標(biāo)題: Titlebook: Rocks and Landforms; A. J. Gerrard Book 1988 J. Gerrard 1988 Denudation.Geomorphology.erosion.evolution.igneous rock [打印本頁] 作者: 戰(zhàn)神 時間: 2025-3-21 19:23
書目名稱Rocks and Landforms影響因子(影響力)
書目名稱Rocks and Landforms影響因子(影響力)學(xué)科排名
書目名稱Rocks and Landforms網(wǎng)絡(luò)公開度
書目名稱Rocks and Landforms網(wǎng)絡(luò)公開度學(xué)科排名
書目名稱Rocks and Landforms被引頻次
書目名稱Rocks and Landforms被引頻次學(xué)科排名
書目名稱Rocks and Landforms年度引用
書目名稱Rocks and Landforms年度引用學(xué)科排名
書目名稱Rocks and Landforms讀者反饋
書目名稱Rocks and Landforms讀者反饋學(xué)科排名
作者: Talkative 時間: 2025-3-21 20:15 作者: 持續(xù) 時間: 2025-3-22 03:11
Resistance to weathering,ular and submolecular scales. The primary weathering mechanisms are triggered by activating processes, promoted by a variety of activating agencies (Table 5.1). The weathering response is the progression of mineralogical, petrological and mechanical properties as they change through time. These chan作者: 1分開 時間: 2025-3-22 08:25
Instability in jointed and fissured rock,. Bisdom (1967) makes the important distinction between structural microcracks, which are present in unweathered rocks and are straight with angular intersections, and weathering microcracks, which are sinuous and exhibit dendritic patterns. As weathering progresses, grain boundaries become stained 作者: Ringworm 時間: 2025-3-22 10:57 作者: 少量 時間: 2025-3-22 15:52
ere was little detailed mention of process and scant attention to the properties of surface materials. There were, of course, exceptions. In the late 19th century G.K. Gilbert was stressing the equilibrium between landforms and processes. Many hydrologists were examining the detailed workings of river ‘system978-94-011-5985-2978-94-011-5983-8作者: entice 時間: 2025-3-22 17:23 作者: 忘川河 時間: 2025-3-22 22:26 作者: Arrhythmia 時間: 2025-3-23 03:09 作者: delusion 時間: 2025-3-23 07:52
A. J. Gerrarde solche aktivierte Adsorption k?nnen nur Moleküle erfahren, die in gro?em Abstand von der Adsorbens-Oberfl?che eine kinetische Energie in Richtung senkrecht zur Oberfl?che .. > .. besitzen. Zur Desorption der Adteilchen ist eine Desorptionsenergie .. aufzuwenden, die gleich der Adsorptionsenergie .作者: antedate 時間: 2025-3-23 13:04 作者: Density 時間: 2025-3-23 14:01
A. J. Gerrarde solche aktivierte Adsorption k?nnen nur Moleküle erfahren, die in gro?em Abstand von der Adsorbens-Oberfl?che eine kinetische Energie in Richtung senkrecht zur Oberfl?che .. > .. besitzen. Zur Desorption der Adteilchen ist eine Desorptionsenergie .. aufzuwenden, die gleich der Adsorptionsenergie .作者: Increment 時間: 2025-3-23 18:29 作者: COLON 時間: 2025-3-24 01:51 作者: 禁止 時間: 2025-3-24 04:35
http://image.papertrans.cn/r/image/831463.jpg作者: debouch 時間: 2025-3-24 06:58
https://doi.org/10.1007/978-94-011-5983-8Denudation; Geomorphology; erosion; evolution; igneous rock作者: asthma 時間: 2025-3-24 12:23 作者: 確定 時間: 2025-3-24 16:44 作者: Sinus-Rhythm 時間: 2025-3-24 22:37 作者: CYN 時間: 2025-3-24 23:52 作者: 果核 時間: 2025-3-25 04:12
Rock strength and resistance,aggregate and the nature of the bond, if any, between the mineral grains. These characteristics will also govern rock behaviour and should figure prominently in any explanation of the interplay between landform evolution and rock type. Erosional agencies attack rock in a variety of ways such as by w作者: 致詞 時間: 2025-3-25 08:12
Resistance to weathering,ical weathering (disintegration), the mechanical breakdown of rock without any contributory chemical alteration; chemical weathering (decomposition), which involves often irreversible chemical change; and biological weathering, which is effected by the growth or movement of plants and animals. Altho作者: 鋼筆尖 時間: 2025-3-25 14:07
Weathering profiles and landform development,physical and chemical properties that vary considerably from the surface downwards. These properties are major influences on slope evolution and landform development and for this reason alone it is important to understand the relationships between weathering and landscape. Weathering profiles may al作者: 使顯得不重要 時間: 2025-3-25 18:59 作者: Overdose 時間: 2025-3-25 22:58
