1 edition of Petrology and physiographic evolution of the Ocate volcanic field, north-central New Mexico. found in the catalog.
Petrology and physiographic evolution of the Ocate volcanic field, north-central New Mexico.
by U.S. Govt. Print. Off., For sale by the Books and Open-File Reports Section, U.S. Geological Survey in Washington, Denver, CO
Written in English
|Other titles||Ocate volcanic field, north-central New Mexico.|
|Series||U.S. Geological Survey professional paper ;, 1478, Geological Survey professional paper ;, 1478.|
|Contributions||O"Neill, J. Michael., O"Neill, J. Michael.|
|LC Classifications||QE461 .P474 1988|
|The Physical Object|
|Pagination||x, 30, 15 p. :|
|Number of Pages||30|
|LC Control Number||87600260|
processes at the volcanic front of the Mexican Volcanic Belt (MVB). New as well as published major- and trace-element and Sr and Nd isotopic data are used to constrain the magma generation and evolution processes in the SCN. Monogenetic fields are found in different tectonic settings: intraplate volcanism such as the Auckland field in New Zealand (Németh and Kereszturi, ; Le Corvec et al., a, Le Corvec et al., b; Lindsay et al., ) and the Eiffel field in Germany (Schmincke, ) and in volcanic arcs such as the San Francisco field in the USA (Tanaka et al., ) and the Carrán-Los Venados field Cited by: 8.
A Study of Pennsylvanian-Permain Arkoses in North-Central New Mexico: M.S. Chisholm, Earl J Petrology of the San Andres Formation of Central New Mexico: M.S. Clair, Virginia: Some Fusulinidae from San Miguel County, New Mexico: . Major- and trace-element geochemistry and mineralogy of upper Eocene to Quaternary volcanic rocks of the Mogollon-Datil volcanic field, southwestern New Mexico: Publication Type: Book: Authors: Bornhorst, T: Year: Keywords: Volcanic ash - tuff – New Mexico: Call Number: LDG46 B URL.
Volcanic fields are regions of volcanic activity that tap one magma source. Eruptions in the RCVF began approximately 9 million years ago, with Capulin's eruption taking place betw years ago. Potential still exists for future eruptions from dormant volcanoes in the field today. Volcanic fields stretch across New Mexico. This field guide describes a five day trip to examine deposits of Late Pleistocene-Holocene cataclysmic eruptions at Nevado de Toluca and Jocotitlan volcanoes in central Mexico. We will discuss the stratigraphy, petrology, and sedimentological characteristics of these deposits which provide insights into the eruptive history, type of volcanic activity, and transport and .
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Petrology and physiographic evolution of the Ocate volcanic field, north-central New Mexico Professional Paper A,B By: J. O'Neill and H.H. Mehnert. Get this from a library. Petrology and physiographic evolution of the Ocate volcanic field, north-central New Mexico. [J Michael O'Neill;].
Get this from a library. Petrology and physiographic evolution of the Ocate volcanic field, north-central New Mexico. [J Michael O'Neill; Harald H Mehnert; Geological Survey (U.S.),]. NEW MEXICO BUREAU OF GEOLOGY & MINERAL RESOURCES, BULLETIN40Ar/39Ar geochronology of the Ocate volcanic field, northcentral New Mexico Brian W.
Olmsted1 and William C. McIntosh2 1Department of Earth and Environmental Science, New Mexico Institute of Mining and Technology, Socorro, NM 2New Mexico Bureau of Geology and Mineral Resources, New Mexico.
Buy MINERALOGY AND PETROLOGY OF THE RATON-CLAYTON VOLCANIC FIELD, NORTHEASTERN NEW MEXICO on FREE SHIPPING on qualified orders. By Geochrondlogy Petrography, Petrology, Ocate Volcanic Field, Geochronology Petrography, J.
Michael O&apos, Harald H. Mehnert, J. Michael O&apos and Dallas L. Peck Abstract Petrology and physiographic evolution of the Ocate volcanic field, north-central New Mexico.
pp / o’neill, j. m., / petrology and physiographic evolution of the ocate volcanic field, north-central new mexico, a.
the ocate volcanic field and b. late cenozoic physiographic evolution of the ocate volcanic field, pb, 45 pages, 1 plate (in. O'Neill, J.M.,Late Cenozoic physiographic evolution of the Ocate Volcanic Field, in Petrology and physiographic evolution of the Ocate Volcanic Field, north-central New Mexico: U.S.
