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Salado River basin

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Journal Article
Journal: PALAIOS
Published: 01 April 2015
PALAIOS (2015) 30 (4): 248–257.
... is located in the lower basin of the river, including several outcrops (upper Pleistocene–upper Holocene) over a distance of approximately 35 km from the river mouth, exhibiting a gradient from estuarine to freshwater conditions. Thus, the Salado River study area provides sufficient data to analyze temporal...
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Journal Article
Journal: AAPG Bulletin
Published: 01 October 1939
AAPG Bulletin (1939) 23 (10): 1569–1572.
.... The upper, or Salado formation, occupies not only the eastern portion of the Delaware basin but spreads northward and eastward above and beyond the basin rim, which is formed by the Capitan reef. This upper formation, which is absent in most of the western half of the basin, is apparently exposed nowhere...
Journal Article
Journal: GSA Bulletin
Published: 01 July 2011
GSA Bulletin (2011) 123 (7-8): 1513–1523.
... reflecting Permian meteoric water, while other cycles may show evaporated Permian seawater. Exposure surfaces are more prominent in the upper part of Salado Formation depositional cycles due to basin desiccation, as indicated by cracks and dish-shaped laminae. Clays were concentrated on many exposure...
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... Throughout most of late Permian time the southeastern Permian Basin was part of a shallow barred lagoon located in an area of high evaporation and low rainfall. Refluxion to the open sea farther west was slowed by the intervening Capitan barrier reef during Guadalupian time, but free surface...
Series: Geological Society, London, Special Publications
Published: 01 January 2005
DOI: 10.1144/GSL.SP.2005.252.01.09
EISBN: 9781862395008
... 1991 ; Wignall & Hallam 1991 ; Wignall 1994 ). Field work was carried out in the central part of the Mendoza Shelf, along the Salado river valley (35°12′S and 69°46′W), where the Tithonian–Valanginian succession (170 m) is part of a large anticlinal structure oriented N–S and accompanied...
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Journal Article
Published: 01 January 1997
Journal of Sedimentary Research (1997) 67 (1): 225–234.
... from the Tubb (Leonardian), San Andres Unit (lower Guadalupian), upper Seven Rivers (upper Guadalupian), and Salado-Tansill (Guadalupian-Ochoan) Formations to determine the times of mineral genesis. Rb-Sr isotopic data, for aliquots of a clay sample that has been leached by diverse ion exchange...
Journal Article
Journal: AAPG Bulletin
Published: 01 September 1937
AAPG Bulletin (1937) 21 (9): 1193–1205.
... to exist. Richardson and Wells 7 have shown that most of the minerals which occur in the Salado when dissolved in water absorb heat. The low gradient in the Permian Basin is a regional effect. If solution of parts of the Salado is the cause of this effect it must also be regional in extent...
FIGURES
Journal Article
Journal: AAPG Bulletin
Published: 01 February 1991
AAPG Bulletin (1991) 75 (2): 219–240.
.... The passive margin phase is represented by a thick sequence of Tertiary sediments that postdate rift-related tectonism and correspond to sedimentation along the margin of the newly opened South Atlantic Ocean. The Punta del Este part of the greater Salado basin is relatively unexplored with only two wells...
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Journal Article
Journal: PALAIOS
Published: 01 March 2014
PALAIOS (2014) 29 (3): 101–120.
... collected from an exceptional concentration at the El Salado locality were probably buried shortly after death. e-mail: leticialuci@gl.fcen.uba.ar 25 6 2013 13 2 2014 Copyright © 2014, SEPM (Society for Sedimentary Geology) 2014 Ancient nautiloid and ammonoid shells...
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Journal Article
Journal: GSA Bulletin
Published: 01 November 2010
GSA Bulletin (2010) 122 (11-12): 1989–2004.
... in the Delaware Basin varies as a result of syndepositional subsidence in localized depositional centers. The Rustler Formation conformably overlies the Salado Formation and is characterized by a variable lithology consisting of interbedded sulfate, carbonate, clastic, and halite rocks. The Rustler Formation...
