Last edited by Vuktilar
Wednesday, May 20, 2020 | History

2 edition of Upper Cenomanian foraminifers from the southern part of the San Juan Basin, New Mexico found in the catalog.

Upper Cenomanian foraminifers from the southern part of the San Juan Basin, New Mexico

Mary Alice Carey

Upper Cenomanian foraminifers from the southern part of the San Juan Basin, New Mexico

by Mary Alice Carey

  • 21 Want to read
  • 31 Currently reading

Published by U.S. G.P.O., for sale by Book and Open-File Report Sales in Washington, DC, Denver, CO .
Written in English

    Places:
  • San Juan Basin (N.M. and Colo.)
    • Subjects:
    • Foraminifera, Fossil -- San Juan Basin (N.M. and Colo.),
    • Paleontology -- Cretaceous.,
    • Paleontology -- San Juan Basin (N.M. and Colo.)

    • Edition Notes

      Other titlesUpper Cenomanian foraminifers, San Juan Basin, New Mexico.
      Statementby Mary Alice Carey.
      SeriesEvolution of sedimentary basins--San Juan Basin ;, ch. N, U.S. Geological Survey bulletin ;, 1808-N
      Classifications
      LC ClassificationsQE75 .B9 no. 1808N, QE772 .B9 no. 1808N
      The Physical Object
      Paginationiv, 17 p., 3 leaves of plates :
      Number of Pages17
      ID Numbers
      Open LibraryOL1560999M
      LC Control Number91042291

      Pillmore CL, Flores RM () Stratigraphy and depositional environments of the Cretaceous - Tertiary boundary clay and associated rocks, Raton basin, New Mexico and Colorado. In: Fassett JE, J. K. Rigby J (eds) The Cretaceous-Tertiary boundary in the San Juan and Raton Basins, New Mexico and Colorado. foraminifers in surface sediments of the Andaman Sea. A comparable analysis of planktonic foramin­ ifers in the samples is in progress. The area is bounded approximately by latitudes 16°N. and 6°N. and longitudes 93 °E. and 98 °E. The northern boundary of the sea is Burma, the eastern boundary.

      San Juan Basin, New Mexico.—The Upper Creta­ ceous sequence in the southwestern part of the San Juan Basin, New Mexico, consists from the base up of the Pictured Cliffs Sandstone, the coal-bearing Fruitland Formation, and the Kirtland Shale. Meas­ urement of new stratigraphic sections by R. M. SEQUENCE STRATIGRAPHY AND DEPOSITIONAL HISTORY OF THE UPPER CAÑON DEL TULE, LAS IMAGENES, AND LOWER CERRO GRANDE FORMATIONS, CENTRAL PARRAS BASIN, NORTHEASTERN MEXICO. Juan Clemente Bermúdez Santana, Ph. D. The University of Texas at Austin, Supervisor: Richard T. Buffler. pages, references, 20 plates.

      About The Product. Published by the American Geophysical Union as part of the Field Trip Guidebooks Series.. The present tectonic regime of northern California includes transform faulting south of the Mendocino triple junction, eastward-directed subduction, north of the junction and extensional rifting and recent volcanism in the Cascade Range to the east. This banner text can have markup.. web; books; video; audio; software; images; Toggle navigation.


Share this book
You might also like
Diabetic Delights

Diabetic Delights

So wild the sea

So wild the sea

first of the few

first of the few

Architecture contemporaine =

Architecture contemporaine =

city of Bath of the days of our grandfathers and of to-day

city of Bath of the days of our grandfathers and of to-day

Planned marketing

Planned marketing

Linux Apache web server administration

Linux Apache web server administration

companion to murder

companion to murder

origin of the Griselda story.

origin of the Griselda story.

Water-ski wipeout

Water-ski wipeout

Eggs and more eggs

Eggs and more eggs

Studies on Voltaire and the eighteenth century.

Studies on Voltaire and the eighteenth century.

