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Finlay Limestone
From Wikipedia, the free encyclopedia
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The Finlay Limestone is a geologic formation in western Texas, southern New Mexico, and northern Chihuahua. It preserves fossils dating back to the early Cretaceous period.[1][2]
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Description
The formation is composed of massive gray limestone with a few thin beds of brown sandstone, with a total thickness of 130–426 feet (40–130 m).[1][2] It is exposed in the Finlay Mountains (31.36°N 105.60°W),[1] the Sierra de Juarez,[3] and the Cerro de Cristo Rey uplift (31.787°N 106.546°W).[2] The formation overlies the Cox Sandstone[1] and is overlain by the Del Norte Formation.[2]
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Fossils
The formation is highly fossiliferous, containing fossils characteristic of early Cretaceous Albian and Comanchean age.[2]
Economic resources
The formation includes carbonate replacement deposits of lead, zinc, and silver in northern Mexico, along the Chihuahua CRD belt.[4]
History of investigation
The formation was first defined by G.B. Richardson in 1904 and assigned to the Fredericksburg Group.[1]
See also
Footnotes
References
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