Landforms on granitic rocks,es of many types of slopes and are good examples of the whole being greater than the sum of the invididual components. When entire landscapes are considered, additional rock properties become important. Widening the spatial context also leads to the necessity of enlarging the time dimension.作者: 身體萌芽 時間: 2025-3-26 03:16 作者: 過剩 時間: 2025-3-26 06:31
A rock-landform synthesis,articular rock types and to draw conclusions, where feasible, about the interaction of geomorphological processes and rock characteristics. Experimental and theoretical work has been incorporated whenever possible. The rock types looked at in detail have been chosen to emphasize major contrasts. Gra作者: AV-node 時間: 2025-3-26 09:07
Rock type and landform assemblages,ns of remote sensing. Also, if specific assemblages are related to rock types, direct comparisons could enable the identification to be made of the rock properties responsible for the distinctiveness. A review of landform assemblages associated with the major rock types together with a brief summary of rock characteristics are now offered.作者: Lacunar-Stroke 時間: 2025-3-26 13:55 作者: GROVE 時間: 2025-3-26 19:18
Rock strength and resistance,inently in any explanation of the interplay between landform evolution and rock type. Erosional agencies attack rock in a variety of ways such as by wear, abrasion, impact, crushing and plucking. The most important rock properties are those which reflect these processes. Rock properties can be grouped into three classes:作者: Absenteeism 時間: 2025-3-26 22:57 作者: freight 時間: 2025-3-27 04:58
Book 1988riving and resisting forces. The driving forces or processes are the methods by which energy is exerted on earth materials and include both surface, geomorphological or exogenous processes and subsurface, geological or endogenous processes. The resisting forces are the surface materials with their i作者: Hemodialysis 時間: 2025-3-27 05:31 作者: 場所 時間: 2025-3-27 11:51 作者: 窒息 時間: 2025-3-27 15:42
lled the driving and resisting forces. The driving forces or processes are the methods by which energy is exerted on earth materials and include both surface, geomorphological or exogenous processes and subsurface, geological or endogenous processes. The resisting forces are the surface materials wi作者: 幼稚 時間: 2025-3-27 18:24
General background,ace into its characteristic features. Both the nature of the forces and intensity of their operation vary in time and space and because of this the degree of interaction of the two groups of forces is also extremely variable.作者: Jargon 時間: 2025-3-27 23:10 作者: 厚臉皮 時間: 2025-3-28 04:16 作者: Magnitude 時間: 2025-3-28 09:17 作者: 笨重 時間: 2025-3-28 13:01
A. J. Gerrard Dampfphase, genannt ., so werden sie mit einer Haft-Wahrscheinlichkeit . 1 festgehalten bzw. mit der Wahrscheinlichkeit (1 — . reflektiert. Die haftenden ., genannt das ., werden entweder durch . oder . oder durch . festgehalten. Die aus diesen Kr?ften resultierende Bindungsenergie wird Adsorptions作者: 同步左右 時間: 2025-3-28 15:33
A. J. Gerrard Dampfphase, genannt ., so werden sie mit einer Haft-Wahrscheinlichkeit . 1 festgehalten bzw. mit der Wahrscheinlichkeit (1 — . reflektiert. Die haftenden ., genannt das ., werden entweder durch . oder . oder durch . festgehalten. Die aus diesen Kr?ften resultierende Bindungsenergie wird Adsorptions作者: obstinate 時間: 2025-3-28 21:03 作者: 情感脆弱 時間: 2025-3-29 01:25 作者: 發(fā)酵 時間: 2025-3-29 06:05 作者: peptic-ulcer 時間: 2025-3-29 08:15 作者: 1FAWN 時間: 2025-3-29 14:25 作者: 合唱團(tuán) 時間: 2025-3-29 19:10
YSEC Yearbook of Socio-Economic Constitutions 2021Triangulating Freedo作者: MITE 時間: 2025-3-29 20:19
978-3-031-39178-1The Editor(s) (if applicable) and The Author(s), under exclusive license to Springer Nature Switzerl
