OREX
发表于 2025-3-28 17:13:21
http://reply.papertrans.cn/32/3166/316558/316558_41.png
BOOM
发表于 2025-3-28 19:08:01
http://reply.papertrans.cn/32/3166/316558/316558_42.png
clarify
发表于 2025-3-29 02:54:35
http://reply.papertrans.cn/32/3166/316558/316558_43.png
大笑
发表于 2025-3-29 03:38:15
Characterization of a Paleokarstic Oil Field (Rospo Mare, Italy): Sedimentologic and Diagenetic Outcg diagenetic imprint on the actual paleokarst. The multiscale (seismic, well logs and core) sedimentologic, diagenetic and structural study of the karst features and their infillings has led to the reconstruction of this complex history and has enabled the recognition of key factors controlling rese
多嘴
发表于 2025-3-29 10:08:18
Subsurface Flow and Sulfate Dissolution Response to the Construction and Restoration of the River We the surface–subsurface water exchange and modified the natural subsurface flow field. In the sulfate-bearing hydrogeological setting, increased infiltration and intensified subsurface flow triggered related dissolution processes. Soon after construction, the structure started suffering from subside
cleaver
发表于 2025-3-29 15:26:11
Development of Sulphate Karst Under Technogenic Impact Conditions in the Western Uralsropogenic impact; this fact needs to be considered in the design, construction and operation of various constructions or technical sites. Impact of sulphate karst was studied by the example of the Kama hydroelectric power station, at the base of which gypsum rocks lie, and also in the area of the Po
Overthrow
发表于 2025-3-29 16:51:56
An Integrated Approach for Investigations of Ground-Subsidence Phenomena in the Ovaro Village (NE Itspecial emphasis on sinkholes. The study area is located in the Degano Valley, Carnian Alps, which are situated in the NE part of Italy. The main village is Ovaro and is historically affected by geohazard associated with ground-subsidence phenomena caused by evaporites, which are widely present in t
Bph773
发表于 2025-3-29 19:47:40
Investigating Physical Processes Leading to Sinkhole Occurrence in Val d’Orléans (France)er 5–15-m-thick alluvial deposits. Intense karstification within the area is caused by infiltration of large amount of Loire River water in the karst aquifer through swallow holes. Two mechanisms for the formation of sinkholes are proposed: (1) suffosion of alluvial deposits towards the karstic cond
FRAX-tool
发表于 2025-3-30 00:18:42
http://reply.papertrans.cn/32/3166/316558/316558_49.png
COKE
发表于 2025-3-30 04:24:43
http://reply.papertrans.cn/32/3166/316558/316558_50.png