Relevant bibliographies by topics / Structural Nevada

Academic literature on the topic 'Structural Nevada'

Author: Grafiati
Published: 10 December 2022
Last updated: 28 January 2023

Create a spot-on reference in APA, MLA, Chicago, Harvard, and other styles

Select a source type:

Contents

Consult the lists of relevant articles, books, theses, conference reports, and other scholarly sources on the topic 'Structural Nevada.'

Next to every source in the list of references, there is an 'Add to bibliography' button. Press on it, and we will generate automatically the bibliographic reference to the chosen work in the citation style you need: APA, MLA, Harvard, Chicago, Vancouver, etc.

You can also download the full text of the academic publication as pdf and read online its abstract whenever available in the metadata.

Journal articles on the topic "Structural Nevada"

1

BHATTACHARYYA, TAPAS, and SCOTT R. PATERSON. "Timing and structural expression of the Nevadan orogeny, Sierra Nevada, California: Discussions and reply." Geological Society of America Bulletin 96, no. 10 (1985): 1346. http://dx.doi.org/10.1130/0016-7606(1985)96<1346:taseot>2.0.co;2.

Full text
APA, Harvard, Vancouver, ISO, and other styles
2

TOBISCH, OTHMAR T., and RICHARD S. FISKE. "Timing and structural expression of the Nevadan orogeny, Sierra Nevada, California: Discussions and reply." Geological Society of America Bulletin 96, no. 10 (1985): 1348. http://dx.doi.org/10.1130/0016-7606(1985)96<1348:taseot>2.0.co;2.

Full text
APA, Harvard, Vancouver, ISO, and other styles
3

SCHWEICKERT, RICHARD A., NICHOLAS L. BOGEN, GARY H. GIRTY, RICHARD E. HANSON, and CHARLES MERGUERIAN. "Timing and structural expression of the Nevadan orogeny, Sierra Nevada, California: Discussions and reply." Geological Society of America Bulletin 96, no. 10 (1985): 1349. http://dx.doi.org/10.1130/0016-7606(1985)96<1349:taseot>2.0.co;2.

Full text
APA, Harvard, Vancouver, ISO, and other styles
4

Loulakis, Michael C., and Lauren P. McLaughlin. "Nevada Supreme Court Dismisses Suit against Structural Engineer." Civil Engineering Magazine Archive 83, no. 11 (December 2013): 84. http://dx.doi.org/10.1061/ciegag.0000726.

Full text
APA, Harvard, Vancouver, ISO, and other styles
5

Huesca, Margarita, Keely L. Roth, Mariano García, and Susan L. Ustin. "Discrimination of Canopy Structural Types in the Sierra Nevada Mountains in Central California." Remote Sensing 11, no. 9 (May 8, 2019): 1100. http://dx.doi.org/10.3390/rs11091100.

Full text
Abstract:
Accurate information about ecosystem structure and biogeochemical properties is essential to providing better estimates ecosystem functioning. Airborne LiDAR (light detection and ranging) is the most accurate way to retrieve canopy structure. However, accurately obtaining both biogeochemical traits and structure parameters requires concurrent measurements from imaging spectrometers and LiDARs. Our main objective was to evaluate the use of imaging spectroscopy (IS) to provide vegetation structural information. We developed models to estimate structural variables (i.e., biomass, height, vegetation heterogeneity and clumping) using IS data with a random forests model from three forest ecosystems (i.e., an oak-pine low elevation savanna, a mixed conifer/broadleaf mid-elevation forest, and a high-elevation montane conifer forest) in the Sierra Nevada Mountains, California. We developed and tested general models to estimate the four structural variables with accuracies greater than 75%, for the structurally and ecologically different forest sites, demonstrating their applicability to a diverse range of forest ecosystems. The model R2 for each structural variable was least in the conifer/broadleaf forest than either the low elevation savanna or the montane conifer forest. We then used the structural variables we derived to discriminate site-specific, ecologically meaningful descriptions of canopy structural types (CST). Our CST results demonstrate how IS data can be used to create comprehensive and easily interpretable maps of forest structural types that capture their major structural features and trends across different vegetation types in the Sierra Nevada Mountains. The mixed conifer/broadleaf forest and montane conifer forest had the most complex structures, containing six and five CSTs respectively. The identification of CSTs within a site allowed us to better identify the main drivers of structural variability in each ecosystem. CSTs in open savanna were driven mainly by differences in vegetation cover; in the mid-elevation mixed forest, by the combination of biomass and canopy height; and in the montane conifer forest, by vegetation heterogeneity and clumping.
APA, Harvard, Vancouver, ISO, and other styles
6

