標(biāo)題: Titlebook: Elements of Structural Geology; E. Sherbon Hills Book 1972 E. Sherbon Hills 1972 fault.structural geology.tectonics [打印本頁(yè)] 作者: 公款 時(shí)間: 2025-3-21 16:14
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書(shū)目名稱(chēng)Elements of Structural Geology讀者反饋
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作者: leniency 時(shí)間: 2025-3-21 20:50
https://doi.org/10.1007/978-3-658-28492-3re aesthetically satisfying in themselves; but above all, the implications of folding with regard to movements in the crust of the earth have always assumed major importance in tectonic thought and consequently in the philosophy of geological science.作者: 濕潤(rùn) 時(shí)間: 2025-3-22 04:28 作者: Bother 時(shí)間: 2025-3-22 08:35
Preoperative Radiological Assessmentdissect the earth. This is a fundamental tenet of physiographic lore, but has been strangely neglected as a method of study by which inferences may be drawn from geomorphology as to geological structure. The topic has recently received some attention as ., but . is preferred as having a wider connotation..作者: 障礙 時(shí)間: 2025-3-22 10:40 作者: BURSA 時(shí)間: 2025-3-22 15:42 作者: BURSA 時(shí)間: 2025-3-22 18:44
Mandala Urbanism, Landscape, and Ecologyo study by the established principles of civil engineering and soil mechanics in relation to earth-masses. Certain structures of a different origin, for instance those due to chemical changes, especially hydration, and to glacial action, are also for convenience dealt with here.作者: Fermentation 時(shí)間: 2025-3-22 22:27 作者: dearth 時(shí)間: 2025-3-23 01:45 作者: 有效 時(shí)間: 2025-3-23 05:52 作者: grounded 時(shí)間: 2025-3-23 12:50 作者: BRIBE 時(shí)間: 2025-3-23 17:48 作者: deface 時(shí)間: 2025-3-23 19:28
Non-diastrophic structures,g of unconsolidated deposits, and in landslides and related effects. In Chapter XI gravity is further discussed as a factor in diastrophism, but the structures now to be described are generally recognized as .. This view is taken because these structures do not necessarily involve deformation of the作者: 捐助 時(shí)間: 2025-3-23 23:35 作者: 歪曲道理 時(shí)間: 2025-3-24 03:29 作者: Medicaid 時(shí)間: 2025-3-24 06:41
Planar and linear structures and jointing,es, including both those which being visible to the naked eye may be mapped in the field, and those that can be determined only under the microscope, and must accordingly be studied in the laboratory. In this chapter we shall deal with macro-structures, and later (Chapter XIII) with structural petro作者: 大吃大喝 時(shí)間: 2025-3-24 13:35
Faults,lt refers both to the plane itself, which is called the ., and to the displacements that have gone on along it. In conformity with the ideas on plastic slip and shear-fracturing expressed in Chapter III, fault planes may be shear-fractures along which the internal cohesion of the rocks has been dest作者: 我就不公正 時(shí)間: 2025-3-24 17:50
Folds,ation on the mechanism that caused the crumpling of the strata; the interest and beauty of the sweeping curves of great folds drawn in cross-section are aesthetically satisfying in themselves; but above all, the implications of folding with regard to movements in the crust of the earth have always a作者: 甜瓜 時(shí)間: 2025-3-24 19:59 作者: Obstreperous 時(shí)間: 2025-3-25 02:09
Major structures and tectonics,e belts, metamorphic zones, and so on, is an outstanding geological fact which leads to the consideration of the regional deployment of major structures, and their spatial relationships one to another. Taken in conjunction with other data such as the distribution of sediments, the kinds of rocks and作者: 草率男 時(shí)間: 2025-3-25 06:15 作者: 不能約 時(shí)間: 2025-3-25 07:36
Structural Petrology,s, and is known as .. The second involves the attempt to establish relationships between these geometrical properties and the movements or strains involved in the generation of the fabric, and even to infer possible causative forces or stresses. This is known as petrotectonics. These two aspects of 作者: inchoate 時(shí)間: 2025-3-25 15:24 作者: GLADE 時(shí)間: 2025-3-25 15:59
https://doi.org/10.1007/978-981-10-2225-8e physical and chemical environment of materials, of the duration of time over which forces act, and of differences in the fine structure of the materials themselves, as, for example, between a crystalline solid and a clay—water, or sand—water mixture. This chapter, then, deals with special aspects of the subject of deformation.作者: 褪色 時(shí)間: 2025-3-25 21:09 作者: 手段 時(shí)間: 2025-3-26 03:10 作者: Ankylo- 時(shí)間: 2025-3-26 06:34 作者: 儲(chǔ)備 時(shí)間: 2025-3-26 12:09
