NaAlSi3O8-hollandite and other high-pressure minerals in the shock melt veins of the Suizhou meteorite |
| |
Authors: | Xie Xiande Chen Ming Wang Deqiang A El Goresy |
| |
Institution: | (1) Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, 510640 Guangzhou, China;(2) Max-Planck-Institute für Chemie, 55128 Mainz, Germany |
| |
Abstract: | The Suizhou L6 chondrite contains a few very thin shock melt veins of 0.02–0.09 mm in width. In spite of small width of the
veins, shock-induced high-pressure phases, such as coarse-grained NaAlSi3O8-hollandite, ringwoodite, majorite and fine-grained matrix majorite-pyropess have been discovered in these veins. NaAlSi3O8-hollandite, the high-pressure phase of plagioclase, in Suizhou shock veins occurs as a single phase mineral, no silicate
glassy phase, such as albitic glass, was incorporated with it. The presence of above-mentioned high-pressure phases constrains
the high pressure (up to 23–24 GPa) and high temperature (up to 1900–2000°C) regime in Suizhou shock veins, and indicates
that the duration of high-pressure regime in the veins should be long enough (a few seconds) for phase transformation and
crystallization of minerals under pressure. The discovery of the first natural single-phase crystalline NaAlSi3O8-hollandite in Suizhou meteorite is of important significance in understanding the Earth’s mantle geochemistry. |
| |
Keywords: | chondrite shock vein high-pressure phase plagioclase hollandite |
本文献已被 SpringerLink 等数据库收录! |
| 点击此处可从《中国科学通报(英文版)》浏览原始摘要信息 |
| 点击此处可从《中国科学通报(英文版)》下载免费的PDF全文 |
|