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501.
502.
通过对大井铜-锡多金属矿床成矿地质环境、矿床地质特征以及对岩(矿)石同位素、稀土元素、成矿温度等地球化学和成矿物理化学环境的研究,认为,大井铜-锡多金属矿床为一典型的岩浆热液充填型矿床。与成矿有关的隐伏岩体受深部隐伏的深大断裂控制,可能与黄岗梁矽卡型铁-锡矿床同属一构造岩浆成矿带上不同成矿环境下形成的矿床。并认为,在该成矿带上及大井矿区深部仍有较大的找矿潜力。 相似文献
503.
504.
Digital Image Based Approach for Three-Dimensional Mechanical Analysis of Heterogeneous Rocks 总被引:2,自引:0,他引:2
Summary This paper presents a digital image based approach for three-dimensional (3-D) numerical simulation and failure analysis of
rocks by taking into account the actual 3-D heterogeneity. Digital image techniques are adopted to extract two-dimensional
(2-D) material heterogeneity from material surface images. The 2-D image mesostructures are further extrapolated to 3-D cuboid
mesostructures by assuming the material surface as a representation of the inner material heterogeneity within a very small
depth. The iterative milling and scanning system is set up to generate the 3-D rock mesostructures. A Hong Kong granite specimen
is used as an example to demonstrate the procedure of 3-D mesostructure establishment. The mechanical responses and failure
process under the conventional Brazilian tensile test condition are examined through numerical analyses. The stress distribution,
crack propagation process and failure model of heterogeneous material cases are simulated with a finite difference software.
The numerical results indicate that material heterogeneity plays an important role in determining the failure behavior of
rocks under external loading. 相似文献
505.
506.
A model is suggested to simulate the physical aspect of diagenesis in porous rocks. A bidisperse ballistic deposition model with relaxation of deposited grains is used to generate the porous structure. Sedimentation and erosion are allowed to restructure the pore space as a fluid flows through the rock. The effect of this restructuring of the pore space on permeability is studied. The Navier–Stokes equation is solved numerically by the finite difference method to determine the pressure and velocity distributions in the pore space. We find that though deposition is the dominant process in our model of diagenesis, reducing the porosity, the permeability may increase dramatically in some cases. These are when the erosion takes place at a single narrow constriction in the pore channel. 相似文献
507.
508.
Guo Qiliang 《中国地震研究》2007,21(3):345-354
The hydrofracturing technique has developed into a reliable and practical method for determining the original three-dimensional crustal stress state of underground caverns,the load-bearing capacity of a high pressure cavern itself,and the high pressure hydraulic permeability of rock masses,and has also been extensively used in disposal of nuclear waste,long and deeply-buried traffic channels and high-pressure cavern engineering for hydraulic power plants.The practice shows that the comprehensive measurement of the physical parameters of the rock mass and taking full use of the wall rock load-bearing capacity to optimize the engineering design hold are very useful in ensuring the engineering safety and improving the design level. 相似文献
509.
Séverine Bernardie Jean-Pascal Gilbert François Lebert Hubert Fabriol 《Pure and Applied Geophysics》2007,164(1):177-197
The monitoring of the stability of old mines constitutes an important research objective for our institution, BRGM. The study
reported here shows the contribution of high-frequency (>30 kHz) acoustic emissions to the detection of the damage within
a rock mass, during an experiment within a pilot site of an old flooded iron mine. The experiment consisted of recording all
the hydroacoustic events in a broad frequency band (between 30 Hz and 180 kHz), during 18 months. The monitoring network has
been calibrated by a triggered block fall that made it possible to highlight a relationship between the occurrence of high-frequency/low-frequency
hydroacoustic emissions and rock falls. The events recorded have been associated with the micro-failure of the rock mass near
the roof, prior to the detachment of the blocks. This monitoring showed important high-frequency hydroacoustic activity, which
may be associated with mechanical instabilities generated by the evolution of water pressure during the experiment. In conclusion,
the high-frequency hydroacoustic activity appears to be a good indicator of instability and, therefore, this new technique
constitutes a promising tool for monitoring abandoned underground cavities. 相似文献
510.
J. Morales A. Goguitchaichvili J. Urrutia-Fucugauchi 《Studia Geophysica et Geodaetica》2007,51(2):315-326
Cooling rate (CR) effects on the intensity of thermoremanent magnetization has been documented for archaeomagnetic materials,
where cooling in laboratory conditions is generally much faster compared to natural cooling rates. Since the latter condition
also applies to many volcanic rocks, we have investigated in this study the influences of the CR on the determination of absolute
paleointensity using recent basaltic rocks. We used magnetically and thermally stable samples mainly containing Ti-poor pseudo-singledomain
titanomagnetites (the most widely used material for Thellier paleointensity experiments). These samples previously succeed
in retrieving the strength of laboratory field intensities with the Coe’s version of the Thellier method in a simulated paleointensity
experiment using similar cooling rates. Our experimental results indicate that the cooling rate effects produce systematic
and significant overestimates of the absolute intensity up to 70%. The effect can be much larger than predicted by Neél theory
for non-interacting single-domain grains. 相似文献