共查询到20条相似文献，搜索用时 421 毫秒
1.
D. D. Picklyk 《Mathematical Geology》1977,9(3):301-308
General principles in evaluation and selection of data to be included in computer processible files intended for use in assisting regional resources appraisal are discussed against the background of activities related to file assembly at the Geological Survey of Canada. Some of the principles discussed are currently being implemented in the assembly of files at the GSC where they apply to the specific data being collected. Others are apparent from our analysis and would be applied if different data were being collected. The files currently being assembled at the Survey are intended to assist the commodity geologists in all project-related activities, one of which is regional resource appraisal. Prior to the commencement of data assembly, each data item considered for inclusion in the data files was scrutinized by members of the Economic Geology Subdivision in order to establish how it would contribute to the overall objectives of the file. At the same time strict definitions of each item were established. The main criteria applied to each data item considered for inclusion in the files were (a) the necessity of the item to satisfy the objectives of the file within the practical limitations of the resources available and (b) the general availability of the item. The characteristics found necessary to ensure integrity of the data files were (a) uniformity—the same definitions must apply to each item of similar type, (b) consistency—analytical results should be of the same method or differences noted in order that the data may be compared, and (c) mutual exclusiveness—especially when dealing with data referring to size. Such data should never be repeated in another part of the file or be included as part of another item.This paper was presented at the International Geological Correlation Program (IGCP) Project 98 entitled Standards for Computer Applications in Resource Studies held at Loen, Norway, September 27–October 1, 1976. 相似文献
2.
David L. Jupp 《Mathematical Geology》1976,8(3):243-266
Sequence convolution formulae, based on the B-splines of I. J. Schoenberg provide simple and effective methods for smoothing and differentiating data sequences. Their time and frequency domain properties allow calculation of the degree of smoothing and noise rejection, and their z-transforms lead to the rapid calculation of formulae from a simple sequence of polynomials. As an example of their use, numerical differentiation is used to produce smooth velocity—depth profiles and to delineate major velocity discontinuities from time—depth data logged at a well. 相似文献
3.
Neil Alderman 《Geoforum》1996,27(4):461-477
The role of innovation in influencing business performance and survival is widely accepted, but there is only limited evidence identifying any direct relationships between them. This paper uses data from a cohort study of mature British mechanical engineering establishments to investigate locational, technological and other characteristics of establishments surviving during two time periods: 1981–1986 and 1987–1992. The study is concerned with all causes of non-survival, whether attributable to business failure or to corporate decision-making. The analysis makes use of a mix of bivariate and multivariate techniques to assess influences on the survival or non-survival of the establishments. The results support previous research concerning the role of such factors as establishment size and industry sector, but contradict conventional wisdom concerning such factors as age, suggesting in particular that the relationship between age and survival applies to new start-ups, but not to mature establishments. Some evidence for locational variation in closure rates, particularly during the most recent recession, is presented. The role of technological innovation is found to be equivocal. The effects of process innovation appear to be limited, but there are suggestions that investment in research and development and design-related technologies have been related to the survival prospects of the establishments in the cohort in recent years. Some of the shortcomings of the measures of innovation available and the approach adopted are discussed. 相似文献
4.
A regionalized composition is a random vector function whose components are positive and sum to a constant at every point of the sampling region. Consequently, the components of a regionalized composition are necessarily spatially correlated. This spatial dependence—induced by the constant sum constraint—is a spurious spatial correlation and may lead to misinterpretations of statistical analyses. Furthermore, the cross-covariance matrices of the regionalized composition are singular, as is the coefficient matrix of the cokriging system of equations. Three methods of performing estimation or prediction of a regionalized composition at unsampled points are discussed: (1) the direct approach of estimating each variable separately; (2) the basis method, which is applicable only when a random function is available that can he regarded as the size of the regionalized composition under study; (3) the logratio approach, using the additive-log-ratio transformation proposed by J. Aitchison, which allows statistical analysis of compositional data. We present a brief theoretical review of these three methods and compare them using compositional data from the Lyons West Oil Field in Kansas (USA). It is shown that, although there are no important numerical differences, the direct approach leads to invalid results, whereas the basis method and the additive-log-ratio approach are comparable. 相似文献
5.
