坎帕尼亚地区(意大利南第勒尼安海)的海洋地质图:对不同规模地质调查的考虑和贡献

G. Aiello
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引用次数: 2

摘要

在意大利国家地质调查局资助的研究项目框架内,坎帕尼亚地区的海洋地质图以1:25.000和1:10.000的比例绘制,特别关注那不勒斯湾(南第勒尼安海),这是一个复杂的火山地区,火山和沉积过程在晚第四纪和Cilento海岬强烈相互作用。本文以第464号“Isola di Ischia”和第502号“Agropoli”地质薄片为例进行了研究。在实现地震剖面解释的基础上,将地质图与研究区地震地层背景进行了整合,为研究区地下地质背景提供了有趣的数据。本文详细研究了伊斯基亚和阿格罗斯波利海域的海岸地质沉积。已绘制的地质单元表示为:i)声基的岩石单元(火山和/或沉积),ii)沿海环境的沉积物,包括淹没海滩的沉积物和海岸悬崖尖的沉积物,iii)内陆架环境的沉积物,包括内陆架沉积物和生物碎屑沉积物,iv)外陆架环境的沉积物,包括碎屑沉积物和生物碎屑沉积物,v)低地体系域,vi)更新世的海洋残体单元,7)不同的火山单元,年龄为更新世。地震地层资料与地质图提供的沉积学和环境资料相结合,使我们对该地区晚第四纪的地质演化有了新的认识。
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Marine geological maps of the Campania Region (Southern Tyrrhenian sea, Italy): considerations and contributions to a different scale of geological survey
Marine geological maps of the Campania region have been constructed both to 1:25.000 and to a 1:10.000 scales in the frame of research projects financed by the Italian National Geological Survey, focusing, in particular, on the Gulf of Naples (Southern Tyrrhenian sea), a complex volcanic area where volcanic and sedimentary processes strongly interacted during the Late Quaternary and on the Cilento Promontory offshore. In this paper the examples of the geological sheets n. 464 “Isola di Ischia” and n. 502 “Agropoli” have been studied. The integration of the geological maps with the seismo-stratigraphic setting of the study areas has also been performed based on the realization of interpreted seismic profiles, providing interesting data on the geological setting of the subsurface. The coastal geological sedimentation has been studied in detail in the Ischia and Agropoli offshore. The mapped geological units are represented by: i) the rocky units of the acoustic basement (volcanic and/or sedimentary), ii) the deposits of the littoral environment, including the deposits of submerged beach and the deposits of toe of coastal cliff, iii) the deposits of the inner shelf environment, including the inner shelf deposits and the bioclastic deposits, iv) the deposits of the outer shelf environment, including the clastic deposits and the bioclastic deposits, v) the Lowstand System Tract, vi) the Pleistocene relict marine units, vii) different volcanic units, Pleistocene in age. The seismo-stratigraphic data, coupled with the sedimentological and environmental data provided by the geological maps, allow to give new insights on the geologic evolution of this area during the Late Quaternary. 
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