高压物理学报

高温高压下黑云斜长片麻岩的电性研究

PDF下载

黄晓葛 ¹ , 白武明 ¹ , 周文戈 ²

高压物理学报 | 2008,22(3): 237-244

收起

高压物理学报 | 2008 , 22 (3) : 237 -244

高温高压下黑云斜长片麻岩的电性研究

全屏

[Author(id=1322941155998048263, tenantId=1146029695717560320, journalId=1255847867265597444, articleId=1322941153145922558, orderNo=0, firstName=null, middleName=null, lastName=null, nameCn=null, orcid=null, stid=null, country=null, authorPic=null, dead=0, email=xghuang@mail.igcas.ac.cn, emailSecond=null, emailThird=null, correspondingAuthor=0, authorType=1, ext={EN=AuthorExt(id=1322941156341981193, tenantId=1146029695717560320, journalId=1255847867265597444, articleId=1322941153145922558, authorId=1322941155998048263, language=EN, stringName=Xiao-Ge HUANG, firstName=Xiao-Ge, middleName=null, lastName=HUANG, prefix=null, suffix=null, authorComment=null, nameInitials=null, affiliation=null, department=null, xref=¹, address=^1.Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China, bio=null, bioImg=null, bioContent=null, aboutCorrespAuthor=null), CN=AuthorExt(id=1322941156404895754, tenantId=1146029695717560320, journalId=1255847867265597444, articleId=1322941153145922558, authorId=1322941155998048263, language=CN, stringName=黄晓葛, firstName=null, middleName=null, lastName=null, prefix=null, suffix=null, authorComment=null, nameInitials=null, affiliation=null, department=null, xref=¹, address=^1.中国科学院地质与地球物理研究所，北京　100029, bio={"content":"

