攀枝花钒钛磁铁矿中纳-微米尖晶石的出溶序次及其成因机制

张志彬; 黄菲; 刘开君; 彭艳东; 任亚群

doi:10.3799/dqkx.2018.417

Volume 43 Issue 5

May 2018

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Article Navigation > Earth Science > 2018 > 43(5): 1635-1649

Zhang Zhibin, Huang Fei, Liu Kaijun, Peng Yandong, Ren Yaqun, 2018. Sequence and Genetic Mechanism of Nano-Micron Spinel Exsolution from Panzhihua V-Ti Magnetite Deposit. Earth Science, 43(5): 1635-1649. doi: 10.3799/dqkx.2018.417

Citation:

Zhang Zhibin, Huang Fei, Liu Kaijun, Peng Yandong, Ren Yaqun, 2018. Sequence and Genetic Mechanism of Nano-Micron Spinel Exsolution from Panzhihua V-Ti Magnetite Deposit. Earth Science, 43(5): 1635-1649. doi: 10.3799/dqkx.2018.417

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Sequence and Genetic Mechanism of Nano-Micron Spinel Exsolution from Panzhihua V-Ti Magnetite Deposit

doi: 10.3799/dqkx.2018.417

1.
School of Resources and Civil Engineering, Northeastern University, Shenyang 110819, China
2.
School of Resources and Materials, Northeastern University, Qinhuangdao 066004, China

Received Date: 2017-08-22
Publish Date: 2018-05-15

Abstract

Abstract

Detailed characterization and formation mechanism of the spinel exsolution in titanomagnetite is crucial for reconstructing the composition of magnetite solid solution precursor and for application to the Fe-Ti oxide oxythermometer. The chemical composition, topographic characteristics and crystallographic relationships of spinel exsolution were studied systematically to probe into its sequence and genetic mechanism through petrographic observation and the integrated use of in-situ microanalysis methods. The results show that there are three output forms of the spinel exsolution. One spinel exsolution is on the edge of the titanomagnetite with Mg^# range from 60-70. Another is granular spinel exsolution distributing dispersedly with big particle-size, with Mg^# range from 71-77. The third spinel exsolution is present as lamellae parallelling to the {100} of the titanomagnetite with Mg^# range from 75-77. Three different types of spinel exsolution are all the magnesia-alumina spinel and have close-packed oxygen planes and directions parallel to those in the host magnetite with {111}_Mag//{111}_Spl, {110}_Mag//{110}_Spl and {100}_Mag//{100}_Spl respectively. Analysis suggests that three different types of spinel exsolution are all the product of the magnetite solid solution in the process of slow cooling with different sequence and genetic significance. The granular spinel exsolution in the titanomagnetite and the spinel exsolution on the edge of the titanomagnetite are related to some crystallographic defects in titanomagnetite and exsolved at the early stages of exsolution. The spinel lamellae exsolved in the way of spinodal decomposition parallelling to {l00}.
- Panzhihua,
- nano-micron,
- spinel exsolution,
- sequence,
- genetic mechanism

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References(101)

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