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首页> 外文期刊>European journal of mineralogy >jade gouge from Emirau Island, Papua New Guinea (Early Lapita context, 3300 BP): a unique jadeitite
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jade gouge from Emirau Island, Papua New Guinea (Early Lapita context, 3300 BP): a unique jadeitite

机译:来自巴布亚新几内亚的埃米尔瑙岛的玉凿(早期拉皮塔语,3300 BP):一种独特的翡翠

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A small stone artifact fashioned as a wood-carving gouge, discovered during an archaeological excavation on Emirau Island, Bismarck Archipelago, Papua New Guinea, has been determined to consist of jadeitite - jadeite jade. It is very unusual with respect to both pyroxene composition and minor mineral constituents. Pyroxene compositions lie essentially along the jadeite-aegirine join: Jd_(94)Ae_6 to Jd_(63)Ae_(36), and without any coexisting omphacite. This contrasts with Jd-Di or Jd-Aug compositional trends commonly observed in jadeitites worldwide. Paragonite and albite occur in veins and cavities with minor titanite, epidote-allanite, and zircon, an assemblage seen in a few jadeitites. Surprisingly, some titanite contains up to 6 wt% Nb_2O_5 with only trace Ta and a single grain of a Y-Nb phase (interpreted as fergusonite) is present; these are unique for jadeitite. A possible source is along the Torare River in northeast Papua, Indonesia, from which samples of "chloromelanite" (actually jadeitite) were collected by C.E.A. Wichmann in 1903 near Humboldt Bay along with stone adzes fashioned from the same material.
机译:在巴布亚新几内亚的s斯麦群岛的埃米尔瑙岛的考古发掘过程中发现的一种细小的木制品,像木头凿子,已被确定为翡翠-翡翠。就辉石成分和微量矿物质成分而言,这是非常不寻常的。辉石成分基本沿翡翠-金刚玉连接:Jd_(94)Ae_6至Jd_(63)Ae_(36),并且没有任何共存的绿辉石。这与全球翡翠中常见的Jd-Di或Jd-Aug成分趋势形成鲜明对比。石蜡石和钠长石出现在静脉和空腔中,并伴有少量的钛铁矿,显辉石-白云母和锆石,在一些翡翠中可见。出人意料的是,一些钛铁矿含有高达6 wt%的Nb_2O_5,仅含有痕量的Ta,并且存在一个单晶的Y-Nb相(被解释为铁矾)。这些对于翡翠来说是独一无二的。一个可能的来源是印度尼西亚巴布亚东北部的托拉雷河沿岸,C.E.A。公司从那里收集了“氯黑石”(实际上是翡翠)样品。 Wichmann于1903年在洪堡湾附近,并用相同的材​​料制成了石雕。

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