Rupture geometry from high-precision relative hypocentre locations of microearthquake clusters   总被引：2，自引：0，他引：2  

Nicholas Deichmann  Mariano Garcia-Fernandez 《Geophysical Journal International》1992,110(3):501-517

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The influence of microform bed roughness elements on flow and sediment transport in gravel bed rivers: Comment on a paper by marwan A. Hassan and ian reid     

Nicholas J. Clifford  Keith S. Richards  Andre Robert 《地球表面变化过程与地形》1992,17(5):529-534

Data from Turkey Brook are used to demonstrate that the interaction between gravel bedforms, flow resistance and bedload transport is a dynamic one, both between and within hydrographs. and that creation of a significant component of form drag through construction of microforms (pebble clusters) may precede the eventual break-up of the bed in a transport event. This process of drag augmentation', which can be seen as a feedback mechanism delaying transport and can be likened to dilation of a soil tested in a direct shear apparatus, itself appears to be dependent on the characteristics of turbulence, and therefore involves feedback at a finer resolution than envisaged by Hassan and Reid (1990).  相似文献   

Internal control of fluid compositions in amphibolite-facies scapolitic calc-silicates,Mary Kathleen,Australia     

Nicholas H. S. Oliver  Victor J. Wall  Ian Cartwright 《Contributions to Mineralogy and Petrology》1992,111(1):94-112

Unaltered metasediments of the Mary Kathleen Fold Belt are composed predominantly of layered amphibolite-facies scapolitic calc-silicate rocks in which minimal infiltration of externally derived fluids occurred during regional metamorphism. There were substantial differences in volatile activities between different layers in the layered sequences, in particular: a _CO2/a _{H 2 O} inferred from reaction progress estimates and analysis of biotite-clinopyroxene-fluid phase relations; a _NaCl/a _{H 2 O} inferred from scapolite compositions; and a _HCl/a _{H 2 O} inferred from biotite compositions. In one outcrop in which a clinopyroxene-producing reaction dominated, differences in approximate X _{CO 2}of up to 0.25 occurred between several samples collected over 50 metres. Variations in a _{H 2 O}/a _HCl of up to one order of magnitude are inferred at 1 to 50 m scales from biotite-Cl contents, and variations in NaCl contents of scapolite from 0.0 to up to 0.6 Cl atoms in the Cl–CO₃–SO₄ site reflect a large variation of a _NaCl in the coexisting fluid at similar scales. Most calcsilicate layers internally buffered fluid compositions in the H₂O–CO₂–NaCl–HCl system. Local occurrences of NaCl-rich scapolite suggest that some layers may have been in equilibrium with halite during early prograde metamorphism. At peak metamorphic temperatures, disolution of halite was complete but layers containing high-NaCl scapolite continued to buffer fluid at high values of a _NaCl. Fluid immiscibility does not appear to have affected the progress of the devolatilization reactions. Although fluid was predominantly internally buffered, moderate quantities of fluid were released by prograde mineral reactions in many layers, up to 30 cm³ fluid per 100 cm³ rock. Numerous episodes of fluid escape were required, probably via microfractures, such that the released fluid did not obviously influence reaction progress in the layers through which it passed. The anomaly of beautifully preserved internal buffering signatures and the requirement for produced fluid locally to pass across layers in a deforming rock sequence suggest that the escaping fluid did not leave any readily observable tracks. This is explained by rapid rates of fracture propogation and fluid migration therein. This internally buffered system contrasts strongly with adjacent calc-silicate rocks that show evidence for infiltration of externally derived fluids at high fluid/rock ratios, and highlights the broad range of fluid behaviour that can be expected in deforming, heterogeneous rock sequences.  相似文献   

Seismic displacements on shear surfaces in cohesive soils     

Theodora E. Tika-Vassilikos  Sarada K. Sarma  Nicholas N. Ambraseys 《地震工程与结构动力学》1993,22(8):709-721

The paper is concerned with the earthquake-induced displacements on pre-existing shear surfaces in cohesive soils. Results from ring shear tests have shown that during fast shearing the strength of such surfaces depends on displacement and rate of shearing. The test results have been used in a numerical analysis to assess the displacement of a rigid block sliding on a plane surface. The results from the analysis show that the earthquake-induced displacements on pre-existing shear surfaces are influenced significantly by the soil behaviour under earthquake loading conditions. The results are consistent with the field performance of pre-existing slides in cohesive soils during earthquakes.  相似文献   

The dynamics and environmental context of aeolian sedimentary systems. Edited by K. Pye,Geological Society of London,Special Publication No. 72, 1993. No. of pages: viii + 336. ISBN 0-903317-885     

Nicholas Lancaster 《地球表面变化过程与地形》1994,19(4):387-387

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The role and disposition of military forces in the Russian Federation     

Nicholas F. Bradshaw 《GeoJournal》1994,34(2):155-166

The article discusses Russian motivation in the context of the restructuring of the military industrial complex and the new political districts of the former Soviet Union. It draws on Allison (1993) to describe the new military district structure, and considers what the combination of the boundaries of these areas indicates of Russian intentions for the future development of their forces and their relationship with the West. It goes on to consider the role of the media and of western political leaders in achieving images suitable for the identification of a peace dividend, and the repercussions of the situation as regards the future security of bi-polar relationships.  相似文献   

