Research for the deformation field in middle to lower crust from the viewpoints of water-rock interactions.
从水-岩相互作用角度研究中下地壳变形场。
基本信息
- 批准号:14204047
- 负责人:
- 金额:$ 36.52万
- 依托单位:
- 依托单位国家:日本
- 项目类别:Grant-in-Aid for Scientific Research (A)
- 财政年份:2002
- 资助国家:日本
- 起止时间:2002 至 2004
- 项目状态:已结题
- 来源:
- 关键词:
项目摘要
1)We made experimental apparatus of a mini-piston cylinder system for state-equation of crustal fluids, and tested its capability. It is used in the pressure vessel of gas-type high T & P tri-axial apparatus. CO2 is injected out of the pressure vessel into the mini-piston cylinder system in which NaCl solution is confined, P, V and T is continuously measured. The accuracy of P and V measurements is sufficient, but the measurement of T must be improved.2)We performed stick-slip experiments using the data recording system of a high acquisition rate which was attached with the tri-axial apparatus. They elucidated that friction coefficient increased abruptly and promptly just after the melting of slip surfaces by frictional heating, and that slips were stopped temporarily or finally.3)We overhauled our old solid-pressure type tri-axial apparatus and renewed the measurement system of T and P. This enabled us to performed deformation experiments under the P and T conditions at a Moho depth. … More We succeeded also in measuring the differential stress precisely. By using this refined apparatus, we stared the deformation experiments far quartzite with an aim to investigate the effects of H2O on plastic flow and fracturing in lower crust.4)On the basis of statistical thermodynamics theory, we analyzed the temperature-, pressure-and composition-dependences of the dihedral angles of solid/liquid systems which control the distribution patterns of liquids and melts in solids. The results are consistent with the experimental data for metals, and the wetting behaviors in quartz + H2O system under the condition of the lower crust were successfully explained at least qualitatively.5)By using FLASH algorism, we made a computer code of the phase equilibrium for all of the state equations of H2O + NaCl + CO2 systems that have been proposed previously. Moreover, we calculated enthalpies by differentiating the state functions for temperature that is derived from the state equations. The accuracy of the state equations was checked based on temperature changes.6)We measured the electric impedance for sintered glass beads which was immersed in electrolyte solutions in order to understand its relation to the internal structure of the sintered glass beads. These experiments elucidated that the electric conductivity is determined by the connectivity of liquid, and that the dielectric constant is governed by the isolated liquid patches. These results enable us to establish realistic models for the distributional configuration of liquid phases in rocks. Less
1)我们将固定的气体型容器进行了实验,将二氧化碳的二氧化碳注入了小动物,将NaCl溶液限制为p,v和coninules coninuely测量。 3)我们在p和t tonditions下,在Moho深度上,我们在P和T张力下进行了过度的压力三轴设备这种精制的设备阐明了H2O对塑料流量和下层地壳中的破裂的影响。4)根据统计热力学理论,我们分析了控制分布模式的固体/液体系统二面角的温度,压力和依赖性固体中的缝制和熔体的结果与金属的实验数据一致,并且在下壳下的石英 + H2O系统中的润湿行为至少质量地浮出水面。5)此外,对于H2O + NaCl + CO2系统的所有状态方程,我们通过根据烧结的玻璃珠珠子的电力来理解其使用的锥度来计算焓的焓。烧结的玻璃珠。
项目成果
期刊论文数量(46)
专著数量(0)
科研奖励数量(0)
会议论文数量(0)
专利数量(0)
Can Newtonian viscous-matrix model be applied to the microboudinage of columnar mineral grains in quartzose metamorphic tectonites?
牛顿粘性基体模型能否应用于石英变质构造岩中柱状矿物颗粒的微观结构?
- DOI:
- 发表时间:2004
- 期刊:
- 影响因子:0
- 作者:Masuda;T.;Kimura;N.
- 通讯作者:N.
Frictional melting terminates seismic slip : Experimental results of stick-slips.
摩擦熔化终止地震滑移:粘滑实验结果。
- DOI:
- 发表时间:2004
- 期刊:
- 影响因子:0
- 作者:Koizumi;Y.;Otsuki;K.;Takeuchi;H.;Nagahama;H.
- 通讯作者:H.
Otsuki, K., Monzawa, N., Nagase, T.: "Fluidization and melting of fault gouge during seismic slip : Identification in the Nojima fault zone and implications for focal earthquake mechanisms"Jour.Geophys.Res.. 108. ESE 4-1-ESE 4-18 (2003)
Otsuki, K.、Monzawa, N.、Nagase, T.:“地震滑动过程中断层泥的流化和熔化:野岛断层带的识别及其对震源地震机制的影响”Jour.Geophys.Res.. 108. ESE 4
- DOI:
- 发表时间:
- 期刊:
- 影响因子:0
- 作者:
- 通讯作者:
Stallard, A.R., Ikei, H., Masuda, T.: "Numerical simulations of spiral-shaped inclusion trails : can 3D geometry distinguish between end-member models of spiral formation?"Journal of Metamorphic Geology. 20. 801-812 (2002)
Stallard, A.R.、Ikei, H.、Masuda, T.:“螺旋状包裹体轨迹的数值模拟:3D 几何学能否区分螺旋形成的端元模型?”变质地质学杂志。
- DOI:
- 发表时间:
- 期刊:
- 影响因子:0
- 作者:
- 通讯作者:
Microboudin structures of piemontite along the Sambagawa metamorphic belt, Japan : implications for lateral variation of differential stress....
日本三波川变质带沿线皮蒙特岩的微布丁结构:对差异应力横向变化的影响......
- DOI:
- 发表时间:2004
- 期刊:
- 影响因子:0
- 作者:Masuda;T.;Shibutani;T.;Ochiai;T.;Akagi;S.;others
- 通讯作者:others
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OTSUKI Kenshiro其他文献
OTSUKI Kenshiro的其他文献
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{{ truncateString('OTSUKI Kenshiro', 18)}}的其他基金
Basic study for prediction of large earthquakes off Miyagi Prefecture by monitoring deep groundwater fluctuations
通过监测深层地下水波动预测宫城县近海大地震的基础研究
- 批准号:
18204046 - 财政年份:2006
- 资助金额:
$ 36.52万 - 项目类别:
Grant-in-Aid for Scientific Research (A)
Understanding the physical processes of frictional slip of subduction zone earthquakes from the characteristics of fault rocks.
从断层岩特征认识俯冲带地震摩擦滑移物理过程
- 批准号:
12440132 - 财政年份:2000
- 资助金额:
$ 36.52万 - 项目类别:
Grant-in-Aid for Scientific Research (B)
Study on the Extension Tectonics of Northeast Honshu Arc Just Before 15 Ma.
本州岛东北弧15 Ma之前的伸展构造研究。
- 批准号:
01540622 - 财政年份:1989
- 资助金额:
$ 36.52万 - 项目类别:
Grant-in-Aid for General Scientific Research (C)