作者: NEIL H. LANDMAN , RALPH O. JOHNSON , LUCY E. EDWARDS
DOI: 10.1206/0003-0090(2004)287<0001:CFTTBI>2.0.CO;2
关键词:
摘要: Abstract Geological investigations in the upper Manasquan River Basin, central Monmouth County, New Jersey, reveal a Cretaceous/Tertiary ( = Cretaceous/Paleogene) succession consisting of approximately 2 m Tinton Formation overlain by Hornerstown Formation. The top consists very fossiliferous unit, 20 cm thick, which we refer to as Pinna Layer. It is laterally extensive and mostly glauconitic minerals some angular quartz grains. Layer truncated at Formation, nearly equal amounts siderite. base marked concentration siderite nodules containing reworked fossils. This layer also contains few fossils organisms that were living environment during time reworking. At downdip sites, there an additional (the Burrowed Unit), sandwiched between top...