Sebaaly, Peter E., Edgard Hitti, and Dean Weitzel. "Effectiveness of Lime in Hot-Mix Asphalt Pavements." Transportation Research Record: Journal of the Transportation Research Board 1832, no. 1 (January 2003): 34–41. http://dx.doi.org/10.3141/1832-05.

Full text
Abstract:
The pavement community has recognized that moisture damage of hot-mix asphalt (HMA) has been a serious problem since the early 1960s. Numerous additives have been evaluated with the objective of reducing the potential of moisture damage in HMA mixtures; lime has been one of the most common ones. The Nevada Department of Transportation has been using lime in HMA mixtures since the mid-1980s. The objective of this research was to quantify the improvements in pavement performance that have been realized through the addition of lime to HMA mixtures. The program evaluated field samples and pavement performance data from untreated and lime-treated pavements. The properties of untreated and lime-treated mixtures from field projects in the southern and northwestern parts of Nevada indicate that lime treatment of Nevada's aggregates significantly improves the moisture resistance of HMA mixtures. The study showed that lime-treated HMA mixtures become significantly more resistant to multiple freeze–thaw cycles than do the untreated mixtures. Long-term pavement performance data indicate that under similar environmental and traffic conditions, the lime-treated mixtures provide better-performing pavements with fewer requirements for maintenance and rehabilitation activities. The analysis of the impact of lime on pavement life indicates that lime treatment extends the performance life of HMA pavements by an average of 3 years. This extension represents an average increase of 38% in the expected pavement life.
APA, Harvard, Vancouver, ISO, and other styles
7

Kumar, Ravhi S., Weldu Gabrimicael, and Andrew L. Cornelius. "Materials Research at University of Nevada, Las Vegas." Materials Science Forum 879 (November 2016): 386–89. http://dx.doi.org/10.4028/www.scientific.net/msf.879.386.

Full text
Abstract:
High-pressure studies on thermoelectric materials allow the study of the relationship between structural, elastic, and electronic properties. The High Pressure Science and Engineering Center (HiPSEC) at UNLV performs interdisciplinary research on a wide variety of materials at high pressures. One such system, CrSi2 is an indirect band gap semiconductor that has potential applications in solar cells.
APA, Harvard, Vancouver, ISO, and other styles
8

Nordland, Andrew, Alexander Paz, and Alauddin Khan. "Vehicle Miles Traveled Fee System in Nevada." Transportation Research Record: Journal of the Transportation Research Board 2345, no. 1 (January 2013): 39–47. http://dx.doi.org/10.3141/2345-06.

Full text
Abstract:
Several barriers are associated with the implementation and deployment of a vehicle miles traveled (VMT) fee system; these barriers range from technology issues to public acceptance. Technology-related barriers are easier to address compared with public-related barriers. In addition, addressing technological barriers requires explicit consideration of the public's attitudes and preferences in relation to various technological options. Public perceptions of and billing preferences for a VMT fee system in Nevada were studied. A survey questionnaire was developed to capture these perceptions and preferences. A series of discrete choice models—ordered, probit, and logit models—were tested to determine the best model to use for evaluating the results of the survey. Multinomial logit models provided the best explanatory power. Modeling assumptions were tested to ensure adequate results. The model provided several interesting insights about public perceptions and preferences in regard to the VMT system. On the basis of these insights, some policy recommendations are provided.
APA, Harvard, Vancouver, ISO, and other styles
9

Vickery, Vernon R. "REVISION OF TIMEMA SCUDDER (PHASMATOPTERA: TIMEMATODEA) INCLUDING THREE NEW SPECIES." Canadian Entomologist 125, no. 4 (August 1993): 657–92. http://dx.doi.org/10.4039/ent125657-4.

