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Mesa Redondo Member

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Journal Article
Journal: Geosphere
Published: 01 April 2016
Geosphere (2016) 12 (2): 439–463.
... deposition of the basal Shinarump and Mesa Redondo members, herein collectively called the Shinarump conglomerate, began in Late Triassic time, yet the earliest known arc magmatism is older by as much as 40 m.y. Analysis of detrital zircons from eight sites in southeastern Nevada, southern Utah...
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Summary correlation diagram of the Chinle Formation (shaded) and dinosaur-bearing formations of northwestern Argentina from (A) this study and (B) reproduced from Brusatte et al. (2010) and Langer et al. (2010). Hett.—Hettangian, MR—Mesa Redondo Member, NA—North America, OR—Owl Rock Member, RP—Rock Point Member, SA—South America.
Published: 01 November 2011
Figure 6. Summary correlation diagram of the Chinle Formation (shaded) and dinosaur-bearing formations of northwestern Argentina from (A) this study and (B) reproduced from Brusatte et al. (2010) and Langer et al. (2010) . Hett.—Hettangian, MR—Mesa Redondo Member, NA—North America, OR—Owl Rock
Image
Normalized distribution of Permian–Triassic zircon grains in the Buckskin Formation, Chinle Formation, Waterman formation, and Shinarump Conglomerate (“Chinle Fm” indicates beds exclusive of Shinarump Conglomerate and Mesa Redondo Member). Permian–Triassic data from the Cordilleran arc (Mojave Desert plutons) are provided for comparison. Ca. 275 Ma is taken as the limit of Cordilleran magmatism. Chinle Formation and Waterman formation data are from Riggs et al. (2013); Shinarump Conglomerate data are from Riggs et al. (2016); data on Cordilleran arc igneous rocks are from Barth and Wooden (2006) and Cecil et al. (2018).
Published: 30 June 2020
Figure 8. Normalized distribution of Permian–Triassic zircon grains in the Buckskin Formation, Chinle Formation, Waterman formation, and Shinarump Conglomerate (“Chinle Fm” indicates beds exclusive of Shinarump Conglomerate and Mesa Redondo Member). Permian–Triassic data from the Cordilleran arc
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Selected outcrop photographs of representative paleosols and outcrop stratal successions. The rock hammer in Parts A–G is approximately 28 cm long. A, B) Drainage Index 1 poorly drained paleosols: A) MR46 (FAC 3) of the Mesa Redondo Member with gley matrix colors (10Y) and slickensides, and B) ML 60 (FAC 58) of the Petrified Forest Member with gley matrix colors (5PB), soft iron masses (7.5YR) in the Bkg2, carbonate rhizocretions after roots in both the Bkg1 and Bkg2 (white masses), and post burial gley in A horizon. C, D, E) Drainage Index 2 intermediate drained paleosols: C) GT17 (FAC 28) of the Blue Mesa Member with gray matrix colors (10R) and soft iron masses (7.5YR) in the Bw(g), D) ML53 (FAC 51) of the Sonsela Member with gray matrix colors (5R) and post burial gley after roots in all horizons, and E) CH75 (FAC 97) of the Owl Rock Member with gray matrix colors (7.5R) and indurated carbonate reflecting a complex drainage history. F, G) Drainage Index 3 well drained paleosols: F) C39 (FAC 78) of the Petrified Forest Member with high-chroma matrix colors (7.5R) and post-burial gley after roots in all horizons, and white carbonate nodules in the Bk horizon, and G) CH68.5 (FAC 87) of the Owl Rock Member with high chroma matrix colors (10R) and strong ped structure. H, I, J) Outcrop photopanoramas annotated with the distribution of fluvial aggradational cycles (FACs): H) FAC 97 to 99 in the Owl Rock Member at the Chinde Mesa locality. The total thickness of the photographed section is approximately 40 m; I) FAC 51 to 62 in the Sonsela Member at the Mountain Lion Mesa locality. Also shown is the location of the Adamanian–Revueltian (A-R) faunal turnover. The total thickness of the photographed section is approximately 30 m; J) FAC 36 to 49 in the uppermost Blue Mesa and lower Sonsela members at the Blue Mesa locality. The total thickness of the photographed section is approximately 50 m.
Published: 01 December 2013
Fig 3.— Selected outcrop photographs of representative paleosols and outcrop stratal successions. The rock hammer in Parts A–G is approximately 28 cm long. A, B) Drainage Index 1 poorly drained paleosols: A) MR46 (FAC 3) of the Mesa Redondo Member with gley matrix colors (10Y) and slickensides
Journal Article
Journal: GSA Bulletin
Published: 01 November 2011
GSA Bulletin (2011) 123 (11-12): 2142–2159.
