標題: Titlebook: Geology and Water; An introduction to f Richard E. Chapman Book 1981 Martinus Nijhoff / Dr. W. Junk Publishers bv, The Hague 1981 Deformati [打印本頁] 作者: Embolism 時間: 2025-3-21 18:10
書目名稱Geology and Water影響因子(影響力)
書目名稱Geology and Water影響因子(影響力)學科排名
書目名稱Geology and Water網(wǎng)絡(luò)公開度
書目名稱Geology and Water網(wǎng)絡(luò)公開度學科排名
書目名稱Geology and Water被引頻次
書目名稱Geology and Water被引頻次學科排名
書目名稱Geology and Water年度引用
書目名稱Geology and Water年度引用學科排名
書目名稱Geology and Water讀者反饋
書目名稱Geology and Water讀者反饋學科排名
作者: 范例 時間: 2025-3-21 22:40
Pore Water and Sliding,res. On the other hand, if the block slides down a slope under the force of gravity, the previous difficulty is replaced by two others: the coefficient of friction of rock on rock suggests that an angle of about 30° would be required for gravitational sliding — and that also implies a vertical relie作者: Pseudoephedrine 時間: 2025-3-22 02:46 作者: 脫水 時間: 2025-3-22 04:52 作者: Inculcate 時間: 2025-3-22 11:28 作者: fastness 時間: 2025-3-22 15:14 作者: fastness 時間: 2025-3-22 19:16 作者: Middle-Ear 時間: 2025-3-23 00:40 作者: 彎彎曲曲 時間: 2025-3-23 04:36 作者: 表否定 時間: 2025-3-23 07:30
Role of Pore Water in Deformation of Sedimentary Basins, that important deformation occurs in sedimentary basins while they are accumulating sediment on a subsiding sedimentary column — particularly in the terminal regressive sequence. The regressive sequence itself is due to a neighbouring orogeny outside the sedimentary basin: the creation of mountains作者: Carminative 時間: 2025-3-23 12:43
Pore Water and Sliding,eology of the Alps, north-west Scotland, and Scandinavia was being unravelled, evidence emerged of lateral displacements of blocks many tens of kilometres long in the direction of movement. For example, Tornebohm (1896, p. 194) postulated movement of blocks at least 130 km long on Caledonian thrusts作者: ADAGE 時間: 2025-3-23 17:44
Native and Transplanted Kidneys,xamine, in outcrop or in hand speciment, are dry. We are apt to forget that, at depths below only a few metres from the surface, almost all rocks in nature are saturated with water (exceptionally and locally, also oil or gas). Some of this water is important to us as a source of fresh water for drin作者: 隱藏 時間: 2025-3-23 19:51 作者: aptitude 時間: 2025-3-24 02:06 作者: Crayon 時間: 2025-3-24 04:16
Dirk-Jan F. Kamann,Peter Nijkampwater, streams, and occasionally by rain-water runoff during and after storms: perennial streams are fed by ground water, smaller streams, and occasional runoff: the source is a spring or a zone of seepage, and is the highest intersection of the ground surface with the water- table. Common causes of作者: aerobic 時間: 2025-3-24 09:25 作者: 只有 時間: 2025-3-24 11:46
Marion M?hle,Dorothea M. Hartmann that important deformation occurs in sedimentary basins while they are accumulating sediment on a subsiding sedimentary column — particularly in the terminal regressive sequence. The regressive sequence itself is due to a neighbouring orogeny outside the sedimentary basin: the creation of mountains作者: 損壞 時間: 2025-3-24 18:11 作者: monologue 時間: 2025-3-24 19:26 作者: 傻瓜 時間: 2025-3-25 02:18
https://doi.org/10.1007/978-3-8349-9911-5We revert in conclusion to the central theme of this book — the movement of water in the subsurface. The principles we have developed and discussed can be applied to a range of geological problems either as qualitative or as semi-qualitative arguments. We take one of each for illustrative purposes.作者: 繁重 時間: 2025-3-25 04:54 作者: otic-capsule 時間: 2025-3-25 07:41 作者: POINT 時間: 2025-3-25 14:42 作者: Dendritic-Cells 時間: 2025-3-25 16:00 作者: expire 時間: 2025-3-25 23:41
book that sets out the fundamentals of fluid mechanics, written for geologists rather than engineers. The efforts to repair my own deficiencies in this respect led me along various unfamiliar paths, few of which were unrewarding. This book is the result of my journeys through the literature and as 作者: APRON 時間: 2025-3-26 02:30 作者: temperate 時間: 2025-3-26 07:37
Alfred Leipertz,Andreas P. Fr?bar-Stokes equation, but rather to express them in terms of the measurable and useful parameters of sedimentary rocks. Our purpose is to understand the processes rather than to develop predictive equations or formulae. Those who seek a higher goal may find the note at the end of the chapter a useful starting point作者: 誓言 時間: 2025-3-26 12:04 作者: esculent 時間: 2025-3-26 13:08
Liquid Flow through Porous Sands,r-Stokes equation, but rather to express them in terms of the measurable and useful parameters of sedimentary rocks. Our purpose is to understand the processes rather than to develop predictive equations or formulae. Those who seek a higher goal may find the note at the end of the chapter a useful starting point作者: Ostrich 時間: 2025-3-26 18:28 作者: Cocker 時間: 2025-3-27 00:13 作者: 不理會 時間: 2025-3-27 04:40 作者: 遍及 時間: 2025-3-27 08:31
R. E. Cunningham,R. J. J. Williamsl encounter water in it that will flow at the surface unless it is restrained by wellhead equipment. The pressure of the water and its density can be measured at the surface, and so the pressure head computed (if the density varies well to well, mean or unit density is taken)作者: 運氣 時間: 2025-3-27 10:22
https://doi.org/10.1007/978-3-322-81100-4hs of two or three kilometres. The distinction is also seen as a distinction between . water and what is called ., the former being derived ‘recently’ from rainfall, the latter being defined as water that was trapped in the pore spaces when the sediment accumulated作者: 潛移默化 時間: 2025-3-27 14:04 作者: 蕨類 時間: 2025-3-27 18:00
The Aquifer and Fields of Flow,l encounter water in it that will flow at the surface unless it is restrained by wellhead equipment. The pressure of the water and its density can be measured at the surface, and so the pressure head computed (if the density varies well to well, mean or unit density is taken)作者: 中國紀念碑 時間: 2025-3-28 00:45 作者: 晚間 時間: 2025-3-28 05:46
Role of Pore Water in Deformation of Sedimentary Basins, creates sediment in increasing amounts until the supply of sediment to a sedimentary basin exceeds the volume created by subsidence of the sedimentary basin. The sea then tends to become shallower, and the sediments prograde away from the orogeny.作者: 錢財 時間: 2025-3-28 07:08 作者: fiscal 時間: 2025-3-28 10:44 作者: Malleable 時間: 2025-3-28 18:02
https://doi.org/10.1007/978-94-6300-818-1series of elementary steps to fully rearrange the starting material. Before the results being presented and discussed, we will shortly introduce the reactivities accessible from allenyl esters upon gold catalysis and focus on their use in allenyne-type cycloisomerizations.
