Transcript Group6_2012
Stratigraphy San Ysidro Anticline and Syncline Jemez Mountains Valle Caldera San Ysidro An eroded anticline and syncline make up the major geology near this little town with late Triassic to early Cretaceous sedimentary rocks exposed in the folds. Late Triassic – Mid Jurassic Units The core of the anticline contains the Painted Desert Member of the Petrified Forest Formation (Chinle Group). A red to green siltstone and mudstone deposited on the floodplain of a large northwest flowing river system about 205 – 210 Ma. The Middle Jurassic Todilto formation lies directly on the Chinle group in this area. View toward the north of the east limb of the anticline. TRcpd is the Triassic Painted Desert member of the Petrified Forest Formation (Chinle Group) and Jt is the Jurassic Todilto Formation. The mountains on the skyline are the Sierra Nacimient o. Photograph taken by Richard Kelley. The Todilto Formation was deposited in a salina about 159Ma during the . Jurassic ocean, and is composed of two units; •Mesa Luciano Member – a basal laminated shale and limestone •Tonque Arroyo Member – an upper gypsum deposit The Summerville Formation lies above the Todilto and was deposited on an arid coastal plain •Summerville Formation – a maroon mudstone and pinkish-tan, poorly cemented sandstone. The Morrison Formation has two units exposed in this area; •Salt Wash Member - this is a river channel sandstone making up the basal unit of the Morrison. It has distinctive gold colored cross-bedded sandstone and red to green silt stone. The sandstone contains a good amount of concretions and form the westdipping beds on the eastern flank in the anticline. •Brushy Basin Member – interbedded salmon pink to a pistachio green siltstone with thin river channel sandstone. This formation has preserved dinosaur bones and highly polished gastroliths. Radiometric dating of ash beds contained in the Brushy Basin in Utah and Colorado place the age of this member at 148 – 150 Ma ( Kowallis, 1998) View of the east limb of the anticline, looking north toward the Sierra Nacimiento. Js is Jurassic Summerville Formation, Jms is the Salt Wash Member of the Jurassic Morrison Formation, and Jmb is the Brushy Basin Member of the Morrison Formation. Photograph by Richard Kelley The top of the Morrison formation is composed of the Jackpile Sandstone. •Jackpile Sandstone Member – River deposit. East limb of the anticline exposing the Brushy Basin Member and the Jackpile Member of the Morrison Formation (Jmb and Jmj) and the basal unit of the Dakota Formation (Kd). Photograph by Richard Kelley. Cretaceous Units The Cretaceous units exposed here are coastal plain, shoreline and marine deposits from along the western area of the Western Interior Seaway about 93 – 125 Ma yrs ago. •Dakota Formations - base is distinguished by the chert and quartzite pebble conglomerate that was deposited on and irregular surface. This formation is composed of six units in this area, five of which are in continuous sequence. The top unit is separated by a tongue of the Mancos Shale. •Encinal Canyon Sandstone – the basal unit, a thin bedded, cross-bedded, gold colored sandstone interbedded with carbonaceous beds and black shale. •Oak Canyon Member – a shale containing plant material fossils interbedded with thin bioturbated sandstone beds. The sandstones are cross-bedded locally and intensely burrowed. •Cubero Sandstone – gold colored, bioturbated sandstone •Clay Mesa Member – black marine shale •Paguate Sandstone – orange – yellow sandstone that has been bioturbated, and contains ripple marks. -A thin tongue of the Mancos Shale overlays the Paguate sandstone here •Twowells Member - Sandstone The Jemez Mountains The Jemez mountains surround the Valle Caldera, One of the largest volcanic craters in the world. There are some Triassic age stratagraphic units exposed on the southern end of the Jemez uplift though. - Anton Chico Member of the Moenkopi Formation. This unit is the oldest unit Exposed here and overlies disconformably, middle Permian sandstones that are relatively thin units (up to 39m) recognized as red-bed sandstones. - Agua Zarca Formation of the Chinle Group overlies disconformably the Moenkopi Formations and are a thick sequence ( up to 400m) of red-bed mudstones with a fairly thick basal unit ( up to 61m) of sandstone and extrabasinal conglomerates. Triassic Units Chinle Group •Agua Zarca Member sandstones are white to brown, med-coarse grained quartz arenite, typically crossbedded