...Figure 6. Summary correlation diagram of the Chinle Formation (shaded) and dinosaur-bearing formations of northwestern Argentina from (A) this study and (B) reproduced from Brusatte et al. (2010) and Langer et al. (2010) . Hett.—Hettangian, MR—Mesa Redondo Member, NA—North America, OR—Owl Rock...
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Journal Article
Journal: GSA Bulletin
Published: 20 July 2020
GSA Bulletin (2021) 133 (3-4): 539–558.
... (from oldest to youngest): the Shinarump Conglomerate and Mesa Redondo Member, Blue Mesa Member, Sonsela Member, Petrified Forest Member, and Owl Rock Member ( Parker, 2006 ; Woody, 2006 ; Martz and Parker, 2010 ). Following the description by Martz et al. (2012) , all five...
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Journal Article
Journal: GSA Bulletin
Published: 01 November 2015
GSA Bulletin (2015) 127 (11-12): 1798–1815.
... Forest National Park study area, the “long Norian” Stage ( Muttoni et al., 2004 ) of the Chinle Foramtion is represented by the Mesa Redondo, Blue Mesa, Sonsela, and Petrified Forest Members. The Owl Rock Member is part of the Rhaetian Stage ( Dubiel, 1994 ; Tanner, 2003 ; Martz and Parker, 2010...
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Proposed tectonic model of the evolving Middle and Late Triassic Cordilleran magmatic arc and the response of continental backarc sequences observed in the distal basin (Chinle Formation). (A) Migration of the arc onto southwestern North America at ca. 235 Ma results in dynamic subsidence and the trapping of coarse-grained detritus adjacent to the magmatic highlands. This event likely created a flexural “back-bulge” (topographic high); lack of sediment and accompanying drop in base level resulted in an unconformity (Tr-3 unconformity). (B) Slowing subsidence likely contributed to an isostatic adjustment of the arc hinterland and a progradation of coarse-grained material to the distal basin, marked by the sheet sandstone and conglomerate bodies of the basal Shinarump Member. One such tectonic mechanism that could be responsible for the coarse-grained progradations evident in Shinarump and lower Sonsela deposits is decreased dip of the subducting slab (pictured left); however, several other possibilities exist to explain this change (see text). (C) Mudstone-dominated units of the Mesa Redondo and Blue Mesa Members reflect a return to an aggradational regime, likely the result of a phase of increased subsidence and trapping of coarser-grained clastic material near the arc. (D) Following what may have been a depositional hiatus prior to the inception of Sonsela deposition, slowing subsidence results in a coarse-grained progradation evident in the lower Sonsela Member. Basin overfilling and resultant sediment bypass are speculated to be the mechanism responsible for the creation of the persistent red silcrete. (E) Units of the upper Sonsela Member–Owl Rock Members are consistent with persisting high rates of tectonic subsidence and backarc aggradation. Box indicates generalized location of Petrified Forest National Park. All cross sections are oriented perpendicular to structural trends and the basin axis, from southwest to northeast.
Published: 01 July 2013
and lower Sonsela deposits is decreased dip of the subducting slab (pictured left); however, several other possibilities exist to explain this change (see text). (C) Mudstone-dominated units of the Mesa Redondo and Blue Mesa Members reflect a return to an aggradational regime, likely the result of a phase
Journal Article
Journal: GSA Bulletin
Published: 06 October 2023
GSA Bulletin (2024) 136 (5-6): 2305–2324.
..., extensive radioisotope geochronology within the Chinle Formation has made these strata the standard by which the Late Triassic of the western USA can be relatively dated ( Fig. 8 ). Most relevant to the Popo Agie is the establishment of precise U 238 /Pb 206 radioisotopic ages from the Mesa Redondo Member...
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Journal Article
Journal: Geosphere
Published: 30 June 2020
Geosphere (2020) 16 (4): 1042–1057.
...Figure 8. Normalized distribution of Permian–Triassic zircon grains in the Buckskin Formation, Chinle Formation, Waterman formation, and Shinarump Conglomerate (“Chinle Fm” indicates beds exclusive of Shinarump Conglomerate and Mesa Redondo Member). Permian–Triassic data from the Cordilleran arc...
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Journal Article
Journal: AAPG Bulletin
Published: 01 August 1959
AAPG Bulletin (1959) 43 (8): 2003–2007.
