insipid
发表于 2025-3-25 03:36:38
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).
Archipelago
发表于 2025-3-25 10:04:55
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.
BIPED
发表于 2025-3-25 14:06:37
978-94-015-6843-2Springer Science+Business Media Dordrecht 1989
赞成你
发表于 2025-3-25 18:52:06
http://reply.papertrans.cn/39/3859/385823/385823_24.png
噱头
发表于 2025-3-25 20:13:28
http://reply.papertrans.cn/39/3859/385823/385823_25.png
提升
发表于 2025-3-26 02:16:16
http://reply.papertrans.cn/39/3859/385823/385823_26.png
顶点
发表于 2025-3-26 08:01:49
http://reply.papertrans.cn/39/3859/385823/385823_27.png
vanquish
发表于 2025-3-26 09:42:27
http://reply.papertrans.cn/39/3859/385823/385823_28.png
ordain
发表于 2025-3-26 15:20:44
https://doi.org/10.1007/978-981-15-8143-4idges as, ‘a 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
分开
发表于 2025-3-26 18:25:33
http://reply.papertrans.cn/39/3859/385823/385823_30.png