作者: Th. E. Wong , Th. H. M. van Doorn , B. M. Schroot
DOI: 10.1007/BF01988367
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摘要: The Callovian to Ryazanian (late Middle Jurassic earliest Cretaceous; here referred as »Late Jurassic«) sediments of the Dutch Central North Sea Graben, comprising Graben and Scruff Groups, form several potential reservoirs. Source rocks are present within both these groups Carboniferous Late Triassic-Early Jurassic.