新疆西南天山超高压变质带的形成与演化
The formation and tectonic evolution of UHP metamorphic belt in southwestern Tianshan, Xinjiang
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摘要: 本文系统地总结了近年来有关新疆西南天山超高压变质带在野外地质产状、岩石学、矿物学、地球化学和年代学等方面研究取得的进展。根据野外地质产状特征,西南天山出露的榴辉岩可以分为三类:即在蓝片岩中呈透镜体的块状榴辉岩、保存有玄武岩岩枕的枕状榴辉岩和夹杂在大理岩中的条带状榴辉岩。详细的岩石学研究表明它们都经历过超高压变质作用,其变质作用演化经历了3个阶段:峰期榴辉岩阶段(560~600℃,4.95~5.07GPa)、主期榴辉岩阶段(598~496℃,25.72~26.66±1kbar)和退变绿帘石蓝片岩相阶段。地球化学研究显示其原岩相当于源于富集地幔的(ε_(Nd)-1.4~-0.4)具有 OIB 特点的变碱性玄武岩、源于亏损地幔的(ε_(Nd)= 6.7~ 7.4)具有 NMORB 特点的洋中脊玄武岩和源于较富集地幔的(ε_(Nd)=-2.5~ 3.2)具有 EMORB 特点的洋中脊玄武岩,它们形成于海山环境下的洋壳。榴辉岩中锆石 SHRIMP定年结果表明榴辉岩的原岩形成于石炭纪(>310Ma)之前,洋壳开始俯冲发生在二叠纪末(280~290Ma),高压一超高压变质发生在三叠纪(220~230Ma)。结合在其北侧低压麻粒岩带的发现,提出了新疆西南天山超高压变质带双变质带构造演化模式。
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