Age, geochemistry and zircon Hf isotope of the alkaline basaltic rocks in the middle section of the Yan-Liao aulacogen along the northern margin of the North China Craton: New evidence for the breakup of the Columbia Supercontinent
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摘要: 本文报导了华北克拉通北缘燕辽裂陷槽中部长城系大红峪组、团山子组碱性玄武质岩和侵入串岭沟组基性岩脉的岩石学、地球化学以及锆石SHRIMP U-Pb年龄和Hf同位素特征。结合区域地质资料与前人研究成果,对这些碱性玄武岩与基性岩脉的时代问题、岩浆岩起源和源区类型以及岩浆作用的动力学背景进行了讨论。研究表明大红峪组碱性玄武岩和串岭沟组基性岩脉分别形成于1624±9Ma和1620±9Ma,二者在误差范围内一致;这些基性岩浆岩普遍具有高的Zr含量(94×10-6~196×10-6)、富集轻稀土((La/Yb)N=10.63~ 21.97)及大离子亲石元素,大多数样品无明显的Eu异常,微量元素组成与OIB相似。锆石Hf同位素显示弱亏损特征,ε Hf(t)值为 -0.6~3.8。燕辽裂陷槽中部长城系碱性岩的原始岩浆可能起源于同一软流圈地幔源区的低程度部分熔融(2%~3%),且有岩石圈地幔物质加入。岩浆受地壳混染的程度低,经历了强烈的结晶分异作用。研究进一步表明,燕辽裂陷槽中部长城系碱性岩从1635Ma(团山子组)开始喷发,1625Ma达到峰期,大红峪组地层沉积时间晚于1635Ma。联系该阶段全球各大陆情况,华北地区该期的碱性岩岩浆事件应与哥伦比亚超大陆裂解有关。
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关键词:
- 碱性岩 /
- 锆石U-Pb年代学和Lu-Hf同位素 /
- 哥伦比亚超大陆裂解 /
- 燕辽裂陷槽 /
- 华北克拉通
Abstract: In this contribution, we reported geochemistry, zircon U-Pb ages and Lu-Hf isotopes of the alkali basalt (Dahongyu and Tuanshanzi formations) and mafic dyke (Chuanlinggou Formation) from the Early Mesoproterozoic Changchengian System in Yan-Liao aulacogen along the northern margin of the North China Craton (NCC). Together with regional geology and previous research, we discuss the time, source and geodynamic regime of these basic rocks. The SHRIMP zircon U-Pb ages of alkaline basalt and mafic dyke are coeval, 1624±9Ma and 1620±9Ma respectively. All the studied basic rocks share similar geochemical feature: alkaline, high Zr content (94×10-6~196×10-6), enrichment in light rare earth elements (LREE) ((La/Yb)N=10.63~21.97) and large ion lithophile element (LILE); insignificant Eu anomaly, trace element characteristics resemble those of oceanic island basalt (OIB-like). Zircon εHf(t) values range from -0.6 to 3.8, indicating slightly depleted signature. The primitive magma of these basic rocks were derived from low-degree partial melting (2%~3%) of asthenospheric mantle source with minor involvement of lithospheric mantle materials and insignificant crust contamination, intensive crystal fractionation took place before eruption and emplacement. The alkaline magmatism eruption in Yan-liao aulacogen initiated at ca.1635Ma and peaked at ca.1625Ma. Thus, the depositional age of the Dahongyu Formation was younger than ca.1635Ma. Comparing with the other continents around world at that time, the Mesoproterozoic igneous activity in the Yan-Liao aulacogen were most possibly related with the break-up of the Columbia Supercontinent. -
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