標(biāo)題: Titlebook: Glaciotectonic Landforms and Structures; James S. Aber,David G. Croot,Mark M. Fenton Book 1989 Springer Science+Business Media Dordrecht 1 [打印本頁(yè)] 作者: 分期 時(shí)間: 2025-3-21 17:44
書(shū)目名稱Glaciotectonic Landforms and Structures影響因子(影響力)
書(shū)目名稱Glaciotectonic Landforms and Structures影響因子(影響力)學(xué)科排名
書(shū)目名稱Glaciotectonic Landforms and Structures網(wǎng)絡(luò)公開(kāi)度
書(shū)目名稱Glaciotectonic Landforms and Structures網(wǎng)絡(luò)公開(kāi)度學(xué)科排名
書(shū)目名稱Glaciotectonic Landforms and Structures被引頻次
書(shū)目名稱Glaciotectonic Landforms and Structures被引頻次學(xué)科排名
書(shū)目名稱Glaciotectonic Landforms and Structures年度引用
書(shū)目名稱Glaciotectonic Landforms and Structures年度引用學(xué)科排名
書(shū)目名稱Glaciotectonic Landforms and Structures讀者反饋
書(shū)目名稱Glaciotectonic Landforms and Structures讀者反饋學(xué)科排名
作者: 脫毛 時(shí)間: 2025-3-21 23:22
Megablocks and Rafts,ft giving little or no morphologic clue to their presence in the subsurface. They may, in fact, easily be mistaken for bedrock, if deep exposures or drilling logs are not available. In other cases, the megablocks form flat-topped buttes, small plateaus, or irregular hills, which have also been mistaken for bedrock outliers.作者: Range-Of-Motion 時(shí)間: 2025-3-22 01:53
Applied Glaciotectonics,, (2) reduction of sediment or rock strength, and (3) major increase in sediment variability. Activities, for which recognition of glacially thrust terrain is important, include mine planning and operation, drift prospecting and mineral exploration, construction, and soils mapping and utilization.作者: Dysplasia 時(shí)間: 2025-3-22 04:51
Distribution of Glaciotectonic Phenomena,laciotectonic features became increasingly common beginning in the 1950s, leading Sauer (1978) to conclude that such features are probably widespread phenomena in the outer portions of glaciated regions.作者: 舞蹈編排 時(shí)間: 2025-3-22 10:23
Glaciotectonic Analogs, one kind of mass whose distribution and resulting crustal load may increase through time. Local increase of crustal loading may come about in many other non-glacial situations: growth of an alluvial fan or a delta, buildup of volcanic deposits, landslide or mass movement of material, and convergence of lithospheric plates.作者: finite 時(shí)間: 2025-3-22 13:58 作者: finite 時(shí)間: 2025-3-22 19:51 作者: 貪心 時(shí)間: 2025-3-22 23:32 作者: judiciousness 時(shí)間: 2025-3-23 02:12
Yudit Namer,Canan Co?kan,Oliver Razumlaciotectonic features became increasingly common beginning in the 1950s, leading Sauer (1978) to conclude that such features are probably widespread phenomena in the outer portions of glaciated regions.作者: 有幫助 時(shí)間: 2025-3-23 09:05
Changing Directions in Healthcare one kind of mass whose distribution and resulting crustal load may increase through time. Local increase of crustal loading may come about in many other non-glacial situations: growth of an alluvial fan or a delta, buildup of volcanic deposits, landslide or mass movement of material, and convergence of lithospheric plates.作者: PATRI 時(shí)間: 2025-3-23 10:45
Sana Loue,Jaroslaw Richard Romaniuk only be explained as the results of former glaciation. Glacial theory has from the beginning, thus, rested on two groups of geological field evidence: (1) features formed by glacial erosion and (2) features created by glacial deposition.作者: 漫步 時(shí)間: 2025-3-23 15:06 作者: 分解 時(shí)間: 2025-3-23 22:06 作者: thrombosis 時(shí)間: 2025-3-24 01:07
https://doi.org/10.1007/978-3-658-42348-3ge composite-ridges. Small composite-ridges are also found in similar topographic settings, such as escarpments, islands, or valley sides. A source depression is located a short distance upglacier in some cases. Finally, both large and small composite-ridges are usually associated with ice margins marking glacier stillstands or readvances.作者: cartilage 時(shí)間: 2025-3-24 03:11
https://doi.org/10.1007/978-94-009-6693-2l ridged morphology. Bluemle and Clayton (1984) placed such hills from North Dakota into the category of ., that Clayton .. (1980:46) defined as ‘a(chǎn)n irregular jumble of hills with no obvious transverse ridges and no obvious source depression.’作者: ZEST 時(shí)間: 2025-3-24 10:16
https://doi.org/10.1007/978-1-349-09486-8e from only a few cm to > 100 m (fig. 1-4) and may have vertical dimensions of several lOs of m. Intrusive structures rarely give rise to distinctive or noticeable landforms, but they may dominate the subsurface character of a glacial sequence (fig. 7-1).作者: palliative-care 時(shí)間: 2025-3-24 11:24
Monitoring and Evaluating Health Policy,under the center of a thick ice sheet. Deformations may arise during advancing, maximal, or recessional phases of glaciation. All manner of material from well-consolidated bedrock to loose Quaternary sediment in both frozen and thawed conditions may be affected.作者: 河流 時(shí)間: 2025-3-24 18:29
