2 edition of Quaternary movement along the La Jencia fault, central New Mexico found in the catalog.
Quaternary movement along the La Jencia fault, central New Mexico
Michael N Machette
by Dept. of the Interior, U.S. Geological Survey, For sale by the Books and Open-File Reports Section in [Reston, Va.?], Denver, CO
Written in English
|Statement||by Michael N. Machette|
|Series||U.S. Geological Survey professional paper -- 1440|
|Contributions||Geological Survey (U.S.)|
|The Physical Object|
|Pagination||iv, 82 p. :|
|Number of Pages||82|
|LC Control Number||86600026|
We mapped sections of the north trending faults in a km long left-stepping fault array. Starting in the south, the San Jose del Cabo fault (east dipping) bounds the ~2 km high Sierra La Laguna. It is >70 km long with well defined meter fault scarps cutting the youngest late Quaternary . Using statistical geophysical relationships and mountain front morphology as tools for evaluation of fault segment lengths: The la Jencia fault, New Mexico. Geological Society of America, annual meeting. Abstracts with Programs, v. 29, n. 6, p. Eppes, M., Harrison, B., A chronosequence study of soils developing on basalt flows.
Quaternary faulting history along the Deep Springs fault, California Jeffrey Lee* Department of Geological Sciences, Central Washington University, Ellensburg, Washington , USA and Institute for Crustal Studies, University of California, Santa Barbara, California , USA Charles M. Rubin. Activity on this fault influences offshore faults that parallel the Pacific coast from Ensenada to Los Angeles and is a potential threat to communities in northern Mexico and southern California. We present a detailed Quaternary slip history for the ABF, including new quantitative constraints on geologic slip rates, slip-per-event, the timing.
Peter, J. Bakewell's study, "Silver Mining and Society in Colonial Mexico, Zacatecas ," is the fifteenth and final work in a series of Cambridge Latin American Studies. This is a worthwhile primer for Latin American research because the author includes an essay on primary sources at the end of the by: The most prominent structure of this segment is the 45‐km‐long Venta de Bravo fault with a relief ≤ m. The Febru , m b = Maravatio earthquake occurred on this fault. The late Quaternary vertical slip rate along the easternmost part of the Venta de Bravo fault is estimated at 2 mm/ by:
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From abstract: The La Jencia fault is a recently reactivated late Cenozoic basin margin structure of major proportions that forms the western margin of the Rio Grande rift, which borders the eastern sides of the northern Magdalena Mountains and the southern Bear Mountains in central New by: Quaternary movement along the La Jencia fault, central New Mexico.
[Michael N Machette; Geological Survey (U.S.)] -- A detailed study of movement along a late Quaternary fault of the Rio Grande rift utilizing geologic mapping, exploratory trenches, soil development, laboratory analyses, and fault-scarp morphology. Quaternary movement along the La Jencia fault, central New Mexico (OCoLC) Material Type: Government publication, National government publication, Internet resource: Document Type: Book, Internet Resource: All Authors / Contributors: Michael N Machette.
The La Jencia and Albuquerque-Belen basins are two of the main structural depressions in the central part of the Rio Grande rift of New Mexico.
Within these two basins are many faults that displace basin- fill deposits of Pliocene and Quaternary age and surficial deposits of middle and late Quaternary age. Both ranges have embayed range-fronts, suggesting a lack of significant Quaternary faulting.
However, La Jencia fault forms the tectonic margin between the mountains to the west and the Cenozoic La Jencia basin to the east.
Hueco fault zone. Structure Number Structure NameHueco fault zone Comments: Named by Seager ( #). Refers to numerous Quaternary intrabasin faults in the northwestern part of the Hueco bolson (basin) of west Texas and southern New Mexico (see Machette, #).
MS Book and Mineral Company. USGS Professional Papers 6 - Geologic and Mining Central New Mexico book, Numbers - M. / QUATERNARY MOVEMENT ALONG THE LA JENICA FAULT, CENTRAL NEW MEXICO,pb, 82 pages, 2 plates (in pocket), 17 Ed.
/ ASSESSMENT OF REGIONAL EARTHQUAKE HAZARDS AND RISK ALONG THE WASATCH FRONT, UTAH,pb, pages. However, there is evidence for such an event in northwestern Sonora, Mexico, just 20 km from the southwest corner of New Mexico.