黄晓葛（1970—），女，博士，副研究员，主要研究方向为岩石物理学. E-mail：xghuang@mail.igcas.ac.cn

"}, bioImg=null, bioContent=

黄晓葛（1970—），女，博士，副研究员，主要研究方向为岩石物理学. E-mail：xghuang@mail.igcas.ac.cn

, aboutCorrespAuthor=null)}, companyList=[AuthorCompany(id=1322941155557646336, tenantId=1146029695717560320, journalId=1255847867265597444, articleId=1322941153145922558, xref=1., ext=[AuthorCompanyExt(id=1322941155566034945, tenantId=1146029695717560320, journalId=1255847867265597444, articleId=1322941153145922558, companyId=1322941155557646336, language=EN, country=null, province=null, city=null, postcode=null, companyName=null, departmentName=null, remark=^1.Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China), AuthorCompanyExt(id=1322941155574423554, tenantId=1146029695717560320, journalId=1255847867265597444, articleId=1322941153145922558, companyId=1322941155557646336, language=CN, country=null, province=null, city=null, postcode=null, companyName=null, departmentName=null, remark=^1.中国科学院地质与地球物理研究所，北京　100029)])]), Author(id=1322941156497170444, tenantId=1146029695717560320, journalId=1255847867265597444, articleId=1322941153145922558, orderNo=1, firstName=null, middleName=null, lastName=null, nameCn=null, orcid=null, stid=null, country=null, authorPic=null, dead=0, email=null, emailSecond=null, emailThird=null, correspondingAuthor=0, authorType=1, ext={EN=AuthorExt(id=1322941156581056526, tenantId=1146029695717560320, journalId=1255847867265597444, articleId=1322941153145922558, authorId=1322941156497170444, language=EN, stringName=Wu-Ming BAI, firstName=Wu-Ming, middleName=null, lastName=BAI, prefix=null, suffix=null, authorComment=null, nameInitials=null, affiliation=null, department=null, xref=¹, address=^1.Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China, bio=null, bioImg=null, bioContent=null, aboutCorrespAuthor=null), CN=AuthorExt(id=1322941156757217295, tenantId=1146029695717560320, journalId=1255847867265597444, articleId=1322941153145922558, authorId=1322941156497170444, language=CN, stringName=白武明, firstName=null, middleName=null, lastName=null, prefix=null, suffix=null, authorComment=null, nameInitials=null, affiliation=null, department=null, xref=¹, address=^1.中国科学院地质与地球物理研究所，北京　100029, bio=null, bioImg=null, bioContent=null, aboutCorrespAuthor=null)}, companyList=[AuthorCompany(id=1322941155557646336, tenantId=1146029695717560320, journalId=1255847867265597444, articleId=1322941153145922558, xref=1., ext=[AuthorCompanyExt(id=1322941155566034945, tenantId=1146029695717560320, journalId=1255847867265597444, articleId=1322941153145922558, companyId=1322941155557646336, language=EN, country=null, province=null, city=null, postcode=null, companyName=null, departmentName=null, remark=^1.Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China), AuthorCompanyExt(id=1322941155574423554, tenantId=1146029695717560320, journalId=1255847867265597444, articleId=1322941153145922558, companyId=1322941155557646336, language=CN, country=null, province=null, city=null, postcode=null, companyName=null, departmentName=null, remark=^1.中国科学院地质与地球物理研究所，北京　100029)])]), Author(id=1322941156836909073, tenantId=1146029695717560320, journalId=1255847867265597444, articleId=1322941153145922558, orderNo=2, firstName=null, middleName=null, lastName=null, nameCn=null, orcid=null, stid=null, country=null, authorPic=null, dead=0, email=null, emailSecond=null, emailThird=null, correspondingAuthor=0, authorType=1, ext={EN=AuthorExt(id=1322941156912406547, tenantId=1146029695717560320, journalId=1255847867265597444, articleId=1322941153145922558, authorId=1322941156836909073, language=EN, stringName=Wen-Ge ZHOU, firstName=Wen-Ge, middleName=null, lastName=ZHOU, prefix=null, suffix=null, authorComment=null, nameInitials=null, affiliation=null, department=null, xref=², address=^2.Institute of Geochemitry, Chinese Academy of Sciences, Guiyang 550002, China, bio=null, bioImg=null, bioContent=null, aboutCorrespAuthor=null), CN=AuthorExt(id=1322941156983709716, tenantId=1146029695717560320, journalId=1255847867265597444, articleId=1322941153145922558, authorId=1322941156836909073, language=CN, stringName=周文戈, firstName=null, middleName=null, lastName=null, prefix=null, suffix=null, authorComment=null, nameInitials=null, affiliation=null, department=null, xref=², address=^2.中国科学院贵阳地球化学研究所，贵州贵阳　550002, bio=null, bioImg=null, bioContent=null, aboutCorrespAuthor=null)}, companyList=[AuthorCompany(id=1322941155884802051, tenantId=1146029695717560320, journalId=1255847867265597444, articleId=1322941153145922558, xref=2., ext=[AuthorCompanyExt(id=1322941155893190660, tenantId=1146029695717560320, journalId=1255847867265597444, articleId=1322941153145922558, companyId=1322941155884802051, language=EN, country=null, province=null, city=null, postcode=null, companyName=null, departmentName=null, remark=^2.Institute of Geochemitry, Chinese Academy of Sciences, Guiyang 550002, China), AuthorCompanyExt(id=1322941155905773573, tenantId=1146029695717560320, journalId=1255847867265597444, articleId=1322941153145922558, companyId=1322941155884802051, language=CN, country=null, province=null, city=null, postcode=null, companyName=null, departmentName=null, remark=^2.中国科学院贵阳地球化学研究所，贵州贵阳　550002)])])]

黄晓葛¹, 白武明¹, 周文戈²

作者信息

^1.中国科学院地质与地球物理研究所，北京　100029

^2.中国科学院贵阳地球化学研究所，贵州贵阳　550002

作者简介:

黄晓葛（1970—），女，博士，副研究员，主要研究方向为岩石物理学. E-mail：xghuang@mail.igcas.ac.cn

Experimental Study on Electrical Conductivity of Biotite- and Plagioclase-Bearing Gneiss at High Temperature and High Pressure

