Discovery of the Late Carboniferous adakite in the Erenhot-Hegenshan suture zone and intra-oceanic subduction of the Paleo-Asian Ocean
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摘要:
内蒙古二连—贺根山缝合带额很傲包图英云闪长岩体，出露于西乌旗梅劳特乌拉SSZ型蛇绿岩带北侧。为了确定该岩体的岩石成因类型，探讨其构造环境及古亚洲洋俯冲消亡过程，对该岩体进行了岩石学、地球化学和LA-ICP-MS锆石U-Pb年代学研究。额很傲包图英云闪长岩高硅富铝，富钠贫钾，高锶低钇，富集Rb、Ba、Sr等大离子亲石元素和LREE，亏损Nb、Ta、Ti、P等高场强元素和HREE，无明显Eu异常。岩石学和岩石地球化学特征表明，该英云闪长岩体为高Si埃达克岩（HSA），形成于岛弧环境，具有洋内俯冲洋壳+俯冲深积物部分熔融并与上覆地幔楔橄榄岩反应成因特征。锆石LA-ICP-MS U-Pb测年表明，额很傲包图英云闪长岩体的侵位年龄为（305.6±1.5）Ma，形成时代为晚石炭世。结合二连—贺根山缝合带石炭纪蛇绿岩、石炭纪—二叠纪岛弧型岩浆岩的时空分布与演化特征，认为古亚洲洋二连—贺根山洋盆在石炭纪—早二叠世处于以洋内俯冲为特征的大洋俯冲消亡过程中。
Abstract:The Ehenaobaotu tonalite is outcropped in the northern part of the Meilaotewula SSZ-type ophiolite of the Erenhot-Hegenshan suture zone in Xi Ujimqin Banner of Inner Mongolia. Based on the study of petrology, geochemistry and zircon LA-ICP-MS U-Pb geochronology, the genetic type and tectonic setting of the tonalite were determined, and the final closure time and subduction process of the Erenhot-Hegenshan ocean basin of the Paleo-Asian Ocean were discussed. The tonalite is characterized by high SiO2, Al2O3, Na2O, Sr and low K2O, Y contents, enrichment of Rb, Ba, Sr large ion lithophile elements and LREE, and depletion of Nb, Ta, Ti, P high field strength elements and HREE. There is no pronounced Eu anomaly. The lithological and geochemical characteristics show that the Ehenaobaotu pluton is a high Si adakite (HSA) formed in island arc, and was derived from patial melting of the intra-oceanic subductingd oceanic crust and sediment and subsequently reaction with overlying mantle wedge peridotite. Its U-Pb LA-ICP-MS dating yields (305.6±1.5) Ma and suggests that the Ehenaobaotu pluton was formed during Late Carboniferous. Combined with the study of spatio-temporal evloution of the Carboniferous ophiolites and Carboniferous-Permian island arc magmatic rocks in the Erenhot-Hegenshan suture, it is assumed that the Erenhot-Hegenshan oceanic basin of the Paleo-Asian Ocean was in the process of oceanic subduction characterized by intra-oceanic subduction during the Carboniferous-Early Permian.
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图 1 额很傲包图英云闪长岩大地构造单元图(a)(修改自Miao et al., 2008), 区域地质图(b), 地质图(c), 野外照片(d)和显微照片(e)
Figure 1.
图 4 额很傲包图英云闪长岩铝饱和指数(A/NK-A/CNK)图解（据Maniar and Piccoli, 1989
Figure 4.
图 5 额很傲包图英云闪长岩TAS分类图（据Middlemost, 1994）
Figure 5.
图 6 额很傲包图英云闪长岩An-Ab-Or分类图解（据O'Connor, 1965）
Figure 6.
图 7 额很傲包图英云闪长岩稀土元素球粒陨石标准化配分模式(球粒陨石标准化数值据Boynton, 1984; 高Si埃达克岩据Martin et al., 2005)
Figure 7.
图 8 额很傲包图英云闪长岩微量元素原始地幔标准化蛛网图(原始地幔标准化数值据Sun and McDonough, 1989; 高Si埃达克岩据Martin et al., 2005)
Figure 8.
图 9 额很傲包图英云闪长岩Y-Sr/Y构造判别图解(据Defant and Drummond, 1990; Martin, 1999; 高Si埃达克岩据Martin et al., 2005）
Figure 9.
图 10 额很傲包图英云闪长岩SiO2-MgO、(CaO+NaO2)-Sr、Y-Sr/Y和SiO2-Nb图解(据Martin et al., 2005)
Figure 10.
图 11 额很傲包图英云闪长岩(Y+Nb)-Rb（a）及(Yb+Ta)-Rb（b）构造判别图解（据Pearce, 1984；高Si埃达克岩据Martin et al., 2005）
Figure 11.
表 1 额很傲包图英云闪长岩（PS1-10）LA-ICP-MS锆石U-Pb测试结果
Table 1. LA-ICP-MS U-Pb dating of zircons from the Ehenaobaotu tonalite
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表 2 额很傲包图英云闪长岩主量（%）、微量和稀土（10-6）元素分析结果
Table 2. Major element(%), trace element and REE analyses(10-6)of the Ehenaobaotu tonalite
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表 3 额很傲包图英云闪长岩和高Si埃达克岩平均成分
Table 3. Average compositions of the Ehenaobaotu tonalite and high-SiO2 adakites
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