An inverse method is developed to determine the optimal stress inversion from imperfect fault data. It is specifically designed to process fault data at variable division—either with observed slip directions or with observed fault/slip senses or with both. The method has the flexibility of processing data with a few fault/slip senses incorrectly determined—a case we occasionally meet in the field. A vast number of artificial 10-datum examples are processed to illustrate the reliability of the method and to examine the effects of the data set at variable division on stress estimation. The results show that the precision of solution decreases with the increase in either of two factors, the percentage of the data limited to slip sense and the range of measurement error, both resulting in a broader dispersion of estimated stress vectors relative to the assigned stress vector in the sigma space. Thus, in order to keep the dispersion within a range of 5° requires the percentage of data for which only slip sense is known to be less than about 20%. This in turn allows for a measurement error range in the data of 10° in real space, much larger than real measurement errors. We believe that the proposed method would be of practical value for stress inversion of fault/slip data. 相似文献
6.
Yukio Sadahiro 《GeoJournal》2000,52(3):237-252
The present paper proposes a new method for analyzing the spatial structure of retailing, using microscale locational data
of individual retail stores. The method is based on the probability density function (PDF) of stores estimated from their
locational data, and consequently it is applicable to both micro- and macro-scale retail analyses. The PDF approach provides
a set of quantitative methods that permit us (1) to measure the degree of agglomeration, (2) to classify spatial patterns
of store location, (3) to analyze the relationship between the size and function of retail agglomerations, and (4) to analyze
the spatial structure of retail agglomeration. An empirical study is performed to test the validity of the method, and some
empirical findings are shown.
This revised version was published online in July 2006 with corrections to the Cover Date. 相似文献
7.
R.A. Facer 《Tectonophysics》1981,74(3-4)
A section 300 m thick across the Permian—Triassic boundary has been sampled in the Southern Coalfield of the Sydney Basin, New South Wales. 55 samples, mainly grey to drab sandstones, were collected from 9 diamond drill holes which penetrated the entire Narrabeen Group and the upper part of the conformably underlying Illawarra Coal Measures, as well as a sill emplaced into the coal measures. The samples included fully oriented cores. Additional reconnaissance samples from two further drill holes were also studied.Partial alternating field demagnetization and petrography indicate the magnetic remanence to be a stable DRM. Partial thermal demagnetization above 300°C or 400°C caused large increases in magnetic susceptibility. Partial chemical demagnetization did not cause significant changes in remanence directions.For the Coal Cliff Sandstone (basal Narrabeen Group, Triassic) the palaeomagnetic pole position (Normal) was calculated to be at 59°N 322°E (dp = 27°, dm = 29°), which agrees with previously published data. For the uppermost coal measures (Permian) the pole position was calculated as 58°N 340°E (dp = 09°, dm = 10°). Data for samples from the lower to middle coal measures yield a pole position which is between the new Permian—Triassic pole position and that for the underlying Middle Permian igneous rocks. The top of the Reversed “Kiaman Magnetic Interval” (Permian) may be near the Tongarra coal and Appin Formation boundary — (early) Late Permian. 相似文献
8.
Peter Jones 《Geoforum》1982,13(1):39-43
M.F.I. has emerged as the major retailer of self-assembly furniture in the United Kingdom and their trading philosophy has led to a search for suburban retail sites. This paper outlines M.F.I.'s locational policies and traces the company's geographical expansion. 相似文献
9.
10.
John C. Butler 《Mathematical Geology》1976,8(1):25-36
The application of R-mode principal components analysis to a set of closed chemical data is described using previously published chemical analyses of rocks from Gough Island. Different measures of similarity have been used and the results compared by calculating the correlation coefficients between each of the elements of the extracted eigenvectors and each of the original variables. These correlations provide a convenient measure of the contribution of each variable to each of the principal components. The choice of similarity measure (variance-covariance or correlation coefficient)should reflect the nature of the data and the view of the investigator as to which is the proper weighting of the variables—according to their sample variance or equally. If the data are appropriate for principal components analysis, then the Chayes and Kruskal concept of the hypothetical open and closed arrays and the expected closure correlations would seem to be useful in defining the structure to be expected in the absence of significant departures from randomness. If the data are not multivariate normally distributed, then it is possible that the principal components will not be independent. This may result in significant nonzero covariances between various pairs of principal components. 相似文献
11.
