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461.
Carl Richter 《Geophysical Journal International》1992,110(3):451-464
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Richard J. Lisle 《Mathematical Geology》1992,24(5):455-461
Procedures are outlined for the selection of a least squares best-fit circle to data points defined by rectangular Cartesian coordinates. Equations are derived to allow fitting of circles centered on the x-axis as well as off-axis Mohr circles. These procedures are applicable to the estimation of second-order tensors such as stress and strain by means of Mohr's diagram. 相似文献
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R. J. MERRIMAN B. ROBERTS D. R. PEACOR S. R. HIRONS 《Journal of Metamorphic Geology》1995,13(5):559-576
Abstract TEM and XRD techniques were used to study crystal growth characteristics of the fabric-forming phyllosilicates which developed in response to low-grade metamorphism and tectonic imbrication in part of the Southern Uplands thrust terrane. Prograde regional metamorphism, ranging from late diagenesis through the anchizone to the epizone, was accompanied by the development of a slaty cleavage which is commonly bedding-parallel. TEM-measured mean thicknesses of white mica and chlorite crystallite populations increase with advancing grade and correlate with XRD-measured crystallinity indices. Analytical TEM data show that prograde changes in composition lead to a net loss of Si, Ca and minor Fe from the fabric-forming phyllosilicates. White micas are paragonite-poor phengites with a mean b lattice parameter of 9.037 Å, and indicate an intermediate pressure series of metamorphism with a field gradient of <25° C km-1. Chlorite compositions evolved from diabantite (with intergrown corrensite) to ripidolite over an estimated temperature range of 150–320° C. Field gradient and temperature estimates suggest that crystal growth and fabric development occurred at burial depths ranging from 6 km to at least 13 km in the thrust terrane. During late diagenesis, crystal growth of white mica and chlorite was predominantly a consequence of polytypic and phase transitions, and resulted in similar size distributions which resemble typical Ostwald ripening curves. Under anchizonal and epizonal conditions, white mica grew more rapidly than chlorite because of its greater ability to store strain energy and recover from subgrain development; as a result crystal thickness distributions are not typical of Ostwald ripening. In contrast, chlorite crystals which grew under these conditions developed subgrain boundaries at high strain rates which were only partially recovered at low strain rates; these retained dislocations reduce the crystallite thicknesses detected by TEM and XRD, compared with those of white mica. These differences in strain-induced crystal growth indicate that white mica (illite) and chlorite crystallinity indices are likely to show significant differences where low-grade metamorphism is closely associated with tectonic fabric development. 相似文献
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Yuri V. Lyubitsky 《Natural Hazards》1995,11(2):99-110
All the available historic records of sea level and appropriate weather charts have been used to study storm surges in the northern part of the Sea of Japan. The generation of surges in this area was investigated by means of a two-dimensional numerical model. Computed sea levels were compared with hourly observed residual sea levels in De-Kastri. The agreement between computed and observed storm surges is quite satisfactory. The relative importance of various meteorological parameters and bottom topography in formation of the strong storm surge on 20–21 September 1975 was studied numerically. 相似文献
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本文将银山成矿体系为富含H2S,CO2的NaCl体系,对Cu,Pb,Zn,Ag和Au等金属元素在该体系降温过程中的地球化学行为和银山矿床的成矿过程进行计算机数字模拟,并与沸腾降温体系进行对比,证明了成矿体系地球化学演化对金属元素的迁移与沉淀具有得要影响。成矿硫体地球化学模拟在矿床成因,深部成矿预测和区域成矿规律研究中具有重要意义。 相似文献
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岩石有限应变测量的莫尔圆图解网法 总被引:1,自引:1,他引:1
通常进行的应变测量需经过繁杂的数学计算或莫尔圆作图才能获得应变结果。本文介绍了笔者新设计的莫尔圆图解网及其使用方法。它可以快速准确地作出莫尔圆,进而求得应变结果,也可用于求解应力莫尔圆问题。 相似文献