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Boron Cycling in Subduction Zones
被引:46
|作者:
Palmer, Martin R.
[1
]
机构:
[1] Univ Southampton, Sch Ocean & Earth Sci, Southampton SO14 3ZH, Hants, England
来源:
关键词:
subduction zones;
water;
serpentinite;
phengite;
crustal recycling;
MARIANA FORE-ARC;
ISOTOPIC COMPOSITION;
CRUSTAL ASSIMILATION;
SYSTEMATICS;
MANTLE;
SEDIMENTS;
INSIGHTS;
LITHIUM;
FLUIDS;
ROCKS;
D O I:
10.2138/gselements.13.4.237
中图分类号:
P3 [地球物理学];
P59 [地球化学];
学科分类号:
0708 ;
070902 ;
摘要:
Subduction zones are geologically dramatic features, with much of the drama being driven by the movement of water. The "light and lively" nature of boron, coupled with its wide variations in isotopic composition shown by the different geo-players in this drama, make it an ideal tracer for the role and movement of water during subduction. The utility of boron ranges from monitoring how the fluids that are expelled from the accretionary prism influence seawater chemistry, to the subduction of crustal material deep into the mantle and its later recycling in ocean island basalts.
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页码:237 / 242
页数:6
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