| 词汇 | example_english_basin |
| 释义 | Examples of basinThese examples are from corpora and from sources on the web. Any opinions in the examples do not represent the opinion of the Cambridge Dictionary editors or of Cambridge University Press or its licensors. Both basins accumulated great thicknesses of molasse comprising fluviatile conglomerates and lacustrine shales of continental affinity. However, many people who enjoy eating raw fish still remain in certain areas, especially in the basins of rivers. Indeed, perioddoubling cascades up to period seven with chaotic windows were recorded, and a thorough study of the basins of attraction was undertaken. Six such basins representative of different types of small exchange environments were studied, using both geochemical and biochemical parameters. Their comparison with the tectonically more active foreland basins can thus help to distinguish between global and local controls. Interpretation of floristic (both palynology and macrofloral) records of individual basins heavily depends on how data were obtained and processed. In all three basins, this mudstone-dominated interval passes into sandstonedominated sediments of a braided fluvial system. If these asymmetric solutions are time dependent and their basins of attraction come close enough, we can expect reconnections, mergings and, working backwards, splittings. We are especially interested in showing how inverse theory can be used to extract quantitative information about a basin's history. Coverage is excellent and provides an opportunity to develop a comprehensive understanding of both basins. The initial stage of sedimentation in these basins was characterized by terrestrial and shallow marine deposits that consist of both clastic and carbonate deposition. Thus, models that have large basins of attraction might be significant not only in simulations but also in experimental settings. By contrast the chapter on intracontinental basins is rather too thin and overpreoccupied with hydrocarbon occurrence to do full justice to its subject. Moreover, many cities in both prefectures are located in natural basins. Is it possible that all three boundaries of these basins coincide? The purpose of this paper is to describe the structure and properties of basins and their boundaries for two-dimensional diffeomorphisms. The basins shown are open, connected, simply connected sets. The advantage of the model proposed here is that it affords a rapid calculation tool for exploring parametric effects in closed basins. The success of such a comparative analysis depends heavily on the character and completeness of the data from the individual basins. Deposition in these basins is controlled mainly by tectonics and sedimentary influx. The different basins may have experienced similar sequences of vegetation change, but not necessarily synchronously. The third grouping included those basins with less well-studied lycophyte floras, where the apparently low species diversity has undoubtedly affected the results. Small basins also briefly developed, filled with silt and clays; some coals also occur in these deposits. The most important temperature data used to characterize the geothermal field of sedimentary basins are those from systematic steady-state temperature measurements and well tests. The final papers are studies of tectonic events as recorded in the stratigraphy of the many sedimentary basins. A general inverse method for modelling extensional sedimentary basins. The progressive contraction of oceanic crust caused the uplift of previously rifted continental margin and platforms and the formation of foredeep flysch basins. A similar mechanism is present at numerous thermal springs in sedimentary basins elsewhere in the world. One gap in the current treatment is the limited coverage of the basins containing hydrocarbon reserves. From it were taken basins of what appeared to be boiled rice, which was eagerly fought for and devoured. We have not obtained a mathematical proof of whether riddled basins appear in the present model. However, studies of each of these species have been carried out in different ocean basins and over time periods of ten years and more. Instead, language processing is perhaps better described as a single trajectory through a high-dimensional space of multiple competing attractor basins. The high salt content of the interior par t of the basins would result in persistent poor water quality there. Percentages on the right give the probabilities of folding pathways leading to the six principal basins of attractions. The suprasubduction zone tectonic setting includes island arcs, forearc and backarc basins for the generation of oceanic crust (ophiolite). A thermal model is then constructed for these basins using transient finite element techniques. One section is devoted to mobilization associated with the enigmatic polygonal fault systems increasingly evidenced from sedimentary basins. Next follow three papers on individual basins that together illustrate the value of studying the soils in a sedimentary succession. Sedimentary basins record vertical motion as a function of time, therefore the temporal variation in strain rate can be determined from a basin's subsidence history. Clearly the debate as to the relevance of sequence stratigraphy in tectonically active basins is not yet over. During formation of the basins the ophiolite nappes were moving. Major chapters follow the large chapter on the development of the basins. Why are there ocean basins, continents and mountains? The model states are divided into several basins of attraction, each with locally stable attracting stationary state. Vegetation of the area consists primarily of a mosaic of forest and savanna, with forest within savanna zones restricted to riparian habitats and headwater basins. In so doing, we obtain correct transition times, and may detect transitions to other basins more easily. Many of the highland lake basins were abandoned. The stucco basins are filled in and sealed, and walls are built directly above them. Between the plateau and the lake are the former ash basins, partly obscured by thick planting and by the local ecological society's