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The AAPG/Datapages Combined Publications Database
AAPG Bulletin
Abstract
AAPG Bulletin, V.
1Manuscript received May 12, 1997; revised manuscript received
May 28, 1998; final acceptance July 19, 1998.
2Consulting Geologist, 17 El Arco Drive, Albuquerque, New
Mexico 87123; e-mail: [email protected]
ABSTRACT
(1) The upper Cathedral Mountain, Road Can yon, and Word formations
of Permian (upper Leonardian, during Road Canyon deposition, and lower
Guadalupian) age in the Glass Mountains are now considered to be shallow-marine,
fan-delta to lagoonal deposits rather than deep-water, basinal deposits.
(2) The Permian (Ochoan) Tessey Limestone in the Glass Mountains, at
least in part, is a bioepigenetic limestone that formed as a replacement
of anhydrite in the middle Tertiary. The Tessey is not a deep-water, marine,
limestone facies that demarked the position of the Hovey channel.
(3) The location of the Capitan reef in the Salt basin is unknown. One
possible interpretation of the "missing" Capitan is that it was never deposited
in the area of the Salt basin because an open channel existed there instead.
(4) Isostatic gravity anomaly maps of southeastern New Mexico and west
Texas show a "channel" entering the Delaware basin on its southwest, Salt
basin, side. This may have been the inlet to the Delaware basin in the
Late Permian; I suggest that it be called the Diablo channel.
New evidence calls for a reevaluation of the Hovey channel, Glass Mountains,
west Texas, as being the inlet for water into the Delaware basin during
the Guadalupian (Permian). The new evidence includes the following information.
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