Precambrian Rocks of the Northern Part of the Nacimiento Uplift, New Mexico Lee A
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New Mexico Geological Society Downloaded from: http://nmgs.nmt.edu/publications/guidebooks/28 Precambrian rocks of the northern part of the Nacimiento uplift, New Mexico Lee A. Woodward, Douglas McLelland, and J. W. Husler, 1977, pp. 93-98 in: San Juan Basin III (northwestern New Mexico), Fassett, J. F.; James, H. L.; [eds.], New Mexico Geological Society 28th Annual Fall Field Conference Guidebook, 319 p. This is one of many related papers that were included in the 1977 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. 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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 Geol. Soc. Guidebook, 28th Field Conf., San Juan Basin III, 1977 93 PRECAMBRIAN ROCKS OF THE NORTHERN PART OF THE NACIMIENTO UPLIFT, NEW MEXICO LEE A. WOODWARD, DOUGLAS McLELLAND, and JOHN W. HUSLER Department of Geology University of New Mexico Albuquerque, New Mexico INTRODUCTION hypabyssal sills and dikes or ash-flows of silicic composition The Nacimiento uplift bounds the central-eastern margin of interlayered with basalt; intense folding and metamorphism; the San Juan Basin and is the area of Precambrian exposure post-tectonic intrusion of granite about 1,720-1,780 m.y. (mil- closest to the route covered by this field conference. Precam- lion years) ago; deep erosion; deposition of Uncompahgre brian basement rocks have probably had a profound but subtle Formation (quartz sand, aluminous shale and silt); low-grade influence on the later geological development of the region; metamorphism and isoclinal folding; intrusion of quartz mon- they are potential source rocks for mineral deposits (Wood- zonite and gabbro about 1,460 m.y. ago. ward and others, 1974a; LaPoint, 1974) and have controlled A summary of the Precambrian rocks of the Tusas Moun- some Cenozoic structures (Cordell, 1976). tains was presented by Bingler (1974). He noted the occur- rence of quartzite, quartz-muscovite-biotite schist, hornblende- REGIONAL SETTING chlorite schist, leptite, granitic gneiss, quartz diorite gneiss and The principal areas having outcrops of Precambrian rocks granite porphyry. Bingler (1974, p. 111-112) reported three around the San Juan Basin are the Needle Mountains to the fold systems and described the facies developed during re- north, the Tusas Mountains to the northeast, the Nacimiento gional metamorphism. Schistosity generally trends northwest. Mountains to the east and the Zuni Mountains to the south In the Nacimiento Mountains, there are two major areas of (fig. 1). Small outcrops of Precambrian rocks in the Defiance Precambrian exposures. The northern exposures are the main uplift to the west are not discussed in this report. topic of this report and are discussed in detail below. Precam- Barker (1968) summarized the Precambrian geologic history brian rocks of the southern part of the Nacimiento Mountains of the Needle Mountains as follows: deposition of quartzose were described by Woodward and others (1974c); they polymictic conglomerate; deposition of volcanic rocks of described, from oldest to youngest, mafic xenoliths, muscovite- basaltic to intermediate compositions with minor graywacke, quartz schist, hornblendite, gneiss, quartz diorite, mafic dike quartzite, siltstone, clay and iron-formation; emplacement of rocks, granite, muscovite quartz monzonite and leucocratic dike rocks. At least two episodes of regional metamorphism occurred; the later metamorphism imparted a strong northeast- trending foliation across much of the area. Fitzsimmons (1967) reported that the Precambrian rocks in the northwestern part of the Zuni Mountains were mostly red gneissic granite with minor metarhyolite and suggested that west-northwest-trending foliation is common. A map of the southeastern Zuni Mountains by Goddard (1966) shows that the most abundant rocks are gneissic granite, metarhyolite and porphyritic aplite; other lithologic types present include bio- tite schist, quartz biotite gneiss, hornblende gneiss, quartzite, quartz monzonite gneiss, aplitic granite, porphyritic granite, gneissic aplite, hornblendite, gabbro, intrusive basalt, diorite and monzonite dikes, syenite and biotite granite. In the south- ern part of the area, the foliation mostly trends northeast; in the northern and western part, the foliation is mostly east- west, although it is locally variable. Northern Nacimiento Area Only a generalized geologic map (fig. 2) is presented here, but the reader interested in the details of the geology can consult a series of 1:24,000-scale maps published by the New Mexico Bureau of Mines and Mineral Resources (Woodward and others, 1972, 1973, 1974b, 1974c, 1976; Woodward and Timmer, 1977). This area is about 6.4 km east of Cuba, New Mexico. The mapping of the Precambrian rocks was done by PRECAMBRIAN ROCKS OF NACIMIENTO UPLIFT 95 Woodward and McLelland, and the chemical analyses were per- ism, although some may be attributed to relict primary flow. formed by Husler. After regional metamorphism the metavolcanics were locally No previous detailed work has been done on the Precam- metasomatized near the contacts with a tonalite intrusion, brian rocks of this area. A reconnaissance map by Wood and resulting in growth of oligoclase poikiloblasts. Non-metasoma- Northrop (1946) shows the generalized outcrop pattern of tized metavolcanics analyzed by the Rb-Sr method give ages of Precambrian rocks undivided. A report by Santos and others 1,800 ± 50 m.y. (Brookins, 1974). (1975, p. C5-C7) noted that the Precambrian rocks of this area are granite, granite porphyry and diorite gneiss; however, the Amphibolite map in that report shows all the Precambrian as "granitic" A few small lenses of amphibolite up to 10 m long and 1 m rock. wide are surrounded by metasedimentary rocks in the north- Most of the area covered by this report is within the San western part of the area. The amphibolite is fine grained, dark Pedro Parks Wilderness, except for a strip about a kilometer greenish gray and slightly schistose. It is composed mostly of wide along the western margin and small areas on the southern subhedral to euhedral hornblende and sodic plagioclase that is and eastern sides. altered to epidote, sericite and chlorite. Trace amounts of opaque minerals and quartz are present. ROCK UNITS These rocks appear to be derived from basic igneous dikes Fourteen Precambrian rock units were mapped in the north- and sills injected into the sedimentary rocks prior to regional ern Nacimiento Mountains. Metasedimentary and metavolcanic metamorphism. rocks appear to be the oldest; they are followed by plutonic igneous rocks ranging in composition from ultramafic to leuco- Ultramafic and Melagabbroic Rocks granite. The rocks are described in their probable chronologic A body of ultramafic and melagabbroic rocks about 0.7 km order from oldest to youngest, and their generalized distribu- across was marginally assimilated by tonalite. Near the core of tion is shown on Figure 2. the body the rock is dark gray to black; fine to medium grained; and composed of 45-50 percent hypersthene, 15-30 Metasedimentary Rocks percent labradorite, 5-10 percent hornblende, 5-10 percent Very fine grained, light-tan to medium-gray metasedimen- olivine and 5-10 percent biotite, with minor amounts of chlor- tary rocks are exposed in the northwestern part of the area ite, opaque minerals and epidote. Modally these rocks are near (fig. 2). These rocks are meta-quartz wacke, meta-arkose, the transition between melagabbro and pyroxenite. Four metaquartzite, metagraywacke and silty argillite. They range chemical analyses of rocks from this unit (table 1, nos. 1-4) from mineralogically and texturally mature rocks containing more closely resemble Nockholds' (1954) average olivine-rich 98 percent quartz