Titlebook: Glaciotectonic Landforms and Structures; James S. Aber,David G. Croot,Mark M. Fenton Book 1989 Springer Science+Business Media Dordrecht 1

分期

書(shū)目名稱(chēng)Glaciotectonic Landforms and Structures影響因子(影響力)




書(shū)目名稱(chēng)Glaciotectonic Landforms and Structures影響因子(影響力)學(xué)科排名




書(shū)目名稱(chēng)Glaciotectonic Landforms and Structures網(wǎng)絡(luò)公開(kāi)度




書(shū)目名稱(chēng)Glaciotectonic Landforms and Structures網(wǎng)絡(luò)公開(kāi)度學(xué)科排名




書(shū)目名稱(chēng)Glaciotectonic Landforms and Structures被引頻次




書(shū)目名稱(chēng)Glaciotectonic Landforms and Structures被引頻次學(xué)科排名




書(shū)目名稱(chēng)Glaciotectonic Landforms and Structures年度引用




書(shū)目名稱(chēng)Glaciotectonic Landforms and Structures年度引用學(xué)科排名




書(shū)目名稱(chēng)Glaciotectonic Landforms and Structures讀者反饋




書(shū)目名稱(chēng)Glaciotectonic Landforms and Structures讀者反饋學(xué)科排名

脫毛

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.

Range-Of-Motion

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.

Dysplasia

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.

舞蹈編排

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.

finite

finite

貪心

judiciousness

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.

有幫助

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.