Hill-Hole Pair,n and ice-shoved hill. Other types of glaciotectonic landforms are variations of the hill-hole theme. The association of individual ice-shoved hills with discrete source depressions was first described by Jessen (1931) from northern Jylland, Denmark.作者: allergen 時(shí)間: 2025-3-24 23:00 作者: Abjure 時(shí)間: 2025-3-25 01:58 作者: insipid 時(shí)間: 2025-3-25 03:36
Diapirs, Intrusions and Wedges,e from only a few cm to > 100 m (fig. 1-4) and may have vertical dimensions of several lOs of m. Intrusive structures rarely give rise to distinctive or noticeable landforms, but they may dominate the subsurface character of a glacial sequence (fig. 7-1).作者: Archipelago 時(shí)間: 2025-3-25 10:04
Dynamism of Glaciotectonic Deformation,under the center of a thick ice sheet. Deformations may arise during advancing, maximal, or recessional phases of glaciation. All manner of material from well-consolidated bedrock to loose Quaternary sediment in both frozen and thawed conditions may be affected.作者: BIPED 時(shí)間: 2025-3-25 14:06
978-94-015-6843-2Springer Science+Business Media Dordrecht 1989作者: 贊成你 時(shí)間: 2025-3-25 18:52 作者: 噱頭 時(shí)間: 2025-3-25 20:13 作者: 提升 時(shí)間: 2025-3-26 02:16 作者: 頂點(diǎn) 時(shí)間: 2025-3-26 08:01 作者: vanquish 時(shí)間: 2025-3-26 09:42 作者: ordain 時(shí)間: 2025-3-26 15:20
https://doi.org/10.1007/978-981-15-8143-4idges as, ‘a(chǎn) composite of great slices of up-thrust and commonly contorted sedimentary bedrock that is generally interlayered with and overlain by much glacial drift.’ The term . (= transverse-ridges of Clayton .. 1980) is used here for such ice-shoved ridges. Composite-ridges that include a substan作者: 分開(kāi) 時(shí)間: 2025-3-26 18:25 作者: 過(guò)份 時(shí)間: 2025-3-27 00:56
https://doi.org/10.1007/978-94-009-6693-2l ridged morphology. Bluemle and Clayton (1984) placed such hills from North Dakota into the category of ., that Clayton .. (1980:46) defined as ‘a(chǎn)n irregular jumble of hills with no obvious transverse ridges and no obvious source depression.’作者: 行為 時(shí)間: 2025-3-27 02:18
https://doi.org/10.1007/978-3-319-17963-6auer 1978; Ruszczyńska-Szenajch 1987). These megablocks are more-or-less horizontal, slightly deformed, and are often buried under or within thick drift giving little or no morphologic clue to their presence in the subsurface. They may, in fact, easily be mistaken for bedrock, if deep exposures or d作者: Narcissist 時(shí)間: 2025-3-27 07:33 作者: committed 時(shí)間: 2025-3-27 12:39
https://doi.org/10.1007/978-3-319-55865-3tant for many human activities. The principal deleterious results of glaciotectonism are: (1) disruption and deformation of the stratigraphic sequence, (2) reduction of sediment or rock strength, and (3) major increase in sediment variability. Activities, for which recognition of glacially thrust te作者: LAVE 時(shí)間: 2025-3-27 15:59
Yudit Namer,Canan Co?kan,Oliver Razumfor a long time, because the documented examples of glaciotectonic landforms and structures were few and far between. Recognition and description of glaciotectonic features became increasingly common beginning in the 1950s, leading Sauer (1978) to conclude that such features are probably widespread 作者: 運(yùn)氣 時(shí)間: 2025-3-27 20:49 作者: Anterior 時(shí)間: 2025-3-28 01:36
Changing Directions in Healthcaresing load on weak substratum material, the conditions for deformation may develop both in front of the mass as well as beneath it. Glacier ice is only one kind of mass whose distribution and resulting crustal load may increase through time. Local increase of crustal loading may come about in many ot作者: 善于騙人 時(shí)間: 2025-3-28 05:00 作者: bronchiole 時(shí)間: 2025-3-28 09:20
Hill-Hole Pair,n and ice-shoved hill. Other types of glaciotectonic landforms are variations of the hill-hole theme. The association of individual ice-shoved hills with discrete source depressions was first described by Jessen (1931) from northern Jylland, Denmark.作者: 解凍 時(shí)間: 2025-3-28 13:51
Large Composite-Ridges,idges as, ‘a(chǎn) composite of great slices of up-thrust and commonly contorted sedimentary bedrock that is generally interlayered with and overlain by much glacial drift.’ The term . (= transverse-ridges of Clayton .. 1980) is used here for such ice-shoved ridges. Composite-ridges that include a substan作者: 比賽用背帶 時(shí)間: 2025-3-28 18:16
Small Composite-Ridges,ge composite-ridges. Small composite-ridges are also found in similar topographic settings, such as escarpments, islands, or valley sides. A source depression is located a short distance upglacier in some cases. Finally, both large and small composite-ridges are usually associated with ice margins m作者: cluster 時(shí)間: 2025-3-28 20:44 作者: 反抗者 時(shí)間: 2025-3-29 02:57 作者: 制定 時(shí)間: 2025-3-29 04:12
Diapirs, Intrusions and Wedges,e from only a few cm to > 100 m (fig. 1-4) and may have vertical dimensions of several lOs of m. Intrusive structures rarely give rise to distinctive or noticeable landforms, but they may dominate the subsurface character of a glacial sequence (fig. 7-1).作者: Budget 時(shí)間: 2025-3-29 08:29 作者: TAG 時(shí)間: 2025-3-29 11:24 作者: 疏遠(yuǎn)天際 時(shí)間: 2025-3-29 19:03
