来自地幔过渡区的岩石:来自马来西亚,西南太平洋的大多数带有异岩
1Department of Earth Sciences, The University of Queensland, Brisbane, Qld 4072, Australia. Department of Earth Sciences, University of California Santa Cruz, Santa Cruz, CA 95064, USA.
概括
在马拉伊塔发现的深层地幔岩石揭示了超高压矿物质组合,包括多石和矿石,表明压力高达27千兆帕斯卡尔. 这些样本提供了下层地幔物质到达表面的证据.
科学领域:
- 地质地质地质地质地质地
- 矿物学是一门学科.
- 石化学 石化学是一门学科.
背景情况:
- 来自地幔过渡区 (400-670公里深) 的岩石在地表上很少见.
- 通爪高原是研究深层地球材料的独特地点.
研究的目的:
- 为了分析在Malaita上发现的高压矿物质聚合物,如石和巨晶.
- 为了确定这些深地岩石样本所记录的压力条件.
主要方法:
- 对石和大晶石的岩石分析.
- 矿物化学的地质化学分析 (大矿石,和-矿石,酸盐相,微钻石).
- 实证气温计对多数石榴石的应用.
主要成果:
- 发现了超高压矿物质组合,包括矿,矿,矿和微钻.
- 大多数石榴石显示压力高达22千兆帕斯卡尔.
- 其他矿物阶段表明压力达到27千兆帕斯卡尔.
结论:
- 分析的岩石起源于地幔过渡区和潜在的下层地幔.
- 来自下层地幔的酸超岩带来了这些深层岩石,大约在3400万年前将其带到表面.
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