高压物理学报

石英岩脆塑性转化的实验研究

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宋娟 ¹ , 周永胜 ² , 何昌荣 ²

高压物理学报 | 2008,22(2): 167-174

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高压物理学报 | 2008 , 22 (2) : 167 -174

石英岩脆塑性转化的实验研究

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宋娟¹, 周永胜², 何昌荣²

作者信息

^1.中国石油大学（华东），山东东营　257061

^2.中国地震局地质研究所地震动力学国家重点实验室，北京　100029

通讯作者:

周永胜（1969—），男，博士，研究员，主要从事高温高压岩石物理和岩石力学实验研究. E-mail：zhouysh@ies.ac.cn

作者简介:

宋娟（1975—），女，硕士，讲师，主要从事高温高压岩石力学实验和地震学研究. E-mail：songjuan95@126.com

The Brittle-Plastic Transition in Experimentally Deformated Quartzite

Juan SONG¹, Yong-Sheng ZHOU², Chang-Rong HE²

Affiliations

^1.China University of Petroleum, Dongying 257061, China

^2.State Key Laboratory of Earthquake Dynamics, Institute of Geology, China Earthquake Administration, Beijing 100029, China

出版时间: 2008-06-05

文章导航

摘要

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在温度500~1 000 ℃、围压1 251~1 440 MPa条件下进行了石英岩脆塑性转化的实验研究。通过力学行为和变形微观结构研究表明，在实验温度和压力范围内，石英岩经历了半脆性破裂、半脆性流动和塑性变形3种变形阶段。随着温度升高，石英岩在变形机制上发生了两次转化，从半脆性破裂向半脆性流动转化发生在700~800 ℃，从半脆性流动向塑性变形转化发生在900~950 ℃，这两个变形阶段的转化温度比Hirth（1994）给出的各阶段转化温度高100 ℃。在塑性变形域的大应变实验样品中发现了柯石英。

关键词

石英岩 / 高温高压 / 脆塑性转化

Abstract

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Deformation experiments have been conducted to investigate the brittle-plastic transition of quartzite under temperature of 500~1 000 ℃ and confining pressure of 1 251~1 440 MPa. Mechanical behavior and microstructural characteristics indicated that the brittle-plastic transition of quartzite in experimental condition underwent three deformation mechanisms, namely the semibrittle faulting, semibrittle flow and plastic flow. At least two transitions of deformation mechanism were involved with increasing temperature. The first is the transition from semibrittle faulting to semibrittle flow at 700~800 ℃, and the second is the transition from semibrittle flow to plastic flow at 900~950 ℃. In comparison with the similar results reported by Hirth and Tullis (1994), the temperatures of two transitions we determined is higher by 100 ℃ than Hirth and Tullis’ results. In addition, coesite was found in the thin section of severely deformed plastic flow samples.

Key words

quartzite / high temperature and high pressure / brittle-plastic transition

引用本文

宋娟, 周永胜, 何昌荣. 石英岩脆塑性转化的实验研究. 高压物理学报, 2008 , 22 (2) : 167 -174 .

Juan SONG, Yong-Sheng ZHOU, Chang-Rong HE. The Brittle-Plastic Transition in Experimentally Deformated Quartzite[J]. Chinese Journal of High Pressure Physics, 2008 , 22 (2) : 167 -174 .

基金

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国家自然科学基金(40474067; 40002020)

参考文献

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参考文献引证文献

排序方式：

[1]

Brace W F, Kohlstedt D L. Limits on Lithospheric Stress Iimposed by Labroratory Experiments[J]. J Geophys Res, 1980, 85: 6248-6252.

[2]

Kohlstedt D L, Evans B, Mackwell S J. Strength of the Lithosphere: Constraints Imposed by Laboratory Experiments[J]. J Geophys Res, 1995, 100: 17587-17602.

[3]

Jackson J. Strength of the Continental Lithosphere: Time to Abandon the Jelly Sandwich?[J]. GSA Today, 2002: 4-9.

[4]

Sibson R H. Fault Zone Models, Heat Flow, and Thedepth Distribution of Earthquakes in the Continental Crust of the United States[J]. Bull Seismol Soc Am, 1982, 72: 151-163.

[5]

Chen I-W, Molnar P. Focal Depths of Intracontinental and Intraplate Earthquakes and Their Implications for theThermal and Mechanical Properties of Lithosphere[J]. J Geophys Res, 1983, 88: 4183-4214.

[6]

Zhou Y S, He C R. The Relationship between Low Velocity Layers and Rheology of the Crust in North China and Its Effect on Strong Earthquake[J]. Seismology and Geology, 2002, 24(1): 124-132. (in Chinese).

周永胜, 何昌荣. 华北地区壳内低速层与地壳流变的关系及其对强震孕育的影响[J]. 地震地质, 2002, 24(1): 124-132.

[7]

Zhou Y S, He C R. Rheological Parameters of Orustal Rocks and Crustal Rheology of North China[J]. Seismology and Geology, 2003, 25(1): 109-122. (in Chinese)

周永胜, 何昌荣. 地壳主要岩石流变参数及华北地壳流变性质研究[J]. 地震地质, 2003, 25(1): 109-122.

