The subducted component in island arc lavas: constraints from Be isotopes and B-Be systematics
Although high concentrations of beryllium-10 and boron are taken as unequivocal indicators of the contribution of subducting plates, controversy persists about the processes by which material is transferred from slabs to the sources of arc magmas. Data on (10)Be/Be and B/Be ratios from four arcs sug...
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| Published in | Nature (London) Vol. 344; no. 6261; pp. 31 - 36 |
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| Main Authors | , , |
| Format | Journal Article |
| Language | English |
| Published |
London
Nature Publishing
01.03.1990
Nature Publishing Group |
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| Abstract | Although high concentrations of beryllium-10 and boron are taken as unequivocal indicators of the contribution of subducting plates, controversy persists about the processes by which material is transferred from slabs to the sources of arc magmas. Data on (10)Be/Be and B/Be ratios from four arcs suggest that the contribution from the slab is compositionally homogeneous in each arc and that subducted boron is not stored in the sub-arc mantle. The link between subduction and magma-tism at convergent margins seems to be well regulated. |
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| AbstractList | Although high concentrations of beryllium-10 and boron are taken as unequivocal indicators of the contribution of subducting plates, controversy persists about the processes by which material is transferred from slabs to the sources of arc magmas. Data on 10Be/Be and B/Be ratios from four arcs suggest that the contribution from the slab is compositionally homogeneous in each arc and that subconnected boron is not stored in the sub-arc mantle. The link between subduction and magmatism at convergent margins seems to be well regulated. Although high concentrations of beryllium-10 and boron are taken as unequivocal indicators of the contribution of subducting plates, controversy persists about the processes by which material is transferred from slabs to the sources of arc magmas. Data on (10)Be/Be and B/Be ratios from four arcs suggest that the contribution from the slab is compositionally homogeneous in each arc and that subducted boron is not stored in the sub-arc mantle. The link between subduction and magma-tism at convergent margins seems to be well regulated. Although high concentrations of beryllium-10 and boron are taken as unequivocal indicators of the contribution of subducting plates, controversy persists about the processes by which material is transferred from slabs to the sources of arc magmas. Data on super(10)Be/Be and B/Be ratios from four arcs suggest that the contribution from the slab is compositionally homogeneous in each arc and that subducted boron is not stored in the sub-arc mantle. The link between subduction and magmatism at convergent margins seems to be well regulated. Both are strongly enriched in many volcanic arc lavas relative to mid-ocean-ridge basalts (MORBs), ocean-island basalts (OIBs) and reservoirs in the upper plate. Because the budget of these elements in arc magmas is dominated by the subducted component (ocean sediments, altered crust, or melts/fluid derived therefrom), the Be-B systematics of arc lavas are insensitive to chemical variation in the mantle and are largely unaffected by involvement of continental crust. By contrast, 10Be concentrations in mantlederived magmas from mid-ocean ridges, ocean islands and active continental rifts are generally below detection limits (<1 x 106 atom g_1) with a 10Be/Be atom ratio of <5xlO-11 (refs 7, 8). Because of its short half-life, the high 10Be concentrations (1-24 x 106 atom g_1; refs 7,9) and the high 10Be/9Be ratios (1-81 x КΓ11; refs 8-10) measured in many arc lavas require recent incorporation of a component derived from young sediments7. [...]assimilation is more likely to spoil systematics than to produce them. [...]shown are fields for high-10Be pelagic sediments and high-B altered oceanic crust. Because little data yet exist to define end-member characteristics, fields in Fig. 2 are drawn to cover about twice the range of reported data. |
| Author | Morris, J. D Leeman, W. P Tera, F |
| Author_xml | – sequence: 1 givenname: J. D surname: Morris fullname: Morris, J. D – sequence: 2 givenname: W. P surname: Leeman fullname: Leeman, W. P – sequence: 3 givenname: F surname: Tera fullname: Tera, F |
| BackLink | http://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&idt=6913505$$DView record in Pascal Francis https://www.ncbi.nlm.nih.gov/pubmed/18278019$$D View this record in MEDLINE/PubMed |
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| CODEN | NATUAS |
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| Keywords | Marine sediments Island arcs Be-10/Be-9 Isotope geochemistry Melange Fluid phase Mass transfer Subduction Boron Upper mantle Models Plate convergence Recycling Oceanic crust |
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| Snippet | Although high concentrations of beryllium-10 and boron are taken as unequivocal indicators of the contribution of subducting plates, controversy persists about... Both are strongly enriched in many volcanic arc lavas relative to mid-ocean-ridge basalts (MORBs), ocean-island basalts (OIBs) and reservoirs in the upper... |
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| SubjectTerms | Basalt Beryllium Beryllium 10 Boron Chemistry Continental crust Crystalline rocks Detection limits Earth Earth sciences Earth, ocean, space Exact sciences and technology Geology Igneous and metamorphic rocks petrology, volcanic processes, magmas Island arcs Isotope geochemistry Isotope geochemistry. Geochronology Isotopes Lava Magma Marine Melts Mid-ocean ridges Oceanic crust Oceans Organic chemistry Pelagic sediments Plate tectonics Ratios Sediments Slabs Systematics Trends |
| Title | The subducted component in island arc lavas: constraints from Be isotopes and B-Be systematics |
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