Toward a closed shop on the campus

Toward a closed shop on the campus

WORLD Yearbooks of Education 1986

WORLD Yearbooks of Education 1986

Massachusetts Division of Water Pollution Control

Massachusetts Division of Water Pollution Control

Upper Cenomanian foraminifers from the southern part of the San Juan Basin, New Mexico by Mary Alice Carey Download PDF EPUB FB2

Get this from a library. Upper Cenomanian foraminifers from the southern part of the San Juan Basin, New Mexico. [Mary Alice Carey; Geological Survey (U.S.)] -- A multidisciplinary approach to research studies of sedimentary rock and their constituents and the evolution of.

Upper Cenomanian foraminifers from the southern part of the San Juan Basin, New Mexico / By Mary Alice. Carey and Geological Survey (U.S.) Abstract.

Shipping list no.: title: Upper Cenomanian foraminifers, San Juan Basin, New es bibliographical references (page 16).Mode of access: Internet. @article{osti_, title = {Foraminifers suggest environmental differences between Whitewater Arroyo shale tongue and basal main-body Mancos shale, San Juan basin, New Mexico}, author = {Carey, M.A.}, abstractNote = {The Upper Cretaceous (Cenomanian) Whitewater Arroyo Tongue of the Mancos Shale is the upper shale in an intertonguing rock sequence consisting of three Dakota Sandstone.

The crocodylian assemblage from the Upper Cretaceous strata of the San Juan Basin, New Mexico, consists of four identifiable taxa: Brachychampsa montana, cf. Leidyosuchus sp., Denazinosuchus. Upper Cenomanian foraminifers from the southern part of the San Juan Basin, New Mexico / (Washington, DC: U.S.

G.P.O. ; Denver, CO: For sale by Book and Open-File Report Sales, ), by Mary Alice Carey and Geological Survey (U.S.) (page images at HathiTrust) Items below (if any) are from related and broader terms.

Cretaceous stratigraphy and biostratigraphy, Clayton Lake State Park, Union County, New Mexico Article (PDF Available) in New Mexico Geology 8(3) January with 96 Reads. Paleontology San Juan Basin (N.M. and Colo.) See also what's at your library, or elsewhere.

Broader terms: New Mexico; Colorado; Filed under: Paleontology San Juan Basin (N.M. and Colo.) Upper Cenomanian foraminifers from the southern part of the San Juan Basin, New Mexico / (Washington, DC: U.S.

G.P.O. ; Denver, CO: For sale by Book and Open-File Report Sales, ), by Mary Alice Carey. B N / Carey, M. / UPPER CENOMANIAN FORAMINIFERS FROM THE SOUTHERN PART OF THE SAN JUAN BASIN, NEW MEXICO,pb, 17 pages, 3 plates, 16 figs., $ 6 Looking for other sections of B or. They may be in another adjacent state catalog.

Go to the USGS Bulletin catalog and scroll down to those numbers. Conference: Shelf sandstones of Twowells tongue, Dakota Sandstone, northwestern New Mexico. The Ixtapa graben is located in the central part of the shear belt of the Sierra de Chiapas (Figures 1, 2, 3, and 4).This graben exposes the most complete middle Cretaceous (informal term used in Mexico for the Albian-Cenomanian stages)-Quaternary section of southeastern Mexico and displays structural features that are typical of transtensional and transpressional settings ().

The fossil site described here is located in the southern part of the Tlaxiaco Basin (), a geological depression on the Acatlan-Oaxaca block, which extends from southern Puebla, via central and north Oaxaca, to eastern Guerrero states (Cantú-Chapa, b, Nieto-Samaniego et al.,Alvarado-Ortega et al.,fig.

2).The Tlaxiaco Basin was active during the Jurassic and Cretaceous. The Chicxulub crater, km by km in diameter, is located beneath the Yucatan Platform, in the southern Gulf of Mexico basin. The consequent seismic shock triggered submarine slides and mass flows along the continental slope (Bralower et al.,Poag, ).