Xiao-Ge HUANG¹, Wu-Ming BAI¹, Wen-Ge ZHOU²

Affiliations

^1.Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China

^2.Institute of Geochemitry, Chinese Academy of Sciences, Guiyang 550002, China

出版时间: 2008-09-05

文章导航

摘要

收起

在压力1 GPa、温度250~1 100 ℃、频率0.1 Hz~1 MHz的条件下，采用阻抗谱方法，对来自阴山造山带的太古代黑云斜长片麻岩进行了电导率实验研究。实验发现：（1）所有样品的阻抗谱都是由一个大的高频半圆弧Ⅰ和一个小的被压缩了的低频弧Ⅱ组成，阻抗弧Ⅰ主要代表矿物颗粒内部传导机制，阻抗弧Ⅱ更有可能代表的是样品和电极之间的传导机制；（2）电导率随温度的变化遵循Arrhenian定律，但在700~750 ℃间有近一个量级的跳跃，通过对比实验前后样品的显微照片和探针分析数据，认为这一电导率的大幅跳跃可能是样品中黑云母发生大量脱水熔融的缘故；（3）在高温段750~1 100 ℃，部分熔融样品的电导率主要由钠离子传导控制；（4）在低温段250~700 ℃，样品的激活能为0.53 eV；在高温段750~1 100 ℃，样品的激活能为1.41 eV。激活能的改变可能与样品的结构变化有关，还与样品和熔体中钠的含量以及扩散有关。

关键词

电导率 / 黑云斜长片麻岩 / 激活能 / 阴山造山带

Abstract

收起

We have investigated the electrical properties of rock sample from Yinshan orogenic zone by in situ complex impedance spectroscopy using a multianvil apparatus. The electrical conductivity was measured at pressure of 1 GPa and temperature from 250 ℃ to 1 100 ℃ at frequencies from 0.1 Hz to 1 MHz. The data of resistance were obtained by using an equivalent circuit fitting technique. From these measurements we determined the electrical conductivity of the Archean metamorphic biotite- and plagioclase-bearing gneiss. The experimental results indicate that (1) each spectrum consists of an almost semicircular high-frequency arc Ⅰand a depressed high-frequency arc Ⅱ. The impedance spectrum Ⅰ is dominated by grain-interior response; the impedance spectrum Ⅱ is dominated by the sample-electrode interface impedance. (2) Electrical conductivity displays Arrhenian behavior respectively over investigated temperature range from 250 ℃ to 700 ℃ and from 750 ℃ to 1 100 ℃. However, it rapidly increases from 700 ℃ to 750 ℃. This jump is due to dehydration-melting of biotite within sample based on the comparative analysis of SEM photoes and electron probe data for pre-run and post-run samples. (3) Over higher temperature range (750~1 100 ℃), sodium is the dominating charge carrier in partially molten samples. (4) The activation energy of biotite- and plagioclase-bearing gneiss is 0.53 eV over range of temperature from 250 ℃ to 700 ℃. However, the activation energy of partially molten sample is 1.41 eV over range of temperature from 750 ℃ to 1 100 ℃. This change of activation energy has relations with sodium content and mobility in melt. It is possibly due to the change of structure between mineral and melt within samples.

Key words

electrical conductivity / gneiss / activation energy / Yinshan orogenic zone

引用本文

黄晓葛, 白武明, 周文戈. 高温高压下黑云斜长片麻岩的电性研究. 高压物理学报, 2008 , 22 (3) : 237 -244 .

Xiao-Ge HUANG, Wu-Ming BAI, Wen-Ge ZHOU. Experimental Study on Electrical Conductivity of Biotite- and Plagioclase-Bearing Gneiss at High Temperature and High Pressure[J]. Chinese Journal of High Pressure Physics, 2008 , 22 (3) : 237 -244 .

基金

收起

国家自然科学基金(40674047; 40544015)
中国科学院创新项目(KZCX3-SW-148)

参考文献

收起

文献

收起

参考文献引证文献

排序方式：

[1]

Gaillard F. Laboratory Measurements of Electrical Conductivity of Hydrous and Dry Silicic Melts under Pressure[J]. Earth and Planetary Science Letters, 2004, 218(1/2): 215-228.

[2]

Duba A. Electrical Conductivity of Olivine[J]. J Geophys Res, 1972, 77(14): 2483-2494.

