HAWK
发表于 2025-3-30 09:15:26
Evaporite Karst in Calatayud, Iberian Chain,with significant halite and glauberite units in the subsurface. Interstratal dissolution of the salt-bearing evaporites has generated megacollapse structures covering up to 12 km. in which Neogene sediments have subsided as much as 200 m. The Quaternary alluvium related to the present-day fluvial sy
哥哥喷涌而出
发表于 2025-3-30 13:35:18
The Gypsum Karst of Sorbas, Betic Chain,mprises an alternating sequence of gypsum and marly strata deposited during the Messinian salinity crisis. The development of the cave systems is closely linked to this alternation of sediments. The caves have been mainly formed by erosion of the marl units, whilst gypsum dissolution was especially
ASSET
发表于 2025-3-30 20:21:31
http://reply.papertrans.cn/59/5808/580756/580756_53.png
MAOIS
发表于 2025-3-30 23:26:37
http://reply.papertrans.cn/59/5808/580756/580756_54.png
gustation
发表于 2025-3-31 01:13:22
http://reply.papertrans.cn/59/5808/580756/580756_55.png
Transfusion
发表于 2025-3-31 07:33:35
http://reply.papertrans.cn/59/5808/580756/580756_56.png
decipher
发表于 2025-3-31 09:35:04
Block Streams in the Tremedal Massif, Central Iberian Chain, reaches 1,920 m a.s.l. at Caimodorro and has a continental climate characterised by a large number of days with minimum temperatures below freezing point (80–100 days per year). The massif displays a concordant topography controlled by nearly cylindrical folds mainly developed on quartzites and sha
蚀刻术
发表于 2025-3-31 14:48:41
http://reply.papertrans.cn/59/5808/580756/580756_58.png
Alpha-Cells
发表于 2025-3-31 20:38:29
Geology and Geomorphological Evolution of the Ebro River Delta,diment supply, global sea level, wave-induced energy and regional subsidence. Once this equilibrium is lost, the delta may start to retreat and eventually disappear. The ephemeral character of deltas is a serious threat to their lands, as well as to the economic activities developed in these areas f
Eructation
发表于 2025-3-31 23:43:03
http://reply.papertrans.cn/59/5808/580756/580756_60.png