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首页> 外文期刊>Earth Surface Processes and Landforms: The journal of the British Geomorphological Research Group >Late quaternary speleogenesis and landscape evolution in the northern Apennine evaporite areas
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Late quaternary speleogenesis and landscape evolution in the northern Apennine evaporite areas

机译:北亚苯宁蒸发区北部季度季节性生物发生和景观演变

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摘要

Gypsum beds host the majority of the caves in the north-eastern flank of the Apennines, in the Emilia Romagna region (Italy). More than six hundred of these caves have been surveyed, including the longest known epigenic gypsum cave systems in the world (Spipola-Acquafredda, similar to 11 km). Although this area has been intensively studied from a geological point of view, the age of the caves has never been investigated in detail. The rapid dissolution of gypsum and uplift history of the area have led to the long-held view that speleogenesis commenced only during the last 130 000 years. E
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