[3]

Haak V. A Comparison of the Electrical Conductivity of Natural Mono and Polycrystalline Olivines-A Case to Decide[A]//Schreyer W. High-Pressure Researches in Geoscience[C]. Stuttgart: E Schweizerbart'sche Verlagsbuchhandlung, 1982: 407-417.

[4]

Constable S, Duba A. Electrical Conductivity of Olivine, a Dunite, and the Mantle[J]. J Geophys Res, 1990, 95(B5): 6967-6978.

[5]

Tyburczy J A, Roberts J J. Low Frequency Electrical Response of Polycrystalline Olivine Compacts: Grain Boundary Transport[J]. J Geophys Res, 1990, 17(11): 1985-1988.

[6]

Roberts J J, Tyburczy J A. Frequency Dependent Electrical Properties of Polycrystalline Olivine Compacts[J]. J Geophys Res, 1991, 96(B10): 16205-16222.

[7]

Liu J L, Bai W M, Kong X R. Research on Electrical Properties of Rock at High Pressure and Temperature[J]. Acta Seismologica Sinica, 1999, 21(1): 89-97. (in Chinese)

柳江琳, 白武明, 孔祥儒. 高温高压下岩石的电性研究[J]. 地震学报, 1999, 21(1): 89-97.

[8]

Fuji-ta K, Katsura T, Tainosho Y. Electrical Conductivity Measurement of Granulite under Mid-to Lower Crustal Pressure-Temperature Conditions[J]. Geophys J Int, 2004, 157(1): 79-86.

[9]

Sato H, Ida Y. Low Frequency Electrical Impedance of Partially Molten Gabbro: The Effect of Melt Geometry on Electrical Properties[J]. Tectonophysics, 1984, 107(1/2): 105-134.

[10]

Roberts J J, Tyburczy J A. Partial-Melt Electrical Conductivity: Influence of Melt Composition[J]. J Geophys Res, 1999, 104(B4): 7055-7065.

[11]

Partzsch G M, Schilling F R, Arndt J. The Influence of Partial Melting on the Electrical Behavior of Crustal Rocks: Laboratory Examinations, Model Calculations and Geological Interpretations[J]. Tectonophysics, 2000, 317(3-4): 189-203.

[12]

Gardien V, Thompson A B, Grujic D, et al. Experimental Melting of Biotite+Plagioclase+Quartz±Muscovite Assemblages and Implications for Crustal Melting[J]. J Geophy Res, 1995, 100(B8): 15581-15591.

[13]

Wu Z X, Deng J F, Wyllie P J, et al. Dehydration-Melting Experiment of the Biotite-Gneiss, Eastern Hebei, at 1 GPa Pressure[J]. Scientia Geologica Sinica, 1995, 30(1): 12-17. (in Chinese)

吴宗絮, 邓晋福, Wyllie P J, 等. 冀东黑云母片麻岩在1 GPa压力下脱水熔融实验[J]. 地质科学, 1995, 30(1): 12-17.

[14]

Yang X S, Jin Z M, Huenges E, et al. Experimental Study on Dehydration Melting of Natural Biotite-Plagioclasegneiss from Himalayas and Implications for Himalayan Crust Anatexis[J]. Chinese Science Bulletin, 2001, 46(10): 867-872. (in Chinese)

杨晓松, 金振民, Huenges E, 等. 高喜马拉雅黑云斜长片麻岩脱水熔融实验: 对青藏高原地壳深熔的启示[J]. 科学通报, 2001, 46(3): 246-250.

[15]

Fuji-ta K, Katsura T, Matsuzaki T, et al. Electrical Conductivity Measurement of Gneiss under Mid-to Lower Crustal p-T Conditions[J]. Tectonophysics, 2007, 434(1): 93-101.

[16]

Macdonald J R. Impedance Spectroscopy, Emphasizing Solid Materials and Systems[M]. New York: John Wiley & Sons, 1987: 1-26.

[17]

Huebner S J, Dillenaurg G D. Impedance Spectra of Dry Silicate Minerals and Rock: Qualitative Interpretation of Spectra[J]. Am Miner, 1995, 80(1-2): 46-64.

