標(biāo)題: Titlebook: Geological maps: An Introduction; Alex Maltman Book 1990 Alex Maltman 1990 document.information.remote sensing.time [打印本頁] 作者: Inoculare 時(shí)間: 2025-3-21 20:00
書目名稱Geological maps: An Introduction影響因子(影響力)
書目名稱Geological maps: An Introduction影響因子(影響力)學(xué)科排名
書目名稱Geological maps: An Introduction網(wǎng)絡(luò)公開度
書目名稱Geological maps: An Introduction網(wǎng)絡(luò)公開度學(xué)科排名
書目名稱Geological maps: An Introduction被引頻次
書目名稱Geological maps: An Introduction被引頻次學(xué)科排名
書目名稱Geological maps: An Introduction年度引用
書目名稱Geological maps: An Introduction年度引用學(xué)科排名
書目名稱Geological maps: An Introduction讀者反饋
書目名稱Geological maps: An Introduction讀者反饋學(xué)科排名
作者: 生意行為 時(shí)間: 2025-3-21 21:22
The nature of geological maps: the Ten Mile map of the UK and the 1: 2 500 000 map of the USA,ion. It provides a preliminary glimpse of the kinds of interpretations that can be made before the various concepts are examined more closely in succeeding chapters. We begin by noting some of the cartographic matters; first, the scale. Despite its time-honoured name, the Ten Mile UK map (Plate 1) i作者: Confirm 時(shí)間: 2025-3-22 02:55
The three-dimensional aspect: structure contours,maps. Many atlases begin by discussing the question of how to represent the spherical earth in a book. A similar problem is the portrayal of the undulations — the relief — of the earth’s surface. Early map-makers attempted to depict relief by drawing humpy little hills, often wildly exaggerated in h作者: vanquish 時(shí)間: 2025-3-22 05:09
Measurements in three dimensions: strike and dip, formation thickness and depth,n of rocks. Nevertheless, it is often necessary to specify the arrangement in words or numbers. Geologists do this by using the concept of strike and dip. The general idea was introduced in section 2.3.1; the first part of this chapter explains it in detail. The second part of the chapter expands on作者: 財(cái)政 時(shí)間: 2025-3-22 09:38 作者: 全部 時(shí)間: 2025-3-22 15:03 作者: 全部 時(shí)間: 2025-3-22 19:44 作者: 吹牛者 時(shí)間: 2025-3-22 23:24 作者: Acetaminophen 時(shí)間: 2025-3-23 02:49
Faults: the fundamentals,nd industrial work. They can, for example, interfere with the predictions of the mining geologist and cause special problems for the civil engineer. Even non-geologists may well know something about faults, if only the devastating effects of earthquakes that can arise from earth movements along them作者: 四海為家的人 時(shí)間: 2025-3-23 08:24
More on faults: contraction (thrust), extension, and strike-slip faults,e found. It is a rare map which does not show a fault of one kind or another, but this chapter is mainly concerned with those areas of the earth where faults are numerous and dominated by a particular type.作者: ASTER 時(shí)間: 2025-3-23 13:07
Igneous and metamorphic rocks; mineral deposits,ch unit tends to have an overall tabular shape, being bounded at its top and bottom by roughly parallel surfaces, which enables three dimensional interpretations from maps and sections. We have, however, to be more cautious with non-sedimentary materials, for their shape can be much less regular. It作者: Toxoid-Vaccines 時(shí)間: 2025-3-23 16:07
Geological history from maps,geological past. For the outcrop patterns on maps can reveal much of how the rock arrangements evolved through time; they enable interpretations to be made on the geological history of the map area, even the reconstruction of past geological environments. The timings that are derived from maps are u作者: 美麗的寫 時(shí)間: 2025-3-23 21:13 作者: Harbor 時(shí)間: 2025-3-24 01:18 作者: Urea508 時(shí)間: 2025-3-24 04:04 作者: 震驚 時(shí)間: 2025-3-24 06:38
Die trigonometrische Parametrisierung,e patterns on the map record the relationships between the rocks, from which the geologist can deduce much about their arrangement underground and about their geological history. This book is aimed at helping you develop these interpretive skills.作者: exceptional 時(shí)間: 2025-3-24 12:19 作者: Parallel 時(shí)間: 2025-3-24 16:24 作者: 考古學(xué) 時(shí)間: 2025-3-24 20:25
