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61.
Gordon Kaufman 《Natural Resources Research》1994,3(4):304-314
The relative efficiencies of alternative geometric patterns of both discrete borehole and continuous grid line search have been extensively discussed in the mathematical geology literature. However, an equally important problem has received virtually no attention: How to use a sample of properties of geologic anomalies detected by grid line search of a region to estimate systematically both the number and size distribution of geologic anomalies missed by the search. We show how estimation methods developed in the sample survey design literature can be adapted to this problem, and we apply these methods to data describing 94 anomalies identified by a seismic reconnaissance survey. 相似文献
62.
Gordon E. Bigelow 《地球表面变化过程与地形》1984,9(4):383-390
Tumbler simulations of abrasion processes affecting rocks on basaltic marine benches have clarified the effects of mass and volume of rock fragments on their rate of wear. Several experiments indicate that rate of basalt wear increases with mass in the interval 1 g to 8 g, but is not related to volume of fragments abraded in seawater. Relatively small quantities of rock flour suspended in the immersant seawater substantially reduced the rate of basalt wear. Basalt and calcareous beachrock responded differently in systems with both rock types tumbling together. Examination of the cuttings from these low-energy encounters suggests that abrasion on elevated benches along exposed seacoasts reduces virtually all clastic material to particles of silt size or smaller, producing essentially no sand. 相似文献
63.
The average local structure of a rhyolitic composition glass has been determined at 25°C using X-ray radial distribution analysis (RDA) and quasi-crystalline modelling and is best described as similar to that in a stuffed framework composed principally of six-membered rings of Si and Al tetrahedra (basically a stuffed tridymite-like model). Using this model it is possible to calculate a density (2.41 g/cm3) which compares well with the measured density (2.40 g/cm3); a structural model based on four-membered rings (an albite-like model) results in a substantially higher calculated density (2.60 g/cm3). We suggest that the rhyolite glass structural model is appropriate for rhyolitic melts, based on evidence from the recent literature. New viscosity data for an anhydrous rhyolite composition measured between 1200°C and 1500°C are presented and interpreted in terms of our proposed structural model and previous melt structure models for the major normative components of rhyolite. A mechanism for diffusion and viscous flow in framework silicate melts (including rhyolite composition) is proposed on the basis of recent molecular orbital calculations and molecular dynamics simulations of silicate and fluoride melts. 相似文献
65.
66.
Vertical distributions of particulate silica, and of production and dissolution rates of biogenic silica, were determined on two N-S transects across the Pacific sector of the Antarctic Circumpolar Current during the austral spring of 1978. Particulate silica profiles showed elevated levels in surface water and near the bottom, with low (35–110 nmol Si · 1?1) and vertically uniform values through the intervening water column. Both the particulate silica content of the upper 200 m and the production rate of biogenic silica in the photic zone increased from north to south, reaching their highest values near the edge of the receding pack ice. A significant, but variable, fraction (18–58%) of the biogenic silica produced in the surface layer was redissolving in the upper 90–98 m. Net production of biogenic silica in the surface layer (production minus dissolution) was proceeding at a mean rate of ca. 2 mmol Si · m?2 · day?1. This is ca. 4 times greater than the most recent estimate of the mean accumulation rate of siliceous sediments beneath the ACC. We estimate, based on mass balance, that the mean dissolution rate of biogenic silica in subsurface water column in the Southern Ocean is 1.2–2.9 mmol Si · m?2 · day?1. 相似文献
67.
Tectonic systems and the deposition of iron-formation 总被引:8,自引:0,他引:8
Gordon A. Gross 《Precambrian Research》1983,20(2-4)
The iron-formation group of chemically precipitated cherty iron-rich sediments ranges in age from Early Precambrian to Recent and is composed of a variety of lithological facies. Iron-formations are classified as Lake Superior and Algoma types to emphasize the contrasting conditions in the spectrum of sedimentary-tectonic environments in which they formed. Thick stratigraphic units of Lake Superior type iron-formation, which form the most extensive iron ranges of the world, are part of sedimentary-tectonic systems that developed along the margins of cratons or continental platforms and were deposited over extended periods of time under relatively stable tectonic conditions. The Algoma type iron-formations were deposited with volcanic rocks and greywacke in various tectonic-volcanic systems, formed under more dynamic tectonic conditions, but are otherwise comparable to present day spreading ridges on the ocean floor. The thick sequences of Lake Superior type iron-formation deposited between 2.7 and 2.0 Ga form part of major sedimentary-tectonic systems that extended along the margins of continents. Direct biogenic factors and the composition of the atmosphere probably had only limited influence on the precipitation of these chemical sediments. 相似文献
68.
In the context of challenging targets for renewable energy generation, this paper draws out social implications of moves towards low carbon energy systems. As renewable energy develops as a heterogeneous category, many potential forms of social relation between 'publics' and technologies are emerging. Utilising perspectives from science and technology studies, we outline five modes in which renewable energy has been implemented in the UK and how these involve different configurations of technology and social organisation. We argue that a multiplicity of roles for 'the public' are implicated across this increasingly complex landscape, cutting across established categories and raising questions of meaning, differentiation, interrelation and access. Policy assumptions and conceptions are questioned, highlighting that dominant characterisations of public roles have been part of a concentration on particular socio-technical pathways to the exclusion of others. 相似文献
69.
Hypothesized large-scale climatic extremes require verification from distantregions in order toconfirm the magnitude and timing of such events. Three of the most massivehypothesized volcanic events of the past two millennia, occurring in or aboutAD 536, 934 and1258, had profound climatic and demographic repercussions over much of Europe,the MiddleEast, and other areas, according to historical accounts recently described inStothers (1998, 1999,2000) as well as other research. Here we report on frost ring and otherdendrochronologicalevidence derived from a 1738-year tree-ring chronology from Mongolia andmillennial-scaletree-ring data from northern Siberia which demonstrate that these three eventsmay have alsoimpacted conditions in these distant regions. 相似文献
70.
A statistical test has revealed that abrupt regional climate changes are produced in a coupled atmosphere-ocean general circulation
model. Abrupt changes are detected over much of the globe although the occurrence frequency is small over the continents.
Over the tropical Pacific Ocean and northern Pacific Ocean, surface air temperature (SAT) and sea level pressure (SLP) shift
rapidly on decadal time scales. The regional climate changes presented here have been classified into three types. The first
type consists of statistically significant shifts in SLP and statistically significant shifts in SAT which are of opposite
sign, and which are reinforced through a positive feedback between the atmosphere and the ocean. The second type is for those
occurrences where changes are of the same sign. The third type includes those with a significant shift in only one meteorological
element. The second and third types are generally generated by changes in air pressure and wind fields induced by changes
of the first type. For example, when SLP increases and sea surface temperature (SST) decreases abruptly in the tropical Pacific
Ocean, it triggers abrupt regional changes in middle and high latitudes. The abrupt changes in the model climate have characteristics
which are very similar to those of observed rapid shifts. Thus, it is concluded that abrupt changes are a predominant part
of regional climate change on decadal time scales.
Received: 11 February 1999 / Accepted: 18 May 2000 相似文献