[18]

Bai L P, Du J G, Liu W, et al. The Experimental Studies on Electrical Conductivities and P-Wave Velocities of Anorthosite at High Pressure and High Temperature[J]. Acta Seismologica Sinica, 2002, 24(6): 638-646. (in Chinese)

白利平, 杜建国, 刘巍, 等. 高温高压下斜长岩纵波速度与电导率实验研究[J]. 地震学报, 2002, 24(6): 638-646.

[19]

Roberts J J, Tyburczy J A. Frequency Dependent Electrical Properties of Dunite as Function of Temperature and Oxygen Fugacity[J]. Phys Chem Minerals, 1993, 19(8): 545-561.

[20]

Skjerlie K, Johnston A D. Fluid-Absent Melting Behavior of an F-Rich Tonalitic Gneiss at Mid-crustal Pressures: Implication for the Generation of Anorogenic Granites[J]. J Petrology, 1993, 34(4): 785-815.

[21]

Patiňo Douce A E, Johnston A D. Phase Equilibria and Melt Productivity in the Politic System: Implications for the Origin of Peraluminous Granitoids and Aluminous Granulites[J]. Contrib Miner Petrol, 1991, 107(2): 202-218.

[22]

Waff H S. Theoretical Considerations of Electrical Conductivity in a Partially Molten Mantle and Implications for Geothermometry[J]. J Geophys Res, 1974, 79(26): 4003-4010.

[23]

Waff H S, Weill D F. Electrical Conductivity of Magmatic Liquids: Effects of Temperature, Oxygen Fugacity and Composition[J]. Earth Planet Sci Lett, 1975, 28(2): 254-260.

[24]

Rai C S, Manghnani M H. Electrical Conductivity of Basalts to 1 550 ℃[A]//Dick H J B. Magma Genesis[C]. Portland: Bull 96 Oregon Dept Geol Miner Ind, 1977: 219-237.

[25]

Rai C S, Manghnani M H. Electrical Conductivity of Ultramafic Rocks to 1 820 Kelvin[J]. Phys Earth Planet Inter, 1978, 17(1): 6-13.

[26]

Behrens H. Na and Ca Tracer Diffusion in Plagioclase Glasses and Supercooled Melts[J]. Chem Geol, 1992, 96(3-4): 267-275.

[27]

Henderson P, Nolan J, Cunningham G C, et al. Structural Controls and Mechanisms of Diffusion in Natural Silicate Melts[J]. Contrib Miner Petrol, 1985, 89(2/3): 263-272.

2008年第22卷第3期

PDF下载

引用本文

BibTeX

文章信息

接收时间：2007-06-09
首发时间：2026-10-30
出版时间：2008-09-05

补充材料

相关文章

文章信息

作者

出版历史

收稿日期：2007-06-09
修回日期：2007-08-29

基金

国家自然科学基金(40674047; 40544015)

中国科学院创新项目(KZCX3-SW-148)

作者信息

^1.中国科学院地质与地球物理研究所，北京　100029

^2.中国科学院贵阳地球化学研究所，贵州贵阳　550002

参考文献

分享链接

https://castjournals.cast.org.cn/joweb/gywlxb/CN/1322941153145922558

分享至

全文二维码

扫描看全文

引用本文

BibTeX

本文的引用情况

2种不同金属材料的力学参数

科 Family	属数 Number of genus	种数 Number of species	占总种数比例 Percentage of total species (%)	属 Genus	种数 Number of species	占总种数比例 Percentage of total species (%)
鹅膏菌科Amanitaceae	2	11	5.26	鹅膏菌属 Amanita	10	4.78
小菇科 Mycenaceae	2	12	5.74	丝盖伞属 Inocybe	5	2.39
多孔菌科 Polyporaceae	8	14	6.70	蜡蘑属 Laccaria	5	2.39
红菇科 Russulaceae	3	23	11.00	小皮伞属 Marasmius	6	2.87
				小菇属 Mycena	11	5.26
				光柄菇属 Pluteus	5	2.39
				红菇属 Russula	17	8.13
				栓菌属 Trametes	5	2.39

关闭全屏

BibTeX
EndNote
RefWorks
TxT