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Tessey Limestone

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Image
—Thin section showing remnant native sulfur in the <span class="search-highlight">Tessey</span> <span class="search-highlight">Limestone</span>. Sample...
Published: 01 February 1999
Figure 11 —Thin section showing remnant native sulfur in the Tessey Limestone. Sample collected in the Frenchman Hills area, northern Glass Mountains. Arrows point to the sulfur. Thin section photograph courtesy of Cyndi Mosch.
Journal Article
Journal: AAPG Bulletin
Published: 01 February 1999
AAPG Bulletin (1999) 83 (2): 277–294.
...Figure 11 —Thin section showing remnant native sulfur in the Tessey Limestone. Sample collected in the Frenchman Hills area, northern Glass Mountains. Arrows point to the sulfur. Thin section photograph courtesy of Cyndi Mosch. ...
FIGURES | View All (14)
Image
—Thin section showing calcitized anhydrite pseudomorphs in the <span class="search-highlight">Tessey</span> Limes...
Published: 01 February 1999
Figure 10 —Thin section showing calcitized anhydrite pseudomorphs in the Tessey Limestone, Bird Mountain area. Thin section photograph courtesy of Shannon Rudine.
Image
—Diagrammatic map of the Hovey channel region showing the location of all t...
Published: 01 February 1999
Figure 4 —Diagrammatic map of the Hovey channel region showing the location of all the place names in the text. Bold lines are taken from King’s (1942) map ( Figure 1 ). Limestone symbols represent Tessey Limestone outcrops, which originally were identified by King (1930) as part
Image
—(A) Matrix-free, interlocking, laminated breccia clasts of the <span class="search-highlight">Tessey</span> Lime...
Published: 01 February 1999
Figure 8 —(A) Matrix-free, interlocking, laminated breccia clasts of the Tessey Limestone, Bird Mountain (photograph courtesy of Shannon Rudine). (B) Laminated breccia textures are characteristic of the anhydrite/gypsum of the Castile Formation, such as at this Yeso Hills outcrop (photograph
Image
Monomict impact breccia from Sierra Madera. Monomict impact breccia is char...
Published: 01 January 2011
of matrix between clasts. Scale bar is in cm. (B) Monomict impact breccia within the Tessey Limestone with a large amount of matrix between clasts. Note irregular rough appearance of outcrop. Field book is 15 cm in length. (C) Photomicrograph of monomict impact breccia within the Word Formation. Plane
Journal Article
Journal: AAPG Bulletin
Published: 01 December 1950
AAPG Bulletin (1950) 34 (12): 2356–2359.
... of the Delaware basin, are outcrops of Tessey limestone of Ochoa age. The well known “top of Yates” and the top of the Gilliam member appear to be the same horizon. Above the Gilliam are ledges of limestone that closely resemble the Tansill outcrops in the foothills of the Guadalupe Mountains west of Carlsbad...
Journal Article
Journal: GSA Bulletin
Published: 01 January 2011
GSA Bulletin (2011) 123 (1-2): 371–383.
... of matrix between clasts. Scale bar is in cm. (B) Monomict impact breccia within the Tessey Limestone with a large amount of matrix between clasts. Note irregular rough appearance of outcrop. Field book is 15 cm in length. (C) Photomicrograph of monomict impact breccia within the Word Formation. Plane...
FIGURES | View All (9)
Journal Article
Journal: AAPG Bulletin
Published: 01 July 1935
AAPG Bulletin (1935) 19 (7): 1010–1022.
... and coalescing of the anhydrite stringers of the salt series at the north. Associated with this gradation, tongues of dolomite appear in the section. This change is progressive, and in the Glass Mountains the Upper Castile appears to be equivalent to the limestones and dolomites of the lower Tessey. Capitan...
FIGURES
Journal Article
Journal: AAPG Bulletin
Published: 01 August 1929
AAPG Bulletin (1929) 13 (8): 997–1031.
... dolomite into brown non-porous primary dolomite. This is also true of the Powell field. The Word carries more sandstone than the Leonard, but shows the same gradation eastward into dolomite and limestone. The Vidrio, Gilliam, and Tessey formations are predominantly limestone and dolomite...
FIGURES | View All (12)
Journal Article
Journal: AAPG Bulletin
Published: 01 April 1942
AAPG Bulletin (1942) 26 (4): 650–763b.
