Trace element systematics of ultramafic and mafic volcanic rocks from the 3 Ga North Caribou greenstone belt, northwestern Superior Province

被引:76
作者
Hollings, P [1 ]
Kerrich, R [1 ]
机构
[1] Univ Saskatchewan, Dept Geol Sci, Saskatoon, SK S7N 5E2, Canada
基金
加拿大自然科学与工程研究理事会;
关键词
Archean; geochemistry; komatiite; tholeiite;
D O I
10.1016/S0301-9268(98)00088-6
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
High precision trace element data from ultramafic and mafic volcanic rocks from two units of the similar to 3 Ga North Caribou greenstone belt in the northwestern Superior Province reveals new evidence for the contamination of early Archaean komatiites. Spinifex-textured komatiites (MgO = 20--27wt.%) of the Opapimiskan-Markop unit are characterised by flat to moderately enriched light rare earth element (LREE) trace element patterns (La/Sm-n = 1-2) in conjunction with negative Nb and Ti anomalies (Nb/La-pm = 0.48-0.59; Ti/Ti* = 0.6-0.8), consistent with contamination of a primary Munro-type Al-undepleted ultramafic melt by felsic material compositionally similar to Archaean tonalitic-trondhjemitic-granodioritic (TTG) suites. The trace element characteristics of these komatiites are distinct from both Proterozoic and Phanerozoic are and rift picrites. Mg-tholeiites intimately associated with the komatiites display variable rare earth elements (REE) (La/Sm-n = 0.8-1.5) and Nb and Ti anomalies also consistent with variable degrees of contamination (Nb/La-pm = 0.58-0.98; Ti/Ti* = 0.6-1.0). An intermediate suite of high-Mg andesites (54-60 wt.% SiO2) associated with both the tholeiites and the komatiites can be derived by fractional crystallisation of a melt with the trace element characteristics of the most contaminated komatiites. Compositionally uniform Mg-to Fe-tholeiites of the South Rim unit are believed to overlie the Opapimiskan-Markop unit, possibly in stratigraphic contact. They are characterised by flat trace element patterns (La/Sm-n = 0.9-1.0), are uncontaminated, and comparable with modern day oceanic plateaux, such as Ontong Java. The two units likely represent the eruptive products of a single mantle plume that entrained tholeiitic melts from the upper mantle before impinging upon the Archaean crust at similar to 3 Ga. (C) 1999 Elsevier Science B.V. All rights reserved.
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收藏
页码:257 / 279
页数:23
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