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Domain structures in rutile in ultrahigh-pressure metamorphic rocks from Dabie Mountains, China; Domain structures in rutile in ultrahigh-pressure metamorphic rocks from Dabie Mountains, China
D. W. Meng; X. L. Wu; X. Meng; Y. J. Han; D. Li
2004 ; 2004
发表期刊Micron ; Micron
ISSN0968-4328 ; 0968-4328
卷号35期号:6页码:441-445
摘要According to the HRTEM study, the UHP jadeite-quartzite mineral (Rutile, TiO2) in Anhui Province, Dabie Mountains, China, has ultrastructures such as <011> two-dimensional commensurable modulated structures or superstructures, {011} twin domain structures, dislocations and crystal deformations. The SAED patterns and HRTEM images indicate the existence of the deformations and stacking faults on the interface of {011} twin crystal of rutile and its two-dimensional commensurate modulated structures with repetition period 0.753 nm (3d(011)) has tetragonal symmetry, cell parameters a = 3a(0) = 1.377 nm (a(0) = 0.459 nm), c = c(0) = 0.3 nm. The modulated structures of rutile were probably caused by the isomorphic replacement of Ti4+ and position modulation or occupation modulation of oxygen atoms in different degree; the deformation structures reveal that during the process of crystallization and mineralization, this mineral may be affected by the geological environment (such as temperature, pressure and stress), metamorphism and deformation. (C) 2004 Elsevier Ltd. All rights reserved.; According to the HRTEM study, the UHP jadeite-quartzite mineral (Rutile, TiO2) in Anhui Province, Dabie Mountains, China, has ultrastructures such as <011> two-dimensional commensurable modulated structures or superstructures, {011} twin domain structures, dislocations and crystal deformations. The SAED patterns and HRTEM images indicate the existence of the deformations and stacking faults on the interface of {011} twin crystal of rutile and its two-dimensional commensurate modulated structures with repetition period 0.753 nm (3d(011)) has tetragonal symmetry, cell parameters a = 3a(0) = 1.377 nm (a(0) = 0.459 nm), c = c(0) = 0.3 nm. The modulated structures of rutile were probably caused by the isomorphic replacement of Ti4+ and position modulation or occupation modulation of oxygen atoms in different degree; the deformation structures reveal that during the process of crystallization and mineralization, this mineral may be affected by the geological environment (such as temperature, pressure and stress), metamorphism and deformation. (C) 2004 Elsevier Ltd. All rights reserved.
部门归属china univ geosci, testing ctr, wuhan 430074, peoples r china. chinese acad sci, met res inst, shenyang natl lab mat sci, shenyang 110016, peoples r china. wuhan univ, fac foreign language, wuhan 430070, peoples r china.;meng, dw (reprint author), china univ geosci, testing ctr, wuhan 430074, peoples r china;dwmeng@cug.edu.cn ; china univ geosci, testing ctr, wuhan 430074, peoples r china. chinese acad sci, met res inst, shenyang natl lab mat sci, shenyang 110016, peoples r china. wuhan univ, fac foreign language, wuhan 430070, peoples r china.;meng, dw (reprint author), china univ geosci, testing ctr, wuhan 430074, peoples r china;dwmeng@cug.edu.cn
关键词Ultrahigh-pressure Metamorphic Rocks Ultrahigh-pressure Metamorphic Rocks Rutile Rutile Domain Structure Domain Structure Tem Tem Dabic Mountains Dabic Mountains Eclogites Eclogites Anatase Anatase Tio2 Tio2 Tem Tem
URL查看原文 ; 查看原文
WOS记录号WOS:000221721000007 ; WOS:000221721000007
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被引频次:5[WOS]   [WOS记录]     [WOS相关记录]
文献类型期刊论文
条目标识符http://ir.imr.ac.cn/handle/321006/35501
专题中国科学院金属研究所
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GB/T 7714
D. W. Meng,X. L. Wu,X. Meng,et al. Domain structures in rutile in ultrahigh-pressure metamorphic rocks from Dabie Mountains, China, Domain structures in rutile in ultrahigh-pressure metamorphic rocks from Dabie Mountains, China[J]. Micron, Micron,2004, 2004,35, 35(6):441-445, 441-445.
APA D. W. Meng,X. L. Wu,X. Meng,Y. J. Han,&D. Li.(2004).Domain structures in rutile in ultrahigh-pressure metamorphic rocks from Dabie Mountains, China.Micron,35(6),441-445.
MLA D. W. Meng,et al."Domain structures in rutile in ultrahigh-pressure metamorphic rocks from Dabie Mountains, China".Micron 35.6(2004):441-445.
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