The engineering properties of solid waste produced by the combustion of Western oil shale are evaluated and discussed. Index properties and their variability, moisture—density relationships, shear strength, stress—strain characteristics, and hydraulic conductivity were evaluated in laboratory tests. Cementation caused by the formation of hydrous cements when combusted oil shale is exposed to water was found to be the most significant factor affecting its engineering properties. With increasing initial water content, shear strength increases and hydraulic conductivity decreases significantly, primarily because of cementation. Implications for the design of waste disposal embankments are discussed. 相似文献
12.
G. Boschian 《International Journal of Earth Sciences》1993,82(2):227-233
The relationships between the land and sea in the northern Adriatic at the Pleistocene—Holocene boundary are examined by considering sea-level curves and archaeological data. Changes in the Mesolithic (Early Holocene) economy of the inhabitants can be interpreted as a result of palaeoecological variations due to glacioecustatic sea-level changes and recent tectonics. This hypothesis is also supported by evidence of older tectonic movements which may have continued until the end of the Pleistocene. 相似文献
13.
A. Deutsch R. A. F. Grieve M. Avermann L. Bischoff P. Brockmeyer D. Buhl R. Lakomy V. Müller-Mohr M. Ostermann D. Stöffler 《International Journal of Earth Sciences》1995,84(4):697-709
The occurrence of shock metamorphic features substantiates an impact origin for the 1.85 Ga old Sudbury Structure, but this has not been universally accepted. Recent improvements in knowledge of large-scale impact processes, combined with new petrographic, geochemical, geophysical (LITHOPROBE) and structural data, allow the Sudbury Structure to be interpreted as a multi-ring impact structure. The structure consists of the following lithologies: Sudbury Breccia —dike breccias occurring up to 80 km from the Sudbury Igneous Complex (SIC); Footwall rocks and Footwall Breccia — brecciated, shocked crater floor materials, in part thermally metamorphosed by the overlying SIC; Sublayer and Offset Dikes, Main Mass of the SIC and Basal Member of the Onaping Formation (OF) — geochemically heterogeneous coherent impact melt complex ranging from inclusion-rich basal unit through a dominantly inclusion-free to a capping inclusion-rich impact melt rock; Grey Member of OF — melt-rich impact breccia (suevite); Green Member of OF — thin layer of fall back ejecta; Black Member of OF — reworked and redeposited breccia material; Onwatin and Chelmsford Formations — post-impact sediments. Observational and analytical data support an integrated step-by-step impact model for the genesis of these units. Analysis of the present spatial distribution of various impact-related lithologies and shock metamorphic effects result in an estimated original rim-to-rim diameter of the final crater of 200 or even 280 km for the Sudbury Structure, prior to tectonic thrusting and deformation during the Penokean orogeny. 相似文献
14.
Guy Jalut Jean Jacques Dedoubat Michel Fontugne Thierry Otto 《Quaternary International》2009,200(1-2):4
The Mediterranean climate and its variability depend on global-scale climate patterns. Close correlations appear when comparing Holocene palaeoenvironmental data (lake levels, fluvial activity, Mediterranean surface temperature and salinity, marine sedimentation) with the main stages of the history of the circum-Mediterranean vegetation. They indicate an evolution of the Mediterranean biome controlled by the climate and emphasize the teleconnections between the climate of the Mediterranean area and the global climatic system. In the circum-Mediterranean area, the Holocene can be divided into three periods: a lower humid Holocene (11 500–7000 cal BP) interrupted by dry episodes; a transition phase (7000–5500 cal BP) during which occurred a decrease in insolation as well as the installation of the present atmosphere circulation in the northern hemisphere; and an upper Holocene (5500 cal BP—present) characterized by an aridification process. Throughout the Holocene, humans used and modified more or less strongly the environment but the climatic changes were the determining factors of the evolution of the Mediterranean biome. Societies had to adapt to natural environmental variations, their impact on the environment increasing the ecological consequences of the global changes. 相似文献
15.