Innenansichten der Gelehrtenrepublik,ch unit tends to have an overall tabular shape, being bounded at its top and bottom by roughly parallel surfaces, which enables three dimensional interpretations from maps and sections. We have, however, to be more cautious with non-sedimentary materials, for their shape can be much less regular. It is with these that this chapter is concerned.作者: florid 時(shí)間: 2025-3-25 00:19
https://doi.org/10.1007/978-3-662-43117-7e of what goes into their production. Many stages are involved, from the detailed field surveying required for large-scale maps, through the preparation of ‘fair copy maps’, and the design and execution of a final printed version. Greenly and Williams (1930, p. 99) list twenty-three steps; this chapter merely outlines what is involved.作者: 有罪 時(shí)間: 2025-3-25 06:02 作者: 棲息地 時(shí)間: 2025-3-25 09:28 作者: 艱苦地移動(dòng) 時(shí)間: 2025-3-25 12:04
Unconformities,g directly upon vertical beds, became the first to perceive the long time interval implied by this kind of junction. The underlying material had to have been buried, lithified, rotated, and uplifted before the red sandstones were deposited on it.作者: monochromatic 時(shí)間: 2025-3-25 18:28
More on faults: contraction (thrust), extension, and strike-slip faults,e found. It is a rare map which does not show a fault of one kind or another, but this chapter is mainly concerned with those areas of the earth where faults are numerous and dominated by a particular type.作者: 盡管 時(shí)間: 2025-3-25 21:22
Igneous and metamorphic rocks; mineral deposits,ch unit tends to have an overall tabular shape, being bounded at its top and bottom by roughly parallel surfaces, which enables three dimensional interpretations from maps and sections. We have, however, to be more cautious with non-sedimentary materials, for their shape can be much less regular. It is with these that this chapter is concerned.作者: Calculus 時(shí)間: 2025-3-26 00:56 作者: Astigmatism 時(shí)間: 2025-3-26 07:33 作者: cogent 時(shí)間: 2025-3-26 10:52 作者: 茁壯成長(zhǎng) 時(shí)間: 2025-3-26 15:54
Die trigonometrische Parametrisierung,e patterns on the map record the relationships between the rocks, from which the geologist can deduce much about their arrangement underground and about their geological history. This book is aimed at helping you develop these interpretive skills.作者: Condescending 時(shí)間: 2025-3-26 17:30 作者: 門閂 時(shí)間: 2025-3-26 23:27
https://doi.org/10.1007/978-3-662-33095-1maps. Many atlases begin by discussing the question of how to represent the spherical earth in a book. A similar problem is the portrayal of the undulations — the relief — of the earth’s surface. Early map-makers attempted to depict relief by drawing humpy little hills, often wildly exaggerated in h作者: 有惡意 時(shí)間: 2025-3-27 03:08
https://doi.org/10.1007/978-3-658-11398-8n of rocks. Nevertheless, it is often necessary to specify the arrangement in words or numbers. Geologists do this by using the concept of strike and dip. The general idea was introduced in section 2.3.1; the first part of this chapter explains it in detail. The second part of the chapter expands on作者: Diatribe 時(shí)間: 2025-3-27 08:59
https://doi.org/10.1007/978-3-662-41363-0 this reason that cross-sections seem more immediately familiar than geological maps, and give a more striking picture of the arrangement of the beds. This is borne out historically, as sections were being drawn long before geological maps. Cross-sections portray the arrangement of the rocks as seen作者: Thrombolysis 時(shí)間: 2025-3-27 12:52
https://doi.org/10.1007/978-3-642-90756-2plications small errors could be costly. Now we return to the other approach to geological maps, that of making rapid visual assessments of the geology of an area. Central to this issue is an understanding of the outcrop patterns which appear on maps. Strictly, it is the junctions of outcrops, the t作者: certitude 時(shí)間: 2025-3-27 16:28 作者: Aggrandize 時(shí)間: 2025-3-27 19:49 作者: insidious 時(shí)間: 2025-3-28 01:57
https://doi.org/10.1007/978-3-662-33094-4nd industrial work. They can, for example, interfere with the predictions of the mining geologist and cause special problems for the civil engineer. Even non-geologists may well know something about faults, if only the devastating effects of earthquakes that can arise from earth movements along them作者: BET 時(shí)間: 2025-3-28 02:07 作者: Inflamed 時(shí)間: 2025-3-28 07:38
