Relationship between crystal morphology and twin boundary structures of quartz twinned in accordance with Japan law

Q4 Earth and Planetary Sciences Japanese Magazine of Mineralogical and Petrological Sciences Pub Date : 2017-01-01 DOI:10.2465/GKK.161220
K. Momma
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Abstract

Twinned crystals often grow larger and/or in diŠerent morphologies than coexisting single crystals. Such characteristics of twinned crystals are generally explained as a result of `reentrant corner eŠect'. However, observations of natural quartz crystals twinned in accordance with Japan law and computational simulations on the twin boundary structures revealed more complex growth mechanism, in which formation of dense Brazil twin lamellae at the {112̃2} composition plane of Japanese twin boundary causes the preferential growth of Japanese twin. The intersections of Brazil and Japanese twin boundaries were found to be structurally coherent when they have certain composition planes. This structural diversity of the {112̃2} Japanese twin boundaries causes development of ˆne Brazil twin lamellae and triggers faster growth.
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按日本法研究石英孪晶的晶体形态与孪晶边界结构的关系
孪晶通常比共存的单晶长得更大,或形态为diŠerent。孪生晶体的这种特性通常被解释为“可重入角eŠect”的结果。然而,根据日本法孪晶的天然石英晶体的观察和孪晶边界结构的计算模拟揭示了更为复杂的生长机制,在日本孪晶边界{112²}组成面形成致密的巴西孪晶片导致了日本孪晶的优先生长。当巴西和日本孪晶界的交点具有一定的组成平面时,它们在结构上是一致的。{1122}日本孪晶边界的结构多样性导致了{1122}巴西孪晶片层的发育,并引发了更快的生长。
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来源期刊
Japanese Magazine of Mineralogical and Petrological Sciences
Japanese Magazine of Mineralogical and Petrological Sciences Earth and Planetary Sciences-Economic Geology
CiteScore
0.20
自引率
0.00%
发文量
6
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