An impact tsunami created a distinct event bed that is widely noted around the. b l / hunter, r. e., / clastic pipes of probable solution-collapse origin in jurassic rocks of the southern san juan basin, new mexico,pb, 19 pages, 14 figs., 1 tables, $ 12 B N / Carey, M.

/ UPPER CENOMANIAN FORAMINIFERS FROM THE SOUTHERN PART OF THE SAN JUAN BASIN, NEW MEXICO,pb, 17 pages, 3 plates, 16 figs., $ 6. The upper part of the Comburindiocorrelates with the Lower Aptian El Cajon Formation about 20 kmeast. Key Barremian-Early Aptian foraminifers, Palorbitolinalenticularis, Choffatella sp.

aff. decipiens, Everticyclamina hedbergi, and Praechrysalidina infracretacea range throughout the El Cajon(Omana-Pulido and Pantola-Alor, ).

The Cretaceous–Paleogene (K–Pg) extinction event, also known as the Cretaceous–Tertiary (K–T) extinction, was a sudden mass extinction of three-quarters of the plant and animal species on Earth, approximately 66 million years ago.

With the exception of some ectothermic species such as the leatherback sea turtle and crocodiles, no tetrapods weighing more than 25 kilograms (55 pounds. We used petrofacies analysis, carbon, oxygen and strontium isotope data to interpret the isotopic variations in the carbonate rocks of the Mural Formation of Sonora (Sierra San José section), Mexico.

The petrographic study reveals a range of lithofacies from wackestone to packstone. The analyzed limestones show significant negative δ18O values ( to VPDB) and δ13C values ranging. Conodont faunas from a complete basinal succession of the upper part of the Wordian (Middle Permian, Guadalupian,West Texas) Bruce R.

Wardlaw and Merlynd K. Nestell - online 31 Dec An apparatus reconstruction of the conodont Caenodontus serrulatus Behnken Gordon, W.A., b, Foraminifera from the 4CPR oil test well near Arecibo, Puerto Rico, in Oil and gas possibilities of northern Puerto Rico, Puerto Rico Mining Commission, San Juan, p.

Gordon, W.A.,Two crab species from the Middle Tertiary of Puerto Rico: 3rd Caribbean Geological Conference (Jamaica, April ) Transactions, p. A Color Guide to the Petrography of Carbonate Rocks: Grains, Textures, Porosity, Diagenesis (AAPG Memoir) (Aapg Memoir) Peter A.

Scholle, Dana S. Ulmer-Scholle This volume expands and improves the AAPG classic, A Color Illustrated Guide to Carbonate Rock Constituents, Textures, Cements, and Porosities (AAPG Memoir 27). Revised ages of blueschist metamorphism and the youngest pre-thursting rocks in the San Juan Islands, Washington.

Canadian Journal of Earth Science, Dutton, A., Lohmann, K.C., Leckie, R.M., Insights from the Paleogene tropical Pacific: Foraminiferal stable isotope and elemental results from SiteShatsky Rise.

Sealey P.L. & Lucas S.G. ().Campanian ammonites and other mollusks from the Lewis Shale, eastern San Juan Basin, Rio Arriba County, New Mexico. New Mexico Museum of Natural History and Science Bulletin sandstone complex of the upper part of the Dockum. In it are many small and a few moderate-sized depos­ its in sandstone- and mudstone-matrix conglomerate in the Canadian River valley in Texas and New Mexico and in Briscoe and Garza Counties, Tex.

Origin of roll-type uranium deposits H. C. Granger and C. G. Warren (r) proposed.Pantoja-Alor and Carrillo-Bravo () first described this unit which is also located in Baja California Sur.

Its stratotype is near the intersection of the Coyote and La Trinidad Streams, in the western margin of the Coyote Stream; however, these outcrops are from both San José del Cabo and Los Barriles Basins (Pantoja-Alor and Carrillo-Bravo ; Martínez-Gutiérrez and Sethi