... in eastern Glass Mountains .—If the conclusions just outlined are correct, the beds of upper Guadalupe age in the eastern Glass Mountains are much more restricted than they were thought to be in 1931, when they were supposed to include the Vidrio, Gilliam, and Tessey limestones. The Tessey has already been...
FIGURES | View All (19)
Journal Article
Journal: AAPG Bulletin
Published: 01 November 1928
AAPG Bulletin (1928) 12 (11): 1111–1116.
... to the deposition of the Hess conglomerate along a dip valley between the Wolf Camp and Gap Tank localities. The Gaptank may have been folded into an anticline at some time subsequent to Wolfcamp deposition, either in pre-Hess, pre-Leonard, or post-Tessey time. In other words, there was probably some successive...
Journal Article
Journal: AAPG Bulletin
Published: 01 August 1929
AAPG Bulletin (1929) 13 (8): 903–906.
... the following species from both Delaware Mountain limestone and the Leonard: Fusulina elongata, Guadalupia zitteliana, Cystothalamia permiana, Cladopora spinulata, Domopora? constricta, Acanthocladia guadalupensis, Orthotetes distortus, Leptodus americanus, Richthofenia permiana, Productus meekanus...
FIGURES
Journal Article
Journal: AAPG Bulletin
Published: 01 November 1944
AAPG Bulletin (1944) 28 (11): 1596–1625.
..., clastic) deposition. Typically pontic sediments consisting of black limestones, dark shales and silts, and fine sands accumulated to a thickness exceeding 7,500 feet. The bowl-like depression in which these beds are preserved was outlined by limestone reefs built along the margins of the surrounding...
FIGURES | View All (4)
Journal Article
Journal: AAPG Bulletin
Published: 01 September 1926
AAPG Bulletin (1926) 10 (9): 877–884.
..., but neither the Gilliam nor the Tessey formation, described by Udden as overlying the Vidrio, was recognized in the area studied. Comanchean rocks .—The Comanchean consists of thin layers of marly limestone having several well-marked fossil zones and, locally, thin conglomerate beds at its base...
FIGURES
Journal Article
Journal: AAPG Bulletin
Published: 01 July 1927
AAPG Bulletin (1927) 11 (7): 721–728.
..., the Permian stratigraphic column has been subdivided into the Delaware, the Capitan, and the Carlsbad limestone. On the southwest side of the basin, in the Glass Mountains, the following subdivisions have been made, from bottom to top: Wolfcamp, Hess, Leonard, Word, Vidrio, Gilliam, and Tessey...
FIGURES
Journal Article
Journal: AAPG Bulletin
Published: 01 December 1972
AAPG Bulletin (1972) 56 (12): 2303–2322.
... tectonic activity increased and foredeeps developed and were filled with flysch material. In the Early Permian, seas spread over much of the basin region, depositing shale in the low parts of the sea floor while limestones accumulated on the higher parts. However, by Middle Permian (Leonardian) time...
FIGURES | View All (13)
Journal Article
Journal: AAPG Bulletin
Published: 01 June 1942
AAPG Bulletin (1942) 26 (6): 1007–1039.
... but older than Tessey, is called Capitan. The Capitan of the Glass Mountains grades basinward into Altuda, and lagoonward into thin-bedded Gilliam limestone. The top of the Gilliam coincides with the top of a sandstone member and is probably the same horizon as the top of the Yates. The overlying thin...
FIGURES
Journal Article
Journal: AAPG Bulletin
Published: 01 August 1929
AAPG Bulletin (1929) 13 (8): 927–944.
...K. H. Crandall ABSTRACT The relationships of the Permian formations exposed in the Guadalupe, Delaware, and Apache mountains and immediately east have for some time been the subject of much dispute. These are greatly clarified by the classification of the Capitan and Apache limestones as reef...
FIGURES | View All (6)
Journal Article
Journal: AAPG Bulletin
Published: 01 April 1942
AAPG Bulletin (1942) 26 (4): 535–649.
..., Capitan, and Gilliam formations constituting the Guadalupe series; and by the Tessey limestone, which probably belongs to the Ochoa series. Above the Tessey is the Bissett conglomerate, which is now classed as of Triassic age (although it was once thought to be Permian). This sequence is overlain...
FIGURES | View All (19)