Holocene Depositional History of the Southern New Jersey Barrier and Backbarrier Regions
Holocene Depositional History of the Southern New Jersey Barrier and Backbarrier Regions
复制标题
新泽西州南部屏障和后屏障区域的全新世沉积史
DOI：
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发表时间：
1990
期刊：
影响因子：
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通讯作者：
M. Ferland
中科院分区：
文献类型：
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作者：
M. Ferland
翻译后摘要：地下地层的backbarrier南部新泽西地区进行了检查，以确定全新世沉积历史。研究区域从布里甘廷延伸到五月角，包括七个屏障岛和一个广泛的后屏障区。振动器，钻芯，表面样品，历史地图和图表，和放射性碳年代被用来记录沉积模式。全新世障壁后地层的特征是由底部沼泽或泻湖组成的向上变细层序，上覆砂相、潮坪、沼泽、潮汐通道和浅泻湖。这些数据反映了从较高到较低的能量backbarrier条件的变化，导致整个全新世海侵的屏障岛屿向陆地迁移。地层学，地质学，障壁，新泽西，沉积作用，表面，地貌学，障壁岛，沿海地区，水道。
Abstract : The subsurface stratigraphy of the backbarrier region of southern New Jersey was examined to determine the Holocene depositional history. The study area extends from Brigantine to Cape May and includes seven barrier islands and an extensive backbarrier region. Vibracores, augercores, surface samples, historical maps and charts, and radio-carbon dates were used to document the patterns of sedimentation. The Holocene backbarrier stratigraphy is characterized by a fining upward sequence that consists of a basal marsh or lagoon, overlain by a sand facies, tidal flats, marshes, tidal channels, and shallow lagoons. These data reflect a change from higher to lower energy backbarrier conditions that resulted as the barrier islands migrated landward throughout the Holocene transgression. Stratigraphy, Geology, Barriers, New Jersey, Sedimentation, Surfaces, Geomorphology, Barrier island, Coastal regions, Waterways.