[8]

Tse S T, Rice J R. Crustal EarthquakeInstability in Relation to the Depth Variation of Frictional Slip Properties[J]. J Geophys Res, 1986, 91: 9452-9472.

[9]

He C R, Ma S L, Huang J G. Influence of Loading Rate Variation on the Stability of Fault Motion[J]. Seismology and Geology, 1998, 20(1): 54-62. (in Chinese)

何昌荣, 马胜利, 黄建国. 断层滑动速率变化对滑动稳定性的影响[J]. 地震地质, 1998, 20(1): 54-62.

[10]

He C R. Numerical Simulation of Earthquake Nucleation Process and Seismic Precursors on Faults[J]. Earthquake Research in China, 2000, 14(3), 199-212.

[11]

He C R. Interaction between Two Sliders in a System with Rate- and State-Dependent Friction[J]. Science in China (Series D), 2003, 46(Supp): 67-74.

[12]

He C R, Ma S, Huang J. Transition between Stable Sliding and Stick-Slip due to Variation in Slip Rate under Variable Normal Stress Condition[J]. Geophys Res Lett, 1998, 25: 3235-3238.

[13]

He C R, Wong T-F, Beeler N M. Scaling of Stress Drop with Recurrence Interval and Loading Velocity for Laboratory-Derived Fault Strength Relations[J]. J Geophys, Res, 2003, 108(B1): 2037.

[14]

Gu Y, Wong T-F. Effects of Loading Velocity, Stiffness, and Inertia on the Dynamics of a Single Degree of Freedom Spring-Slider System[J]. J Geophys Res, 1991, 96: 21677-21691.

[15]

Boatwright J, Cocco M. Frictional Constraints on Crustal Faulting[J]. J Geophys Res, 1996, 101: 13895-13909.

[16]

Zhou Y S, He C R. Temporal Evolution of Focal Depths of Aftershock Sequence Following Lijiang ms7.1 Earthquake and the Implication for Rheological Property of the Middle Crust[A]//The 3st International Conference on Continental Earthquakes[C]. Beijing, 2004: 128.

[17]

Scholz C H. The Brittle-Plastic Transition and Depth of Seismic Faulting[J]. Geol Rund, 1988, 77: 319-328.

[18]

Hirth G, Tullis J. The Brittle-Plastic Transition in Experimentally Deformation Quartz Aggregates[J]. J Geophys Res, 1994, 99: 11737-11747.

[19]

Tullis J, Yund R A. Transition from Cataclastic Flow to Dislocation Creep of Feldspar: Mechanisms and Microstructures[J]. Geology, 1987, 15: 606-609.

[20]

Tullis J, Yund R A. The Brittle-Ductile Ttransition in Feldspar Aggregates: An Experimental Study[A]//Fault Mechanics and Transport Properties of Rocks[C]. Academic San Diego, Calif, 1992: 89-117.

[21]

Zhou Y S, Jiang H K, He C R. Experiments of Brittle-Plastic Transition, Modes of Instability of Juyongguan Granite Different T-P Conditions[J]. Earthquake Research in China, 2003, 17(2): 169-182

[22]

Carter N L, Tsenn M C. Flow Properties of Continental Lithosphere[J]. Tectonophysics, 1987, 136: 27-63.

[23]

Gleason G C, Tullis J. A Flow Law for Dislocation Creep of Quartz Aggregates Determined with the Molten Salt Cell[J]. Tectonophysics, 1995, 247: 1-23.

[24]

Zhou Y S, He C R. The Status of Continental Lithosphere Rheology and Experiments on Creep of Rocks at High Temperature and High Pressure[J]. Progress in Geophysical, 2004, 19(2): 246-254. (in Chinese)

周永胜, 何昌荣. 大陆岩石圈流变研究进展与高温高压流变实验现状[J]. 地球物理学进展, 2004, 19(2): 246-254.

[25]

Stipp M, Stunitz H. The Eastern Tonale Fault Zone: A “Natural Laboratory” for Crystal Plastic Deformation of Quartz over a Temperature Range from 250 to 700 ℃[J]. J Struct Geol, 2002, 24: 1861-1884.

[26]

He C R, Zhou Y S, Sang Z N. An Experimental Study on Semi-Brittle and Plastic Rheology of Panzhihua Gabbro[J]. Science in China, Series D, 2003. 46(7): 730-742.

[27]

Zhou Y S, He C R, Song J, et al. An Experiment Study Quartz-Coesite Transition at Differential Stress[J]. Chinese Science Bulletin, 2005, 50(5): 446-451.

[28]

Zhu A L, Xu X W, Zhou Y S, et al. Relocation of Small Earthquakes in Western Sichuan, China and Its Implications for Active Tectonics[J]. Chinese Journal of Geophysis, 2005, 48(3): 692-700.

2008年第22卷第2期

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接收时间：2007-03-20
首发时间：2026-11-01
出版时间：2008-06-05

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收稿日期：2007-03-20
修回日期：2007-08-06

基金

国家自然科学基金(40474067; 40002020)

作者信息

^1.中国石油大学（华东），山东东营　257061

^2.中国地震局地质研究所地震动力学国家重点实验室，北京　100029

通讯作者:

周永胜（1969—），男，博士，研究员，主要从事高温高压岩石物理和岩石力学实验研究. E-mail：zhouysh@ies.ac.cn

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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

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