 15.629 | 38.727 | clay | zeolitic silty clay, clay (clay abundant, zeolite abundant, glass common, pumice rare) | ||
| 20-199 | 13.5130 | 156.1723 | -6100 | 20-199-1-2,80-81 | Eocene - Pliocene | 18.656 | 15.588 | 38.555 | ooze | foram-nannofossil ooze, Mn-micronodule, zeolite and palagonite bearing | ||
| 20-199 | 13.5130 | 156.1723 | -6100 | 20-199-2-1,95-96 | Middle Miocene - Eocene (?) | 18.693 | 15.584 | 38.624 | zeolitic clay | |||
| 20-199 | 13.5130 | 156.1723 | -6100 | 20-199-2-1,95-96 | Middle Miocene - Eocene (?) | 18.711 | 15.570 | 38.649 | zeolitic clay | |||
| 20-199 | 13.5130 | 156.1723 | -6100 | 20-199-6-5,135-136 | Early Miocene - Eocene | 18.683 | 15.545 | 38.627 | ash | ash, nannofossil bearing | ||
| 20-200 | 12.8367 | 156.7827 | -1479 | 20-200-1-CC | Pleistocene | 18.645 | 15.600 | 38.584 | ooze | foraminiferal ooze, nannofossil bearing | ||
| 20-200 | 12.8367 | 156.7827 | -1479 | 20-200-2-CC | Early Pliocene | 18.605 | 15.578 | 38.464 | ooze | forarniniferal ooze, nannofossil bearing | ||
| 20-200 | 12.8367 | 156.7827 | -1479 | 20-200-9-6,149-150 | Early Miocene | 18.595 | 15.598 | 38.615 | ooze | foraminiferal ooze, nannofossil bearing |