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Triassic Stratigraphy of the Southeastern Colorado Plateau, West-Central New Mexico Spencer G New Mexico Geological Society Downloaded from: https://nmgs.nmt.edu/publications/guidebooks/72 Triassic stratigraphy of the southeastern Colorado Plateau, west-central New Mexico Spencer G. Lucas, 2021, pp. 229-240 in: Geology of the Mount Taylor area, Frey, Bonnie A.; Kelley, Shari A.; Zeigler, Kate E.; McLemore, Virginia T.; Goff, Fraser; Ulmer-Scholle, Dana S., New Mexico Geological Society 72nd Annual Fall Field Conference Guidebook, 310 p. This is one of many related papers that were included in the 2021 NMGS Fall Field Conference Guidebook. Annual NMGS Fall Field Conference Guidebooks Every fall since 1950, the New Mexico Geological Society (NMGS) has held an annual Fall Field Conference that explores some region of New Mexico (or surrounding states). Always well attended, these conferences provide a guidebook to participants. Besides detailed road logs, the guidebooks contain many well written, edited, and peer-reviewed geoscience papers. These books have set the national standard for geologic guidebooks and are an essential geologic reference for anyone working in or around New Mexico. Free Downloads NMGS has decided to make peer-reviewed papers from our Fall Field Conference guidebooks available for free download. This is in keeping with our mission of promoting interest, research, and cooperation regarding geology in New Mexico. However, guidebook sales represent a significant proportion of our operating budget. Therefore, only research papers are available for download. Road logs, mini-papers, Color Plates, maps, stratigraphic charts, and other selected content are available only in the printed guidebooks. Copyright Information Publications of the New Mexico Geological Society, printed and electronic, are protected by the copyright laws of the United States. No material from the NMGS website, or printed and electronic publications, may be reprinted or redistributed without NMGS permission. Contact us for permission to reprint portions of any of our publications. One printed copy of any materials from the NMGS website or our print and electronic publications may be made for individual use without our permission. Teachers and students may make unlimited copies for educational use. Any other use of these materials requires explicit permission. This page is intentionally left blank to maintain order of facing pages. New Mexico Geological Society Guidebook, 71st Field Conference, Geology of the Mount Taylor Area, 2021, p. 229-239. 229 TRIASSIC STRATIGRAPHY OF THE SOUTHEASTERN COLORADO PLATEAU, WEST-CENTRAL NEW MEXICO SPENCER G. LUCAS New Mexico Museum of Natural History, Albuquerque, New Mexico 87104; [email protected] ABSTRACT—Triassic strata are well exposed along the southeastern Colorado Plateau and in adjacent areas in west-central New Mexico (McKinley, Catron, Cibola and parts of Valencia and Socorro counties). The oldest Triassic strata are assigned to the Anton Chico Member of the Moenkopi Formation, which disconformably overlies Permian strata and is disconformably overlain by the Upper Triassic Chinle Group. The Moenkopi Formation in west-central New Mexico is as much as 68 m thick, and consists of mostly grayish-red and red- dish-brown sandstone, mudstone siltstone and conglomerate. Overlying Triassic strata in west-central New Mexico are assigned to seven formations of the Chinle Group (in ascending order) – the Shinarump /Zuni Mountains formations, the Bluewater Creek/San Pedro Arroyo formations, the Petrified Forest Formation (including Blue Mesa, Sonsela and Painted Desert members), the Owl Rock Formation and the Rock Point Formation – and to the Wingate Sandstone. As much as 24 m of silica-pebble conglomerate/sandstone and pedogenically-mod- ified and color-mottled siltstone, mudstone and sandstone of the Shinarump and Zuni Mountains formations, which are lateral equivalents, are at the base of the Chinle Group. The 50-60 m of Bluewater Creek Formation are dominated by red sandstones and mudstones and are laterally equivalent to the southeast to the color-mottled San Pedro Arroyo Formation. The Petrified Forest Formation is up to 441 m thick and is divided into the (ascending) Blue Mesa, Sonsela and Painted Desert members. The Blue Mesa Member is 21-45 m thick and mostly purplish and greenish bentonitic mudstone with calcrete nodules and a white tuffaceous sandstone locally present at the base. The Sonsela Member is 15-61 m thick and mostly yellowish-gray, cross-bedded sandstone and siliceous conglomerate with fossil logs. The Painted Desert Member is up to 325 m thick and is mostly reddish brown mudstone and siltstone. It includes some relatively thin, but laterally per- sistent sandstone units, the Perea and Correo beds. The Owl Rock Formation is up to 35 m thick and characterized by reddish siltstone and beds of white limestone. The Rock Point Formation is up to 70 m thick and consists of repetitively-bedded, reddish-brown sandstone and siltstone. The Wingate Sandstone is the stratigraphically-highest Triassic (?) unit in west-central New Mexico. The Moenkopi Formation is