Innenansichten der Gelehrtenrepublik,ch unit tends to have an overall tabular shape, being bounded at its top and bottom by roughly parallel surfaces, which enables three dimensional interpretations from maps and sections. We have, however, to be more cautious with non-sedimentary materials, for their shape can be much less regular. It作者: 條街道往前推 時(shí)間: 2025-3-28 13:49
Die unbewu?te Familie: Rotierende Triadengeological past. For the outcrop patterns on maps can reveal much of how the rock arrangements evolved through time; they enable interpretations to be made on the geological history of the map area, even the reconstruction of past geological environments. The timings that are derived from maps are u作者: 誰在削木頭 時(shí)間: 2025-3-28 17:26
https://doi.org/10.1007/978-3-662-43117-7e of what goes into their production. Many stages are involved, from the detailed field surveying required for large-scale maps, through the preparation of ‘fair copy maps’, and the design and execution of a final printed version. Greenly and Williams (1930, p. 99) list twenty-three steps; this chap作者: 安撫 時(shí)間: 2025-3-28 20:25
Psychotherapie: Behandlung der Seele,use today have not always looked this way, and the earliest maps did not appear overnight. Geological maps have slowly evolved, in many ways reflecting the growth of geology itself. The first part of this chapter briefly outlines this history. Every geological map embodies parts of the story. The tr作者: Apogee 時(shí)間: 2025-3-28 23:21
Die unersch?pfliche Kraft des Einfachens the advent of colour-printing, refinement of ornament and increase in detail, but a geological map produced today would probably be quite intelligible to, say, William Smith. Suddenly, however, the rate of change has begun to accelerate. The purpose of this chapter is to touch on some aspects of t作者: BLA 時(shí)間: 2025-3-29 04:25
for a basic training in map- geologist will have his own views on geological maps - the work, the three-dimensional aspects involved formed the matters needing emphasis, the best methods of interpreta- single most difficult part of an introductory geology tion, good examples of maps, and so on. Ins作者: 巧思 時(shí)間: 2025-3-29 10:02 作者: BLUSH 時(shí)間: 2025-3-29 15:04
https://doi.org/10.1007/978-3-658-11398-8any purposes, the work will have to be done as accurately as possible, especially if sums of money are at risk. Some of the corrections that may have to be borne in mind for this kind of mapwork are introduced.作者: Junction 時(shí)間: 2025-3-29 19:24
Measurements in three dimensions: strike and dip, formation thickness and depth,any purposes, the work will have to be done as accurately as possible, especially if sums of money are at risk. Some of the corrections that may have to be borne in mind for this kind of mapwork are introduced.作者: 猜忌 時(shí)間: 2025-3-29 21:32 作者: 宴會(huì) 時(shí)間: 2025-3-30 02:12 作者: AGGER 時(shí)間: 2025-3-30 07:56 作者: 疼死我了 時(shí)間: 2025-3-30 10:21
Die unbewu?te Familie: Rotierende Triadensually relative, although reference to an absolute time scale may allow real dates to be assigned together with the establishment of time intervals and some idea of the rates at which events proceeded.作者: 反應(yīng) 時(shí)間: 2025-3-30 15:39 作者: separate 時(shí)間: 2025-3-30 17:37 作者: 有偏見 時(shí)間: 2025-3-30 23:37
Folds,mperature and longer times of deformation, the rocks respond to any stress by flow, and there is no fracture. The common way in which bedded sedimentary rocks deform in a ductile way is by warping into the wave-like shapes known as ..作者: cylinder 時(shí)間: 2025-3-31 03:25 作者: Cirrhosis 時(shí)間: 2025-3-31 05:06
Book 1990ic training in map- geologist will have his own views on geological maps - the work, the three-dimensional aspects involved formed the matters needing emphasis, the best methods of interpreta- single most difficult part of an introductory geology tion, good examples of maps, and so on. Instructors m作者: 免除責(zé)任 時(shí)間: 2025-3-31 09:10