Summary statistics in geochemistry: A study of the performance of robust estimates     

Nicholas M. S. Rock 《Mathematical Geology》1988,20(3):243-275

Numerical data summaries in many geochemical papers rely on arithmetic means, with or without standard deviations. Yet the mean is the worst average (estimate of location) for those extremely common geochemical data sets which are non-normally distributed or include outliers. The widely used geometric mean, although allowing for skewed distributions, is equally susceptible to outliers. The superior performance of 19 robust estimates of location (simple median, plus various combined, adaptive, trimmed, and skipped,L, M, andW estimates) is illustrated using real geochemical data sets varying in sources of error (pure analytical error to multicomponent geological variability), modality (unimodal to polymodal), size (20 to >2000 data values), and continuity (continuous to truncated in either or both tails). The arithmetic mean tends to overestimate location of many geochemical data sets because of positive skew and large outliers; robust estimates yield consistent smaller averages, although some (e.g., Hampel's and Andrew's) do perform better than others (e.g., Shorth mean, dominant cluster mode). Recommended values for international standard rocks, and for such important geochemical concepts as average chondrite, can be reproduced far more simply via robust estimation on complete interlaboratory data sets than via the rather complicated and subjective methods (e.g., laboratory ratings) so far used in the literature. Robust estimates also seem generally less affected by truncation than the mean; for example, if values below machine detection limits are alternatively treated as missing values or as real values of zero, similar averages are obtained. The standard (and mean) deviations yield consistently larger values of scale for many geochemical data sets than the hinge width (interquartile range) or median absolute deviation from the median. Therefore, summaries of geochemical data should always include at least the simple median and hinge width, to complement the often misleading mean and standard deviation.  相似文献   

Effect of Horizontal Resolution on the Representation of the Global Monsoon Annual Cycle in AGCMs     

Lixia ZHANG  Tianjun ZHOU  Nicholas P.KLINGAMAN  Peili WU  Malcolm ROBERTS 《大气科学进展》2018,35(8):1003-1020

The sensitivity of the representation of the global monsoon annual cycle to horizontal resolution is compared in three AGCMs:the Met Office Unified Model-Global Atmosphere 3.0;the Meteorological Research Institute AGCM3;and the Global High Resolution AGCM from the Geophysical Fluid Dynamics Laboratory.For each model,we use two horizontal resolution configurations for the period 1998–2008.Increasing resolution consistently improves simulated precipitation and low-level circulation of the annual mean and the first two annual cycle modes,as measured by the pattern correlation coefficient and equitable threat score.Improvements in simulating the summer monsoon onset and withdrawal are region-dependent.No consistent response to resolution is found in simulating summer monsoon retreat.Regionally,increased resolution reduces the positive bias in simulated annual mean precipitation,the two annual-cycle modes over the West African monsoon and Northwestern Pacific monsoon.An overestimation of the solstitial mode and an underestimation of the equinoctial asymmetric mode of the East Asian monsoon are reduced in all high-resolution configurations.Systematic errors exist in lower-resolution models for simulating the onset and withdrawal of the summer monsoon.Higher resolution models consistently improve the early summer monsoon onset over East Asia and West Africa,but substantial differences exist in the responses over the Indian monsoon region,where biases differ across the three low-resolution AGCMs.This study demonstrates the importance of a multi-model comparison when examining the added value of resolution and the importance of model physical parameterizations for simulation of the Indian monsoon.  相似文献   

On Northern Hemisphere Wave Patterns Associated with Winter Rainfall Events in China     

Claudia Christine STEPHAN  Yan Ho NG  Nicholas P.KLINGAMAN 《大气科学进展》2018,35(8):1021-1034

During extended winter(November–April),43% of the intraseasonal rainfall variability in China is explained by three spatial patterns of temporally coherent rainfall.These patterns were identified with empirical orthogonal teleconnection(EOT) analysis of observed 1982–2007 pentad rainfall anomalies and connected to midlatitude disturbances.However,examination of individual strong EOT events shows that there is substantial inter-event variability in their dynamical evolution,which implies that precursor patterns found in regressions cannot serve as useful predictors.To understand the physical nature and origins of the extratropical precursors,the EOT technique is applied to six simulations of the Met Office Unified Model at horizontal resolutions of 200–40 km,with and without air–sea coupling.All simulations reproduce the observed precursor patterns in regressions,indicating robust underlying dynamical processes.Further investigation into the dynamics associated with observed patterns shows that Rossby wave dynamics can explain the large inter-event variability.The results suggest that the apparently slowly evolving or quasi-stationary waves in regression analysis are a statistical amalgamation of more rapidly propagating waves with a variety of origins and properties.  相似文献   

Calculating on a round planet     

Nicholas R. Chrisman 《International journal of geographical information science》2017,31(4):637-657

Despite incontrovertible scientific evidence to support a round Earth, GIS software implementation typically models the Earth with flat map projections. This choice has consequences that vary from mild to severe. This paper explores solutions that range from moderate measures to correct for map projection errors to radical revisions of standard practice that place all calculations on the ellipsoid. On examination, the best practice requires a distinct projection choice for each geometric operation. Multiple reasons, from the technical to ethical, justify revised practices and increased vigilance for the errors induced by inappropriate projections.  相似文献