Anisian in age, whereas the Chinle Group ranges from middle Carnian to Rhaetian in age. The base of the Moenkopi Formation is a regional unconformity (Tr-0/Tr-2 unconformities), and the base of the Chinle Group is the regional Tr-3 unconformity. There are two within-Chinle regional unconformities, Tr-4 at the Sonsela base and Tr-5 (=J-0) at the Rock Point base. The Middle Jurassic Entrada Sandstone overlies Triassic strata across west-central New Mexico at the J-2 unconformity. INTRODUCTION Triassic strata in west-central New Mexico (Fig. 1) are assigned to the Moenkopi Formation and overlying Chinle Group (Fig. 2). Since Marcou (1858) first identified Trias- sic rocks in this part of the state (and in some other areas in New Mexico), a variety of lithostratigraphic relationships and names have been proposed. Triassic strata in west-central New Mexico are exposed over four outcrop belts: (1) the Triassic outcrop belt along the northern and western flanks of the Zuni Mountains, mostly between Gallup and Grants; (2) the Trias- sic outcrops located primarily on the Zuni Indian Reservation in western Cibola County and southwestern McKinley Coun- ty: (3) Triassic outcrops in the upper drainage of Largo Creek and its tributaries, far western Catron County; and (4) Triassic strata that crop out in and around the Lucero uplift of eastern Cibola, western Valencia and northwestern Socorro counties (Fig. 1). Here, I review Triassic lithostratigraphy, chronostra- tigraphy and unconformities in these four outcrop belts. SOME HISTORY Stewart et al. (1972a), Lucas and Hayden (1989) and Heck- FIGURE 1. Distribution of Triassic outcrops in New Mexico showing location of west-central New Mexico outcrops. The numbers refer to the columns in ert and Lucas (2002, 2003) provided detailed reviews of the Figure 12. 230 LUCAS ton’s (1885) Wingate Sandstones, Darton equated Dutton’s Lower Trias with Ward’s (1901) Leroux Formation, at the base of which he identified the Shinarump Conglomerate. Below his Shinarump, Darton termed the Triassic strata Moencopie (?) formation (= Moencopie beds of Ward, 1901) above Penn- sylvanian strata he considered correlative to the Aubrey Group of northern Arizona. Darton (1928) followed the then current USGS practice in abandoning Ward’s (l901) term Leroux in favor of Gregory’s (1915) name Chinle. However, Darton (1910, 1928) erred in correlating what is now known to be the Sonsela Member in west-central New Mexico with the Shinarump Conglomerate in Arizona. Consequently, he assigned underlying Upper Tri- assic strata to the Lower-Middle Triassic Moenkopi Formation. Bates (1942) first recommended abandoning Darton’s use of Moenkopi in west-central New Mexico. Thus, when Kelley and Wood (1946) mapped a Triassic stratigraphy specific to the Lucero uplift, they did not assign any strata to the Moenkopi (although some later workers did, e.g., Momper, 1957). They identified the lower, grayish-red, sand-dominated portion of the Triassic section as Shinarump Conglomerate overlain by “shale”-dominated Chinle Formation capped by a prominent sandstone at Mesa Gigante that they named the Correo Sand- stone Member of the Chinle (Fig. 3). Smith (1954, 1957), working in the Zuni uplift, followed McKee (1954), who argued that both the Moenkopi and the Shinarump are not present in west-central New Mexico. Smith thus used an informal subdivision of the Triassic strata in this area, all of which he assigned to the Chinle Formation (Fig. 3). Smith’s lower and upper Chinle members were mudrock dominated and split by the sandstone-dominated middle mem- ber. Smith also assigned to the Correo Sandstone Member the upper Chinle sandstones west of Mesa Gigante that were strati- graphically much lower in the Chinle-mudrock section. Cooley’s (1957) detailed study of Triassic stratigraphy in FIGURE 2. Generalized lithologic column of Triassic strata in west-central the drainage of the Little Colorado River was published by Ak- New Mexico. ers et al. (1958), Cooley (1958, 1959a, b) and Cooley et al. (1969). At the base of the Triassic section, Cooley tentatively identified “upper Moenkopi (?)” above Permian strata. At the development of the lithostratigraphic nomenclature of Triassic base of the overlying Chinle Formation, he identified scattered strata in west-central New Mexico, so I present only a brief re- channel-type deposits as Shinarump, and he named a lower view. Ten significant works represent turning points or synthe- member the Mesa Redondo Member. A “lower red member” ses of our understanding of Triassic stratigraphy in west-central rested on the Shinarump and was capped by the thick, mud- New Mexico (Fig. 3). rock-dominated Petrified Forest Member split by the Sonsela Marcou (1858) identified Triassic strata in west-central Sandstone Bed. According to Cooley (1957), the youngest Tri- New Mexico as “Trias” or “’New Red Sandstone.” Newber- assic rock-stratigraphic unit in west-central New Mexico, the ry (1876) applied the informal name “Salt Group” to Permian Owl Rock Member of the Chinle Formation, only extends as and Triassic strata up to and including what is now termed the far east as Thoreau.
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