conglomerates. The dominant clast are Metaquartzite pebbles up to 15cm with some red jasper, and petrified wood mixed in. The Agua Zarca generally fines upward and conformably grades to the Salitral. The Salitral Formation is comprised of mostly purple, blue and red mudstone with Calcareous concretions and the maximum thickness of the Salitral is 102m but is Usually thinner. •The Poleo Formation sandstone and conglomerate dominated unit resembles The Agua Zarce Formation. However the Poleo sandstones are gray micaceous Litharenits. The Conglomerates are dominately calcrete clasts with siliceous Clast being uncommon. The Poleo maximum thickness is 40m in northern areas, And thins southward into the Jemez uplifts. The base of this unit is a Disconformity while conformably overlain by the Petrified Forest Formation. •The Petrified Forest formation is dominated by reddish brown mudstone that is the Painted Desert Member. It also contains many thin beds of crossbedded Or laminated micaceous litharenite and calcreteclast dominated conglomerate. The upper part of the Petrified forest formation is the correo sandsone bed of The painted desert member and is disconformably overlain by the Middle Jurassic Entrada Sandstone. Structural Features Cabezon Peak, an eroded volcano throat, near San Ysidro Structural history: 75 million years ago Laramide Orogeny Jemez Mountain Range Jemez Mountain Range Cont. Jemez lineament is a NE trending crustal flaw that controlled volcanism and tectonism in the Jemez Mountains and the Rio Grande rift zone Volcanism did not begin until after the Sante Fe rift The volcanic rocks lie uncomformably on top of igneous, metamorphic, and sedimentary rocks Ages range from Precambrian through late Tertiary. Mesozoic sedimentary rocks form the eastwarddipping backslope of the Sierra Nacimient The Valles Caldera truncated an older volcanic flow Jemez Mountain Range Cont. The western margin of the Rio Grande depression in the Jemez area is delineated by a zone of northeast-trending faults. An en echelon zone is expressed by the Pajarito fault zone in the San Miguel Mts North of Santa Clara Canyon,fault zone is a series of antithetic faults that displace the basalts along the eastern edge of Lobato Mesa. Faults in the West generally show more normal displacement downward to the east with Right-Slip faulting Faults in the East are antithetic (displacement is opposite to faults ) with Left slip faulting Fun Fact: Due to such high geothermal volcanic activity, the Jemez Mountains contain several hot springs, making them a tourist Hot Spot Jemez Mountains Cont. Sandia Mountains Sandia Mountains Dominated by an eastward-tilted fault block An unusual structure of the area is the Tijeras rift belt bounding the uplift that trending northeastwards and contains a southwestern folded graben and a northeastern horst Tijeras rift belt was formed in the Laramide Orogeny North-east striking, subvertical faults : Tijeras, Gutierrez, San Lazarus, Los Angeles, and Lamy faults Sandia Mountains Cont. Tijeras fault is a Left-Lateral Slip Fault system links to north-striking Picuris-Pecos fault system Tijeras–Cañoncito fault system is characterized bysubparallel faults, Horsts and grabens are present along much of its length. Sandia Mountains Cont. Albuquerque Basin The basin is part of an orogenic belt dominated by a rift valley system To the west is the Colorado Plateau, the Sandia fault to the east, the Nacimiento uplift, into the Jemez Mts, and La Bajada scarp to the north, and the Socorro constriction to the south. consists of two subbasins downdropped along low-angle to listric, normal faults of opposing structural polarity seperated by a mid-basin transverse structural zone Lithology Mancos Shale Deposited by an ancient inland sea during the Cretaceous time period. Source: geosciences.fau.edu Dakota Formation Deposited during Early Cretaceous and earliest Late Cretaceous in response to a regional transgression. Source: bforist.blogspot.com Morrison Formation Consists of sandstone and mudstone deposited in fluvial environments. Source: en.wikipedia.org Summerville Formation Summerville deposition took place on a vast arid coastal plain that extended from Utah to Oklahoma (Anderson and Lucas, 1992, 1994; Lucas and Anderson, 1997). Source: urth-picturepost.blogspot.com Todilto Formation Is limestone that was deposited by a saline inland sea. Source: fs.usda.gov Chinle Group Deposited on widespread alluvial plains of low relief. Source: schmunda.blogspot.com Questions?