Английская Википедия:Gray Mesa Formation

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Шаблон:Infobox rockunit

The Gray Mesa Formation is a geologic formation in New Mexico. Its fossil assemblage dates the formation to the Moscovian age of the Pennsylvanian.

The formation as presently defined includes outcrops previously assigned to many local units, including the Los Moyos Formation, the Armendaris Group, and the Nakaye Formation.

Description

The formation consists mostly of cherty limestone, with a few shale, sandstone, and conglomerate beds. It is exposed in the Sandia Mountains,Шаблон:Sfn the Lucero Uplift (Шаблон:Coord),Шаблон:Sfn the western Jemez Mountains,Шаблон:Sfn and the Manzano Mountains.Шаблон:Sfn

The formation has been mapped as the Los Moyos Formation in the Manzano Mountains,Шаблон:Sfn but Spencer G. Lucas and coinvestigators have recommended abandoning the name Los Moyos Formation and using Grey Mesa Formation throughout the Madera Group.Шаблон:Sfn The Gray Mesa Formation likely correlates with the Porvenir Formation in the southeastern Sangre de Cristo Mountains.Шаблон:Sfn

The formation is underlain at most locations by the Sandia Formation, with its base typically placed at the first massive marine limestone bed above the shales of the Sandia Formation. It is overlain by the Atrasado Formation, with the contact placed at the base of a sandstone interval above the uppermost massive limestone of the Gray Mesa Formation.Шаблон:Sfn

Members

The lowermost Elephant Butte Member is about Шаблон:Convert thick and is 78% limestone, half of which contains minor amounts of chert, with indistinct medium to thick bedding. Limestone intervals are Шаблон:Convert thick and separated byh thin shale beds.

The middle Whiskey Canyon Member is about Шаблон:Convert thick and is 46% very cherty limestone and 15% slightly cherty limestone, with perhaps 35% shale. Limestone intervals are up to Шаблон:Convert thick and separated by shale beds that are Шаблон:Convert, with one larger (Шаблон:Convert) shale interval in the middle of the member.

The uppermost Garcia Member is Шаблон:Convert and is 39% non-cherty limestone, 18% cherty limestone, and 7% shale, sandstone, and conglomerate, with the rest covered. Its base is a thin sandstone on top of an eroded limestone bed. Algal limestone is abundant. Limestone intervals are Шаблон:Convert thick and separated by shale beds that are Шаблон:Convert.

Fossils

The Elephant Butte Member contains silicified fossils of the demosponge Chaetetes, brachiopods, solitary corals and fusulinids. The Whiskey Canyon Member contains crinoids, brachiopods, solitary corals, rare calcareous algae, and fusulinids. The Garcia Member contains crinoids, brachiopods, rare bryozoans, fusulinids, calcareous algae, and oncoids.

History of investigation

The unit was first designated as the Gray Mesa Member of the Madera Group by Kelley and Wood in 1946.Шаблон:Sfn

The Pennsylvanian stratigraphy of New Mexico has historically been unusually complex and inconsistent, with dozens of names for groups, formations, and members.Шаблон:SfnШаблон:Sfn Kues and Giles recommended that the name Madera Group be applied to similar exposures of shelf and marginal basin beds of Desmoinean (upper Moscovian) to early Virgilian age found from north-central and central New Mexico south along the west side of the Orogrande Basin as far as the Caballo and Robledo Mountains.Шаблон:Sfn Lucas and coinvestigators recommend discarding the name Los Moyos Formation and using Grey Mesa Formation throughout the Madera Group.Шаблон:Sfn With the Elephant Butte, Whiskey Canyon, and Garcia Formations redesignated as members of the Gray Mesa Formation, the Armendaris Group is abandoned as a synonym for the Gray Mesa Formation.Шаблон:Sfn The Nakaye Formation of the Fra Cristobal and Caballo Mountains is also abandoned as a synonym for the Gray Mesa Formation.Шаблон:Sfn

See also

Шаблон:Portal

Footnotes

Шаблон:Reflist

References

Шаблон:Chronostratigraphy of Colorado