Length This field specifies two types of length data. The first is the end-to-end length of the Quaternary-age fault as measured from the most distal ends of the digital data. The "World Map of Major Active Faults" Task Group is compiling a series of digital maps for the United States and other countries in the Western Hemisphere that show the locations, ages, and activity rates of major earthquake-related features such as faults and fault-related folds; the companion database includes published information on these seismogenic features.
The Pajarito fault forms the western margin of the Rio Grande rift in north-central New Mexico, and lies adjacent to Los Alamos National Laboratory, a major Federal research facility. Vertical displacement on this normal fault over the past Ma has created a to m-high fault scarp on Bandelier Tuff ( Ma), yielding a long-term Cited by: Quaternary movement along the La Jencia fault, central New Mexico.
U.S. Geological Survey Professional PaperPaleoseismic analysis of the Wasatch fault zone the Pole Patch trench site Author: Hasan Cetin.
Claudia J. Lewis, W. Scott Baldridge, "Crustal extension in the Rio Grande rift, New Mexico: Half-grabens, accommodation zones, and shoulder uplifts in the Ladron Peak-Sierra Lucero area", Basins of the Rio Grande Rift: Structure, Stratigraphy, and Tectonic Setting, G.
Randy Keller, Steven M. Cather. The offshore Carrizal fault lies km east of the western edge of La Paz Bay, forming a right step from the onshore Carrizal fault. The offshore Carrizal fault is the oldest fault of the fault system, and the fault likely grew in the latest Miocene to Pliocene in a complex way to the south toward the onshore Centenario and Carrizal faults.
The Water Canyon site (LA) is located in west-central New Mexico (Figure 1), on lands managed by the Energetic Materials Testing and Research Center (EMRTC), a division of the New Mexico Institute of Mining and Technology, Socorro, New Mexico. As such, the property on which the site is located has restricted public access.
Even though independent rupture segments are defined in the literature for the La Jencia fault based on based on the continuity of scarps and inferred timing of the most recent surface-faulting earthquakes (Machette, ), the source extends across both segments.
MS Book and Mineral Company New Mexico Geology and Mining History Catalog I - Federal Publications M. / QUATERNARY MOVEMENT ALONG THE LA JENICA FAULT, CENTRAL NEW MEXICO,pb, 82 pages, 2 plates (in pocket), 17 figs., 23 tables, $ 8 J.
M., / PETROLOGY AND PHYSIOGRAPHIC EVOLUTION OF THE OCATE VOLCANIC FIELD, NORTH-CENTRAL. JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 97, NO. B8, PA, J Active Faults and State of Stress in the Central Part.
Introduction. Current stress conditions of the continental crust in central Mexico have commonly been inferred from structural features such as fault trends, alignment of shield volcanoes, orientation of major dikes, well elongations, etc., (e.g.
Suter et al., ) due to the scarcity of seismicity studies have demonstrated that some of the faults which traverse central Mexico Cited by: The Water Canyon site is one of a series of early-to-middle Holocene age archaeological sites eroding out of sediments along the Water Canyon drainage at the toe end of a large bajadas that flanks the Magdalenas.
The site, as originally documented incovered an area of approximately sq m. The Pajarito fault forms the western margin of the Rio Grande rift in north-central New Mexico, and lies adjacent to Los Alamos National Laboratory, a major Federal research facility.
Vertical displacement on this normal fault over the past Ma has created a to m-high fault scarp on Bandelier Tuff ( Ma), yielding a long-term.
ages of soils based on correlation with soils near Las Cruces in southern New Mexico; (2) use of surface age-fault offset relationships to constrain the age of most-recent fault movement and to estimate the frequency of movement along individual faults; and (3) morphologic analyses of fault File Size: KB.The 35 km long La Jencia fault falls just inside the western boundary of the SSA.
Using the relations of Wells and Coppersmith (), we believe the observations by Machette () on the scarps of the La Jencia fault can be explained qualitatively by the movements of five moment magnitude earthquakes in the p years.The Cerro GoDen fault zone is associated with a curvilinear, continuous, and prominent topographic lineament in western Puerto Rico.
The fault varies in strike from northwest to west. In its westernmost section, the fault is??? m south of an abrupt, curvilinear mountain front separating the to m-high La CaDena De San Francisco range from the Rio A??asco alluvial valley.