landscaping. Beds and enamel basins and sink baths and all kinds of stuff. Simulations are made using time frames and spatial scales considering six scenarios of population, and economic activity growth in seven river basins. A primary analytic concern remains identifying the basins of attraction for strategies which are behaviorally equivalent to cooperative, or just, actions. Also, each cycle of parabolic or ø attracting basins contains a critical point. In conclusion, it appears that long basins, with relatively weak convective forcing, do not experience flushing of deep water by the entrainment mechanism described above. The third iterate of the map therefore has three basins and their boundaries are fractal. The next result is for showing those properties hold for a collection of basins. Thus, minimal attractors, minimal quasi-attractors and their basins have either measure zero or one. The progressive contraction of oceanic crust caused the uplift of previously rifted continental margin and platforms, and formation of foredeep flysch basins. In most basins, this drop in diversity correlates with a depositional break, which makes it difficult to ascertain its precise stratigraphical location. Also, different kinds of evaporitic basins and the importance of hydrology in their development are emphasized. In contrast to the sectors with global markets, water is likely to have only a regional market because it is hard to transfer across basins. The basins are separated from each other by shallow bars. Ablution facilities included flush toilets, hand basins and showers, which were all found to be in a clean condition. The main task of this organization would be to collect and provide impartial data about various river basins. The thick lines delimit the prospected river basins. There is nothing here on different types of basins or climate. Far from plate boundaries, we encounter examples of isostasy at intracratonic basins, mid-plate hotspot swells and seamount chains. Sedimentary basins formed and carried piggyback on active thrust sheets. Evaporitic sedimentation stopped, carbonate platform systems grew and in the intra-platform basins, calcarenitic-calciruditic facies were resedimented. During this period, transtensional basins and the modern morphological and tectonic elements of the region were developed. In summary this book provides a useful up-to-date analysis of structural models for rift basins and the influence of structure on sedimentation. Perhaps more importantly the memoir provides an excellent teaching resource as an example of an industry-style analysis of potentially productive basins. In this study, we use a substantial database of welllog and other stratigraphic information to calculate the tectonic subsidence histories of two such intracratonic basins. As a result, reverse faults and monoclines are associated with earlier normal faults and inversional anticlines are superimposed upon earlier basins. Modelling anatexis in intra-cratonic rift basins than the period of melting (1.0-7.6 m. y.), then our models will overestimate the amount of melt. Many systems are deposited in basins with a pre-existing topography sufficient to steer density flows or confine their deposition to sub-basins within the system. When the model possesses several locally stable equilibria, the equilibrium distribution assigns generally unequal probabilities to the basins. The basins of attraction of the fixed points are concerned with the sensitivity of the initial conditions of the models. The rains feed many ponds or basins in the eastern part of the park, which hold water either temporarily or permanently. No contamination was recorded in basins of sterile soil placed amongst the forest samples. Such a change may have taken place in the lowland paralic basins, but in upland basins the change was more gradual and occurred significantly earlier. Modelling subsidence, heat flow, and hydrocarbon generation in extensional basins. The other studied locations are from the centres of epicontinental seas and basins and were thus far removed from the influence of oceanic circulation regimes. Remarkably, during the peak intensity of anoxia within the basins, oxygenpoor water even spread into shallow forereef settings. The origin of these sedimentary basins is still poorly understood. In addition, syngenetic graphite can be used for tracing ancient organic-rich sedimentary basins. In addition, ovens and platforms, benches and basins of clay were unearthed in and between the building remains. Furthermore, crustal deformation associated with tectonic uplift and exposure of ancient basins often disrupts the lateral continuity of stratigraphic indicators and renders their correlation problematic. In general, this width is small relative to the basin's characteristic length scale. At any time, its lateral position is determined by a complex interaction of the basin's boundary conditions. Fluctuations in the basin's boundary conditions drive it from this equilibrium state. Stratigraphers use this record to solve the inverse problem: the strata are used to infer a basin's history of sediment supply, tectonism, and base level. The features consisted of two pits in the bedrock plastered with stucco to form subfloor basins. The basins may have been created and utilized prior to the construction of the building or just before the one room was constructed. The slow movement in these storage basins allows some of the suspended matter to settle out, and the clarified water is taken for use. The rate is lower on younger lithosphere underlying shallow ocean, but greater on older lithosphere underlying the deeper parts of ocean basins. Chapter 9 discusses the thermal histories of basins and nicely ties together concepts presented throughout the book. Differences in diagenetic alteration of matrix sediments between both basins do not have a considerable impact on brachiopod shell isotopic composition. These examples are from corpora and from sources on the web. Any opinions in the examples do not represent the opinion of the Cambridge Dictionary editors or of Cambridge University Press or its licensors. |
反思网英语在线翻译词典收录了377474条英语词汇在线翻译词条，基本涵盖了全部常用英语词汇的中英文双语翻译及用法，是英语学习的有利工具。