Full text
Abstract:
AbstractThe nine species; of Timema Scudder known previously from California, Arizona, and Nevada are redescribed and three new species are added: Timema nakipa from Baja California, Mexico: T. tahoe from Nevada; and T. cristinae from Santa Barbara County, California. Timema nakipa and T. podura Strohecker are the only representatives of Timema known from Mexico. Keys and identification tables are presented for identification of species.
APA, Harvard, Vancouver, ISO, and other styles
10

Berger, B. R., J. V. Tingley, and L. J. Drew. "Structural Localization and Origin of Compartmentalized FluidFlow, Comstock Lode, Virginia City, Nevada." Economic Geology 98, no. 2 (April 1, 2003): 387–408. http://dx.doi.org/10.2113/gsecongeo.98.2.387.

Full text
APA, Harvard, Vancouver, ISO, and other styles
More sources

Dissertations / Theses on the topic "Structural Nevada"

1

Pearthree, Philip Arnim. "Geomorphic analyses of young faulting and fault behavior in central Nevada." Diss., The University of Arizona, 1990. http://hdl.handle.net/10150/185339.

Full text
Abstract:
This dissertation research assesses the behavior of young faults in central Nevada through analyses of landforms associated with these faults. Four large earthquakes have occurred since 1915 in a striking N-S belt in central Nevada; no comparable earthquakes have occurred elsewhere in the Great Basin. The frequency of large-earthquake occurrence, and temporal and spatial patterns and rates of faulting in central Nevada during the Holocene were assessed through geomorphic and geologic studies of young fault scarps. Ages of paleoseismic events were estimated primarily through analyses of fault scarp morphologies and characterization and quantification of soil development associated with alluvial surfaces. Rates of fault scarp degradation were explored through diffusion-based modeling of latest Pleistocene pluvial shoreline scarps. Morphologic scarp age depends strongly on scarp size; modest variations in local climate, particle size, and aspect are less important. Incorporating a factor that depends on scarp size almost always decreases the scatter in scarp age estimates, and is critical if only small scarps exist along a fault zone. An average of ±30% uncertainty about the mean scarp age estimate remains after these analyses. Soil development indices were calibrated using 14 Holocene to latest Pleistocene soil profiles in central Nevada whose maximum ages are constrained. Soil development indices were used to estimate ages of faulted and unfaulted alluvial surfaces along fault scarps. Soils and morphologic fault scarp age estimates for paleoseismic events are generally consistent. Temporal and spatial patterns and rates of faulting during the Holocene were evaluated using age estimates for paleoseismic events. The long-term rate of faulting is about 10 times lower than the historical rate. There were no other N-S belts of faulting during the Holocene, although scarp ages suggest that there may have been other temporal clusters of faulting. There have been spatial clusters of faulting during portions of the Holocene. The extensional deformation rate across central Nevada during the Holocene is about 0.5-0.75 mm/yr. Integrating this rate with fault-slip data from other portions of the northern Great Basin, the Holocene extensional deformation rate is 3.5-6.5 mm/yr, substantially lower than the historical deformation rate.
APA, Harvard, Vancouver, ISO, and other styles
2

Villa, Danielle E. "Late Paleozoic deformation at Edna Mountain, Humboldt County, Nevada." abstract and full text PDF (free order & download UNR users only), 2007. http://0-gateway.proquest.com.innopac.library.unr.edu/openurl?url_ver=Z39.88-2004&rft_val_fmt=info:ofi/fmt:kev:mtx:dissertation&res_dat=xri:pqdiss&rft_dat=xri:pqdiss:1447592.