Geological Survey Professional Paperp. B1-B Geochemistry and petrology of the Ocampo volcanic field, Coahuila, Mexico Article (PDF Available) in Boletin de la Sociedad Geologica Mexicana 63(2). Dungan. University of Oregon The petrology and geochemistry of the Ocate volcanic field, north-central New Mexico.
Article. Full-text available. Jan. Calvin, E.M.,A review of the volcanic history and stratigraphy of northeastern New Mexico, the Ocate and Raton-Clayton volcanic fields: NM Geological Society, 38th Field Conference, Guidebook, p.
Abstract. The Miocene–Quaternary Jemez Mountains volcanic field (JMVF) is the site of the Valles caldera and associated Bandelier Tuff.
Caldera formation was preceded by > 10 Myr of volcanism dominated by intermediate composition rocks (57–70% SiO 2) that contain components derived from the lithospheric mantle and Precambrian mixing Cited by: pp / o’neill, j.
m., / petrology and physiographic evolution of the ocate volcanic field, north-central new mexico, a. the ocate volcanic field and b. late cenozoic physiographic evolution of the ocate volcanic field, pb, 45 pages, 1 plate (in pocket), 31 figs., 6 tables, $ 15 pp / o’neill, j.
m., ed. Baldridge W.S. () Petrology of Plio-Pleistocene Basaltic Rocks from the Central Rio Grande Rift (New Mexico, USA) and their Relation to Rift Structure. In: Neumann ER., Ramberg I.B. (eds) Petrology and Geochemistry of Continental Rifts. NATO Advanced Study Institutes Series (Series C — Mathematical and Physical Sciences), vol Cited by: 7.
The Volcanoes of New Mexico Volcanoes and volcanic landforms are abundant, well-exposed, and un-eroded in New Mexico, so there are many opportunities to use New Mexico examples for understanding physical volcanology characteristics.
And one of the great rift valleys of Earth, the Rio Grande rift, also cuts through the middle of New Mexico.
Major and trace-element whole rock data, Nd and Sr isotopic data, and microprobe data have been collected from a suite of basanites, olivine nephelinites, and olivine melilite nephelinites from the Raton-Clayton volcanic field, New Mexico.
Most of the lavas have geochemical characteristics that suggest they are primary upper mantle derived melts. The Cited by: The latter is an alignment of late Cenozoic volcanic fields extending from SE Arizona to NE New Mexico, which coincides with the surface boundary of a suture zone complex between the Proterozoic Southern Yavapai (18–17 Ga) and Mazatzal (165 Ga) lithospheric provinces (Shaw & Karlstrom, ; Karlstrom et al., ).
Compared with the Cited by: O’Neill, J. M.,Late Cenozoic physiographic evolution of the Ocate volcanic field; in Petrology and physiographic evolution of the Ocate volcanic field, north-central New Mexico: U.S. Geological Survey, Professional Paper B, pp.
B1–B The TMVB is made up of nearly volcanoes that extend from the Gulf of California to the Gulf of México (Suter et al., ).The MGVF is located in the central part of the TMVB and is affected by three regional fault systems: 1) The youngest is the E-W normal fault system associated with N-S extension that corresponds to the Morelia-Acambay Fault System (MAFS) (Suter et al., Cited by: 3.
IGNEOUS GEOLOGY AND STRUCTURE OF THE MOUNT TAYLOR VOLCANIC FIELD NEW MEXICO Paperback – January 1, by C.B. Hunt (Author) See all formats and editions Hide other formats and editions. Price New from Used from Paperback, Author: C.B.
Hunt. Cambridge Core - Mineralogy, Petrology and Volcanology - Petrology of Sedimentary Rocks - by Sam Boggs, JrAuthor: Jr Sam Boggs.The book focuses on the stratigraphy exposed by the Laramide uplift and subsequent erosion, and on the mid-Tertiary Navajo Volcanic Field.
Also examined is the unusual igneous petrology of several Navajo Volcanic Field centers, as well as their diverse structures and volcanic .Full text of "Bulletin of the United States Geological Survey--Bibliography and Index of North American Geology, Paleontology, Petrology, and Mineralogy for .