Bone Spring Formation

Last updated
Bone Spring Formation
Stratigraphic range: Kungurian
Type Formation
Underlies Cutoff Shale
Thickness1,000 m (3,300 ft)
Lithology
Primary Limestone
Other Shale, sandstone
Location
Coordinates 31°51′03″N104°58′54″W / 31.8508°N 104.9817°W / 31.8508; -104.9817
Region Texas
New Mexico
Country United States
Type section
Named forBone Spring Canyon
Named byBlanchard and Davis
Year defined1929
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Bone Spring Formation (the United States)
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Bone Spring Formation (Texas)

The Bone Spring Formation is a geologic formation found in the Delaware Basin in Texas and New Mexico. It preserves fossils dating back to the Leonardian Age of the Permian Period. [1]

Contents

Description

The formation consists of dark gray deep marine limestone interbedded with shale and sandstone [1] interpreted as turbidites. [2] The total thickness is about 1,000 meters (3,300 ft). The base of the formation is largely concealed in the subsurface, and the formation is overlain by the Cutoff Shale. [1] The formation grades laterally into the Victorio Peak Formation. [3]

The uppermost shale beds of the formation have been assigned to the Avalon Shale. [4]

Fossils

The formation contains fossils of the brachiopods Productus leonardensis, Marginifera cristobalensis, Pugnoides texanus, P. bidentatus, and Composita mexicana ; the ammonites Peritrochia erebus, Paracelites elegans, Agathiceras texanum, and Perrinites . [5]

History of investigation

The formation was first designated the Bone Springs Limestone by Blanchard and Davis in 1929. [6] It has subsequently been demoted to membership as the Bone Canyon Member of the Leonard Formation, [7] renamed the Bone Spring Limestone, [8] and most recently redesigned the Bone Spring Formation. [1] The Cutoff Shale was removed as a separate formation in 1964. [9]

Economic geology

The sandstones of the Bone Spring Formation are important petroleum reservoirs with estimated reserves in 1997 of 300,000–375,000 bbl. [10] [11] The formation lies deep in the subsurface in the Delaware Basin, where its shale facies is known as the Avalon Shale. [12]

See also

Footnotes

Related Research Articles

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The Cherry Canyon Formation is a geologic formation found in the Delaware Basin of southeastern New Mexico and western Texas. It contains fossils characteristic of the Guadalupian Age of the Permian Period.

The Bell Canyon Formation is a geologic formation found in the Delaware Basin of southeastern New Mexico and western Texas. It contains fossils characteristic of the Guadalupian Age of the Permian Period.

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The Capitan Formation is a geologic formation found in western Texas and southeastern New Mexico. It is a fossilized reef dating to the Guadalupian Age of the Permian period.

The Cutoff Formation is a geologic formation in Texas and New Mexico, US. It preserves fossils dating back to the Permian period.

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<span class="mw-page-title-main">San Andres Formation, United States</span> Geologic formation in New Mexico and Texas

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<span class="mw-page-title-main">Seven Rivers Formation</span> Geologic formation in the western United States

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<span class="mw-page-title-main">Tansill Formation</span> Geologic formation in the western United States

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<span class="mw-page-title-main">Yates Formation</span> Gelogic formation in the western United States

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<span class="mw-page-title-main">Madera Group</span> Group of geologic formations in New Mexico, United States

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The Grayburg Formation is a geologic formation in west Texas and southern New Mexico. It preserves fossils dating back to the Guadalupian Epoch of the Permian Period.

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The Salado Formation is a geologic formation in west Texas and southeastern New Mexico. It was deposited in the Ochoan Stage of the Permian period.

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References