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- W118401302 abstract "Publisher Summary This chapter begins with the structure, tectonics, and sedimentation of crustal fissure systems. It then presents a case study of a crustal fissure system, focusing on the structure, morphology, and early history of the Red Sea. The chapter then proceeds to describe the structure and history of the Gulf of California. The crustal fissure stage, or proto-oceanic trough, or young ocean stage, is characterized by the production of oceanic crust, which separates two passive continental margins, as a result of advanced lithosphere thinning and magmatic activity. Because of important tectonic and thermal subsidence at this stage, the structure is generally below sea level. The crustal fissure stage is not commonly observed in modern oceans, with the exceptions of the Red Sea and the Gulf of California. However, crustal fissure structures and sediments are incorporated in passive continental margins, where they are deeply buried below continental shelves. The morphology of crustal fissures is very close to those of the rifts, and the rift shoulders persist on both sides of the structure. The mechanisms responsible for crustal thinning decrease in importance but continue, and the laws of tectonic and thermal subsidence apply." @default.
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- W118401302 date "2008-01-01" @default.
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- W118401302 title "Chapter Five Crustal Fissure Systems" @default.
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- W118401302 doi "https://doi.org/10.1016/s1572-5480(08)00205-4" @default.
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