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Series: Geological Society, London, Special Publications
Published: 01 January 2013
DOI: 10.1144/SP369.22
EISBN: 9781862396173
... Fig. 6. Gravity model of the regional seismic profile along the Pelotas Basin, with sedimentary, crustal and densities. The continental domain is characterized by a narrow rift in the platform. The transitional domain is characterized by a rather thick crust possibly intruded by igneous rocks...
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Journal Article
Journal: AAPG Bulletin
Published: 01 February 1942
AAPG Bulletin (1942) 26 (2): 217–255.
... reference to the West Texas Permian basin. To this end seven paleogeographic maps are presented, drawn on the following horizons: latest Pennsylvanian (Thrifty), Wolfcamp (Coleman Junction), lower Leonard (Choza), San Andres (Blaine), middle Guadalupe (Grayburg), Castile and Salado, and Rustler...
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Journal Article
Journal: AAPG Bulletin
Published: 01 January 1972
AAPG Bulletin (1972) 56 (1): 26–37.
...-seven exploratory and production holes have been drilled to date by the operator. The mine is on the crest of a local culmination on a regional anticline at the Delaware basin edge of the Central Basin platform. The sulfur is produced from a porous limestone facies in the predominantly evaporitic Salado...
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Journal Article
Journal: AAPG Bulletin
Published: 01 November 1963
AAPG Bulletin (1963) 47 (11): 1952–1962.
.... Evenly bedded fine-grained red sandstone and shale beds that are 675 feet thick and contain a 10-foot basal conglomerate lie on the San Andres and are divided in ascending order into the Grayburg, Queen, Seven Rivers, Yates, Tansill, Salado, Rustler, and Dewey Lake Formations. These formations...
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Journal Article
Journal: AAPG Bulletin
Published: 01 December 1960
AAPG Bulletin (1960) 44 (12): 1903–1911.
... on aerial photographs, especially in the Pecos River valley from about the latitude of Malaga south at least as far as the New Mexico-Texas boundary. Reconnaissance in the area near Malaga confirmed that some of these features are domes similar to the four in the Clayton Basin Quadrangle. Many examples...
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Journal Article
Journal: Geology
Published: 01 March 2009
Geology (2009) 37 (3): 231–234.
... magma body at a rate of ~2.5 mm/yr. However, we find no clear evidence for volcanic uplift after an examination of three rivers (Rio Salado, Rio Puerco, Rio Grande), and two terraces (Llano de Manzano, Llano de Albuquerque) crossing the Socorro magma body. Our geomorphic measurements permit at most 25...
FIGURES
Journal Article
Journal: AAPG Bulletin
Published: 01 April 1941
AAPG Bulletin (1941) 25 (4): 593–629.
... is composed of brown, earthy, dolomitic anhydrite. In southern Upton and in Pecos counties the member is also considerably dolomitic. In general, it may be stated that the bed is encountered from 150 to 200 feet above the base of the Salado formation in all wells drilled on the Central Basin platform...
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Journal Article
Journal: GSA Bulletin
Published: 04 November 2019
GSA Bulletin (2019)
... (nahcolite + halite) preserved in a restricted area of the Eocene Green River Formation in the Piceance Creek Basin of Colorado, USA. Nahcolite solubility is dependent on partial pressure of carbon dioxide ( p CO 2 ) as well as temperature (T), so these models covary with both T and p CO 2 . In the lake...
Journal Article
Journal: Geosphere
Published: 01 February 2017
Geosphere (2017) 13 (1): 49–81.
... climate at ca. 6 Ma and ca. 2 Ma. CORRESPONDENCE: kek1@unm.edu 14 12 2015 10 08 2016 04 11 2016 © 2016 Geological Society of America 2016 Little Colorado River (LCR) is one of the largest drainage basin area tributaries to Colorado River (CR). As shown in Figure 1...
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Journal Article
Journal: AAPG Bulletin
Published: 01 September 1941
AAPG Bulletin (1941) 25 (9): 1713–1728.
... basinward than the next older, before beginning its plunge into the Delaware basin. The result is the basinward thickening of almost every member. 4 Salado is used herein instead of the “Upper Castile” of older nomenclature. See Ronald K. DeFord and E. Russell Lloyd, “West Texas-New Mexico Symposium...
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