M. A. Kharinov V. K. Konnikova A. V. Ipatov I. A. Ipatova A. K. Erkenov 《Astronomy Reports》2020,64(4):350-362
The presented observation results of the blazar J0238+1636 were obtained in: 2014–2019 with the RATAN-600 radio telescope from the Special Astrophysical Observatory of the Russian Academy of Sciences at 2.3, 4.8, 8.2, 11.2, and 21.7 GHz; and 2015–2017 with the 32-m Zelenchuk and Badary radio telescopes of the Institute of Applied Astronomy of the Russian Academy of Sciences at 4.84 and 8.57 GHz. Two flares were detected on the long-term light curve. The time scale for variability on the rising branch of the first flare is τvar = 0.5 year, and the upper limit for the linear and angular sizes of the emitting region at 21.7 GHz are 0.3 pc and 0.05 mas, respectively. The brightness temperature is Tb ≥ 2.6 × 1013 K, and the Doppler factor is δ ≥ 3. In three sets of the source’s daily observations, which lasted up to three months each, no significant variability on the day-to-day scale was found after subtracting the long-term variability. In the RT-32 data, the intraday variability (IDV) was found at a frequency of 4.84 GHz in three out of 15 sessions and at 8.57 GHz in two out of 13 sessions. The characteristic times for variability are 4−5 hours. 相似文献
16.
Simulation of Non-Gaussian Transmissivity Fields Honoring Piezometric Data and Integrating Soft and Secondary Information 总被引：1，自引：0，他引：1
The conditional probabilities (CP) method implements a new procedure for the generation of transmissivity fields conditional to piezometric head data capable to sample nonmulti-Gaussian random functions and to integrate soft and secondary information. The CP method combines the advantages of the self-calibrated (SC) method with probability fields to circumvent some of the drawbacks of the SC method—namely, its difficulty to integrate soft and secondary information or to generate non-Gaussian fields. The SC method is based on the perturbation of a seed transmissivity field already conditional to transmissivity and secondary data, with the perturbation being function of the transmissivity variogram. The CP method is also based on the perturbation of a seed field; however, the perturbation is made function of the full transmissivity bivariate distribution and of the correlation to the secondary data. The two methods are applied to a sample of an exhaustive non-Gaussian data set of natural origin to demonstrate the interest of using a simulation method that is capable to model the spatial patterns of transmissivity variability beyond the variogram. A comparison of the probabilistic predictions of convective transport derived from a Monte Carlo exercise using both methods demonstrates the superiority of the CP method when the underlying spatial variability is non-Gaussian. 相似文献
17.
Relative spatial soil geochemical variability along two transects across the United States and Canada 总被引：4，自引：4，他引：0
To support the development of protocols for the proposed North American Soil Geochemical Landscapes project, whose objective is to establish baselines for the geochemistry of North American soils, two continental-scale transects across the United States and Canada were sampled in 2004. The sampling employed a spatially stratified random sampling design in order to estimate the variability between 40-km linear sampling units, within them, at sample sites, and due to sample preparation and analytical chemical procedures. The 40-km scale was chosen to be consistent with the density proposed for the continental-scale project. The two transects, north–south (N–S) from northern Manitoba to the USA–Mexico border near El Paso, Texas, and east–west (E–W) from the Virginia shore north of Washington, DC, to north of San Francisco, California, closely following the 38th parallel, have been studied individually. The purpose of this study was to determine if statistically significant systematic spatial variation occurred along the transects. Data for 38 major, minor and trace elements in A- and C-horizon soils where less than 5% of the data were below the detection limit were investigated by Analysis of Variance (ANOVA). A total of 15 elements (K, Na, As, Ba, Be, Ce, La, Mn, Nb, P, Rb, Sb, Th, Tl and W) demonstrated statistically significant (p < 0.05) variability at the between-40-km scale for both horizons along both transects. Only Cu failed to demonstrate significant variability at the between-40-km scale for both soil horizons along both transects.The patterns of relative variability differ by transect and horizon. The N–S transect A-horizon soils show significant between-40-km scale variability for 29 