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新泽西横断面开始于新泽西沿海平原,终结于下部陆基。人们认为,它是研究北美被动大陆边缘地层学和沉积史的一种手段。现有有关海岸平原、陆架和上部陆坡的大量地质和地球物理成果是研究横断面岸侧部分的雄厚的
New Jersey cross-section begins in the New Jersey coastal plains, ending in the lower land-based. It is believed that it is a means of studying the history of the North American passive continental margin stratigraphy and sedimentation. The extensive geological and geophysical achievements of the existing coastal plains, shelf and upper slopes are strong