Cleavage,s of metamorphism and deformation.. In anyone bed, cleavage is ., which it may intersect at any angle, but because it is influenced by the physical properties of rocks it may change its attitude in passing from one bed to another (Fig. X-I).作者: 密碼 時(shí)間: 2025-3-26 14:51 作者: inflate 時(shí)間: 2025-3-26 20:15
978-0-412-20750-1E. Sherbon Hills 1972作者: 富足女人 時(shí)間: 2025-3-26 23:47
Overview: 978-0-412-20750-1978-94-009-5843-2作者: 稀釋前 時(shí)間: 2025-3-27 03:26 作者: harbinger 時(shí)間: 2025-3-27 08:08 作者: FECK 時(shí)間: 2025-3-27 11:19
Managing with Sense and Sensitivityn of rock-structures. Without for the moment defining precisely what is meant by rock-structures, let us consider any geological cross-section showing beds in various attitudes — flat-lying or inclined, folded or faulted — perhaps in places intruded by igneous rocks or covered with lava-flows, and a作者: Accolade 時(shí)間: 2025-3-27 15:40
Managing your Mental Health during your PhData in a sedimentary succession, and the presence within any one bed of a fine lamination or texture which is connected with its deposition (Fig. II-1). In general each bed is fairly homogeneous and may be distinguished from other beds by some characteristic feature such as texture (e.g. shale, sand作者: 微不足道 時(shí)間: 2025-3-27 21:27 作者: 獎(jiǎng)牌 時(shí)間: 2025-3-28 00:16 作者: ostensible 時(shí)間: 2025-3-28 02:50 作者: gentle 時(shí)間: 2025-3-28 06:21
https://doi.org/10.1007/978-981-10-1035-4es, including both those which being visible to the naked eye may be mapped in the field, and those that can be determined only under the microscope, and must accordingly be studied in the laboratory. In this chapter we shall deal with macro-structures, and later (Chapter XIII) with structural petro作者: Parameter 時(shí)間: 2025-3-28 11:55
https://doi.org/10.1007/978-3-322-93235-8lt refers both to the plane itself, which is called the ., and to the displacements that have gone on along it. In conformity with the ideas on plastic slip and shear-fracturing expressed in Chapter III, fault planes may be shear-fractures along which the internal cohesion of the rocks has been dest作者: 密切關(guān)系 時(shí)間: 2025-3-28 15:06
https://doi.org/10.1007/978-3-658-28492-3ation on the mechanism that caused the crumpling of the strata; the interest and beauty of the sweeping curves of great folds drawn in cross-section are aesthetically satisfying in themselves; but above all, the implications of folding with regard to movements in the crust of the earth have always a作者: BARB 時(shí)間: 2025-3-28 18:44 作者: chastise 時(shí)間: 2025-3-29 00:02
https://doi.org/10.1007/978-3-663-10725-5e belts, metamorphic zones, and so on, is an outstanding geological fact which leads to the consideration of the regional deployment of major structures, and their spatial relationships one to another. Taken in conjunction with other data such as the distribution of sediments, the kinds of rocks and作者: Harness 時(shí)間: 2025-3-29 04:58 作者: POWER 時(shí)間: 2025-3-29 07:18 作者: 低三下四之人 時(shí)間: 2025-3-29 13:04 作者: POWER 時(shí)間: 2025-3-29 17:09 作者: GLUT 時(shí)間: 2025-3-29 21:47
Tectonic analysis of folds,Folds have so far been considered chiefly in cross-section, and it is now necessary to deal with fold geometry in three dimensions. Although much use is made in geological reports of cross-sections of folds, their properties along the regional trend are more immediately obvious in regional mapping and map study.作者: 粗俗人 時(shí)間: 2025-3-30 01:13 作者: VICT 時(shí)間: 2025-3-30 07:55
https://doi.org/10.1007/978-3-322-87130-5ure. The slow deformation or . of rocks under low stress will be discussed later, but whatever weight may be attached to this as a factor in the formation of rock-structures. one may be quite certain that the yielding of a great many rocks took place under conditions such that the deformation was an作者: Agility 時(shí)間: 2025-3-30 11:37 作者: 熔巖 時(shí)間: 2025-3-30 13:29 作者: 口味 時(shí)間: 2025-3-30 18:46 作者: Urgency 時(shí)間: 2025-3-30 23:58 作者: 節(jié)省 時(shí)間: 2025-3-31 01:31 作者: Default 時(shí)間: 2025-3-31 08:53
Faults,ich conforms with the principles of stress-strain relationships already discussed. The stress-conditions that induce faulting in relatively homogeneous rocks do, however, vary widely, and faulting is also strongly influenced by inhomogeneities, particularly where strata of markedly different physica作者: 闡明 時(shí)間: 2025-3-31 11:33
Major structures and tectonics, regional strike as well as in cross-section. Since then geological knowledge has vastly expanded and geophysics has provided an entirely new body of data relevant to the inner structure of the globe, the former distribution of continents in the geological past, and the structure and evolution of oc作者: 玉米 時(shí)間: 2025-3-31 16:25 作者: Instinctive 時(shí)間: 2025-3-31 20:35 作者: AROMA 時(shí)間: 2025-4-1 00:26
