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- W196758061 abstract "Commercial gas production has been established from several Miocene conglomerates in the SW. part of the Veracruz Basin. These conglomerates, with their associated sandstones and shales, make up a zone 1,000 m thick, all of which was deposited in a bathyal environment. The conglomerates consist of recycled Upper Cretaceous limestone clasts and contain minor amounts of igneous and metamorphic rock fragments. This clastic material was derived from the west, where a very thick section of carbonate and terrigenous rocks, Jurassic to Paleocene in age, was uplifted, folded, and thrust-faulted during the Laramide orogeny. Erosion of these deformed source materials is indicated by 2 significant unconformities. One unconformity truncates sediments from Paleocene to Late Cretaceous in age; whereas, the other is at the base of the Miocene. Most of the conglomerate beds are in the lower Miocene." @default.
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- W196758061 date "1974-04-01" @default.
- W196758061 modified "2023-09-22" @default.
- W196758061 title "Influence of Laramide orogeny on tertiary conglomerate distribution, Veracruz Basin, Mexico" @default.
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