elements, with only 4 elements (Ca, Mg, Pb and Sr) showing in excess of 50% of their variability at the within-40-km and ‘at-site’ scales. In contrast, the C-horizon data demonstrate significant between-40-km scale variability for 26 elements, with 21 having in excess of 50% of their variability at the within-40-km and ‘at-site’ scales. In 36 instances, the ‘at-site’ variability is statistically significant in terms of the sample preparation and analysis variability. It is postulated that this contrast between the A- and C- horizons along the N–S transect, that is dominated by agricultural land uses, is due to the local homogenization of Ap-horizon soils by tillage reducing the ‘at-site’ variability. The spatial variability is distributed similarly between scales for the A- and C-horizon soils of the E–W transect. For all elements, there is significant variability at the within-40-km scale. Notwithstanding this, there is significant between-40-km variability for 28 and 20 of the elements in the A- and C-horizon data, respectively. The differences between the two transects are attributed to (1) geology, the N–S transect runs generally parallel to regional strikes, whereas the E–W transect runs across regional structures and lithologies; and (2) land use, with agricultural tillage dominating along the N–S transect. The spatial analysis of the transect data indicates that continental-scale maps demonstrating statistically significant patterns of geochemical variability may be prepared for many elements from data on soil samples collected on a 40 × 40 km grid or similar sampling designs resulting in a sample density of 1 site per 1600 km2. 相似文献
18.
Amplitude and style of ground vibration from two types of pile driving — vibrodriver (periodic) and drophammer (transient) — are considered for the analysis of deformation in a portal frame structure. It is argued that the three-dimensional character of the vibration should be determined in the form of a resultant vector and this requires the measurement of vibration in three directions at right angles together with information on the sense of the motion along each orthogonal axis of vibration. Such resultant vector data during the period of vibration are best processed and presented in the style of a suite of hemispherical projections that comprise upper and lower hemisphere forms, respectively embodying components of upward and downward vibrational motion. It is shown that analysis for the dynamic stability of a simple block foundation is assisted by reference to the hemispherical projection representation and by the use of ground surface acceleration data. 相似文献
19.
Logratio Analysis and Compositional Distance 总被引：10，自引：0，他引：10
J. Aitchison C. Barceló-Vidal J. A. Martín-Fernández V. Pawlowsky-Glahn 《Mathematical Geology》2000,32(3):271-275
The concept of distance between two compositions is important in the statistical analysis of compositional data, particularly in such activities as cluster analysis and multidimensional scaling. This paper exposes the fallacies in a recent criticism of logratio-based distance measures—in particular, the misstatements that logratio methods destroy distance structures and are denominator dependent. Emphasis is on ensuring that compositional data analysis involving distance concepts satisfies certain logically necessary invariance conditions. Logratio analysis and its associated distance measures satisfy these conditions. 相似文献
20.
Ayodele Owoade 《Journal of African Earth Sciences》1995,20(3-4)
Aquifer systems in tropical hard rock catchments generally comprise a sequence of three layers — an upper layer of weathered material (regolith), an intermediate zone of semi-weathered material and a basal zone of fresh, but often fractured, rocks. There is evidence that all three are hydraulically connected and for the purpose of this paper the three zones are referred to as ‘regolith-fractures aquifer’ (RFA). Field evidence is presented which shows that the bulk of the drawdown in boreholes in RFA systems is generally incurred during the early period of pumping — usually within 200 minutes of pump start-up. Well losses are an important part of this early drawdown and a judicious management of the pumping scheme during the early period could result in a reduction in the drawdown. One way of managing the pumping scheme is through phased pumping, whereby a desired total discharge (Q) is imposed in incremental steps (Q1, Q2, …, Q) during the early period of pumping (generally the first 200 to 300 minutes). This paper presents field data which shows reductions in drawdons arising from phased pumping during the early period. 相似文献