西藏依拉山蛇绿岩中铬铁矿特征及构造背景
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摘要
依拉山蛇绿岩位于班公湖-怒江缝合带中部,主要由蚀变较强的方辉橄榄岩和纯橄岩及豆荚状铬铁岩组成。铬铁矿矿体集中分布在依拉山岩体北部,围岩以纯橄岩为主,少量为方辉橄榄岩。铬铁岩中铬尖晶石的电子探针分析结果表明Cr~#值为64.2～73.9,Mg~#值为46.9～71.6,TiO_2为0.03%～0.31%,Al_2O_3为4.5%～18.7%,指示依拉山铬铁矿为高铬型铬铁矿。方辉橄榄岩的稀土元素及微量元素配分模式指示其具有深海地幔橄榄岩的特征,铬铁矿的铂族元素具有IPGE富集而PPGE亏损的特点,呈现出右倾的配分模式,且Pd/Ir与Pt/Pt~*之间不存在明确的相关性,反映出依拉山岩体经历了岩石-熔体反应的演化过程。结合其他岩体内铬铁矿的对比研究,提出依拉山铬铁矿可能是在俯冲带环境下,由玻安质熔体与岩石反应形成,并经历了多阶段的演化过程,即早期的洋中脊(MORB)环境以及后期的俯冲带(SSZ)的改造。
Yilashan ophiolite, located in the middle section of the Bangong lake-Nujiang suture zone, contains predominantly strongly-altered harzburgite and dunite, as well as podiform chromitite.The chromitite orebodies in the Yilashan area are mainly distributed in the northern part of the ophiolite, and consist mainly of dunite with minor amount of harzburgite. Electron microprobe analysis shows that the chromian spinel in the Yilashan chromite has Cr~# values of 64.2～73.9, 46.9～71.6 of Mg~#, TiO_2 of 0.03%～0.31%, Al_2O_3 of 4.5%～18.7%, indicating that the Yilashan chromite should be high-Cr type chromite. The distribution patterns of REEs and trace elements of the Yilashan harzburgite are indicative of abyssal peridotite.The platinum group elements of chromite show enrichment of IPGE and depletion of PPGE, with right-dipping distribution patterns and no clear correlation between Pd/Ir and Pt/Pt~*, reflecting that the Yilashan ophiolite had experienced the rock-melt reaction.Comparison study with other chromite ores suggests that the Yilashan chromite may be formed by the reaction of boninite melt with rocks in the subduction belt environment and undergo a multi-stage evolution process, i.e. the early MORB environment and the transformation of the late suprasubduction zone(SSZ).
Yilashan ophiolite, located in the middle section of the Bangong lake-Nujiang suture zone, contains predominantly strongly-altered harzburgite and dunite, as well as podiform chromitite.The chromitite orebodies in the Yilashan area are mainly distributed in the northern part of the ophiolite, and consist mainly of dunite with minor amount of harzburgite. Electron microprobe analysis shows that the chromian spinel in the Yilashan chromite has Cr~# values of 64.2～73.9, 46.9～71.6 of Mg~#, TiO_2 of 0.03%～0.31%, Al_2O_3 of 4.5%～18.7%, indicating that the Yilashan chromite should be high-Cr type chromite. The distribution patterns of REEs and trace elements of the Yilashan harzburgite are indicative of abyssal peridotite.The platinum group elements of chromite show enrichment of IPGE and depletion of PPGE, with right-dipping distribution patterns and no clear correlation between Pd/Ir and Pt/Pt~*, reflecting that the Yilashan ophiolite had experienced the rock-melt reaction.Comparison study with other chromite ores suggests that the Yilashan chromite may be formed by the reaction of boninite melt with rocks in the subduction belt environment and undergo a multi-stage evolution process, i.e. the early MORB environment and the transformation of the late suprasubduction zone(SSZ).
引文
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