... previously been referred to the Santa Rosa sandstone and the Chinle formation though Dobrovolny and Summerson (1946) named a distinct sequence of beds at the top of the Chinle formation, the Redonda member of the Chinle formation. The name was taken from Redonda (also spelled Redondo) Mesa, a large mesa...
FIGURES
Journal Article
Journal: GSA Bulletin
Published: 01 July 2013
GSA Bulletin (2013) 125 (7-8): 1349–1368.
... and lower Sonsela deposits is decreased dip of the subducting slab (pictured left); however, several other possibilities exist to explain this change (see text). (C) Mudstone-dominated units of the Mesa Redondo and Blue Mesa Members reflect a return to an aggradational regime, likely the result of a phase...
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Journal Article
Published: 01 December 2013
Journal of Sedimentary Research (2013) 83 (12): 1147–1161.
...Fig 3.— Selected outcrop photographs of representative paleosols and outcrop stratal successions. The rock hammer in Parts A–G is approximately 28 cm long. A, B) Drainage Index 1 poorly drained paleosols: A) MR46 (FAC 3) of the Mesa Redondo Member with gley matrix colors (10Y) and slickensides...
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Journal Article
Journal: Geosphere
Published: 01 June 2013
Geosphere (2013) 9 (3): 614–646.
..., the Cat Mesa fault zone in the southwestern Jemez Mountains ( Fig. 3 ) offsets Permian Yeso Formation down to the east ∼240 m; but ca. 9 Ma Keres Group andesite is offset <10 m, and 1.25 Ma Tshirege Member of the Bandelier Tuff is displaced <2 m ( Kelley et al., 2003 , 2007b ). Thus, the Cat Mesa...
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Journal Article
Journal: PALAIOS
Published: 01 November 2011
PALAIOS (2011) 26 (11): 700–719.
..., in ascending stratigraphic order, the Mesa Redondo, Blue Mesa, Sonsela, Petrified Forest, and Owl Rock members within the ∼280-m-thick section exposed in PEFO and the surrounding area ( Fig. 2 ; Ash and Creber, 1992 ; Woody, 2006 ; Martz and Parker, 2010a ). FIGURE 2— Generalized stratigraphic...
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Journal Article
Journal: AAPG Bulletin
Published: 01 October 1955
AAPG Bulletin (1955) 39 (10): 2068–2077.
...., sd., and cgl. Pal eocene Salina fm. Lower Upper Negritos fm. Balcones shale (Danian) Eocene Lower Negritos shale Mesa sands Not known Petacas shale, Ancha cgl. Upper Cretaceous   * The double usage of middle and upper Oligocene is due to the miscorrelation of the Mirador...
Journal Article
Journal: GSA Bulletin
Published: 19 October 2017
GSA Bulletin (2018) 130 (5-6): 775–795.
..., 2010 ; Dubiel and Hasiotis, 2011 ; Atchley et al., 2013 ; Trendell et al., 2013a , 2013b ). The Chinle Formation at the Petrified Forest National Park can be divided into five members. The Shinarump/Mesa Redondo Member ( Fig. 2 ) represents the basal deposit overlying the Early to Middle...
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Journal Article
Journal: AAPG Bulletin
Published: 01 April 2012
AAPG Bulletin (2012) 96 (4): 679–707.
... United States ( Figure 1 ). Outcrops within the PEFO in northeastern Arizona include the upper Carnian Mesa Redondo Member through the Rhaetian Rock Point formation ( Parker, 2006 ; Woody, 2006 ; Martz and Parker, 2010 ) ( Figure 2 ). This study focuses on the lower part of the Norian Sonsela member...
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Journal Article
Journal: AAPG Bulletin
Published: 01 September 1953
AAPG Bulletin (1953) 37 (9): 2093–2118.
... section is composed of three groups lithologically similar, each consisting of a thick shale section with sand or conglomerate at the base. The oldest of these three, the Redondo group, is Senonian in age and is separated from the Muerto limestone by a major unconformity. It crops out extensively...
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Journal Article
Journal: Geosphere
Published: 01 June 2013
Geosphere (2013) 9 (3): 602–613.
... for the Chinle Formation in Petrified Forest National Park follows Woody (2006) and Martz and Parker (2010) . Exposed strata are assigned to five members; from oldest to youngest, these are the Mesa Redondo, Blue Mesa, Sonsela, Petrified Forest (previously the upper Petrified Forest), and Owl Rock Members...
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