期刊
GEOLOGICAL MAGAZINE
卷 152, 期 2, 页码 210-224出版社
CAMBRIDGE UNIV PRESS
DOI: 10.1017/S0016756814000259
关键词
high-alumina basalt; mantle heterogeneity; asthenosphere; subcontinental lithospheric mantle; two-stage model
资金
- CAS/SAFEA International Partnership Program for Creative Research Teams (Intraplate Mineralization Research Team) [KZZD-EW-TZ-20]
- 12th Five-Year Plan project of the State Key Laboratory of Ore Deposit Geochemistry, Chinese Academy of Sciences [SKLOG-ZY125-06]
The Early Palaeozoic Shuanggou ophiolite is the best-preserved part of the Ailaoshan ophiolite belt. The microgabbros (basaltic dykes) and basalts (basaltic lavas) show distinct characteristics in geochemistry, implying that their genetic mechanisms are different. With Al2O3 contents ranging from 14.7% to 17.0%, the microgabbros belong to low-alumina type. They exhibit normal mid-ocean-ridge basalt (N-MORB) -like trace elemental characteristics with positive epsilon(Nd)(t) values (9.7-11.6) and slightly variable (Sr-87/Sr-86)(i) ratios (0.7036-0.7046). In contrast, the basalts have high Al2O3 contents (19.5-23.2%), therefore belonging to high-alumina type. A plagioclase-accumulation model is used to account for the high alumina contents. Moreover, the basalts have enriched MORB (E-MORB) -like trace element characteristics with lower epsilon(Nd)(t) values (6.4-8.0) and (Sr-87/Sr-86)(i) ratios (0.7032-0.7036). Their incompatible element ratios exhibit linear correlation with the isotopic data, which is probably related to the contribution of a mixed lithosphere-asthenosphere source. In summary, a two-stage model is proposed to explain the formation of the Shuanggou ophiolite: (1) at the continent-ocean transition stage, the basalts were generated by low-degree partial melting of the mixed mantle near a slow-spreading embryonic centre; and (2) at the mature stage of the Ailaoshan Ocean, the microgabbros were produced by moderate-degree partial melting of the depleted asthenospheric mantle.
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