Full text
APA, Harvard, Vancouver, ISO, and other styles
3

Doyle, Jessica B. "Geology and structure of Winters Creek, Jerritt Canyon District, Elko County, Nevada." abstract and full text PDF (free order & download UNR users only), 2007. http://0-gateway.proquest.com.innopac.library.unr.edu/openurl?url_ver=Z39.88-2004&rft_val_fmt=info:ofi/fmt:kev:mtx:dissertation&res_dat=xri:pqdiss&rft_dat=xri:pqdiss:1447627.

Full text
APA, Harvard, Vancouver, ISO, and other styles
4

Muehlberg, Jessica M. "Geology of the Tahoe City sub-basin, Lake Tahoe, California-Nevada." abstract and full text PDF (free order & download UNR users only), 2007. http://0-gateway.proquest.com.innopac.library.unr.edu/openurl?url_ver=Z39.88-2004&rft_val_fmt=info:ofi/fmt:kev:mtx:dissertation&res_dat=xri:pqdiss&rft_dat=xri:pqdiss:1442871.

Full text
APA, Harvard, Vancouver, ISO, and other styles
5

Newton, Maury Claiborne III. "Tectonostratigraphic history of the southern Foothills terrane." Diss., The University of Arizona, 1990. http://hdl.handle.net/10150/185077.

Full text
Abstract:
As a tool in discriminating basic rocks from different tectonic settings, a type of diagram was developed that employs three ratios of trace elements. The diagram separates basic rocks formed in mid-ocean ridge, intra-plate, and volcanic arc settings. It can be used to differentiate basalts from marginal basin, forearc, and arc rift zone settings. A second application of this type of diagram, employing major elements, distinguishes tholeiitic, calcalkaline, and boninitic series volcanic rocks. The southern part of the Foothills terrane, western Sierra Nevada, California, is composed chiefly of Jurassic-Triassic(?) metavolcanic and metasedimentary rocks of lower greenschist grade. Major tectonism affecting the terrane, associated with the Late Jurassic-Early Cretaceous Nevadan orogeny, was sinistral transpression with shearing along the Bear Mountains and Melones fault zones. The line of slip in high shear strain regions is approximated by the modal stretching lineation, which is at a rake of approximately 45° SE to the general shear zone orientation, suggesting sub-equal components of strike slip and dip slip. The sense of shear from kinematic indicators is consistently east side to the northwest. The terrane hosts three types of syngenetic massive sulfide deposits: Cyprus-type Cu deposits, Kuroko-type Zn-Cu-Pb deposits, and Besshi-type Cu-Zn deposits. The Cyprus-type deposits lie at the top of a Triassic(?) tholeiitic - basalt sequence in the lower Penon Blanco Formation. The deposits are part of an ophiolitic sequence that appears to have formed in an open-ocean spreading center environment. Felsic lava facies host the Kuroko-type deposits at the top of the Middle to Late Jurassic upper Gopher Ridge Formation, a dominantly bimodal sequence of meta-rhyolitic lavas and tuffs and meta-basaltic lavas. The tectonic setting appears to have been an arc-rift zone that formed during the transition from arc volcanism forming the lower Gopher Ridge Formation to younger basinal sedimentation forming the Mariposa Formation. The Besshi-type deposits are sediment-hosted in the Late Jurassic Mariposa Formation. They appear to have formed in the median part of a long linear basin between rifted arc segments. The inferred tectonic setting of the sulfide deposits was an early back-arc or interarc basin, which may have been related to transtensional tectonics.
APA, Harvard, Vancouver, ISO, and other styles
6

Kirkpatrick, James David. "The structural architecture of seismogenic faults, Sierra Nevada, California; implications for earthquake rupture processes." Thesis, University of Glasgow, 2008. http://theses.gla.ac.uk/179/.

Full text
Abstract:
Earthquake ruptures along tectonically active faults nucleate predominantly at depths of 5 to 12km in the crust, so the portions of faults that slip in these events cannot be directly observed. The geometry and composition of seismogenic faults controls the nucleation, propagation and termination of the earthquake rupture process. This study aims to place constraints on the geometry and composition of seismogenic faults by examining ancient faults exhumed from the depths at which earthquakes are observed to nucleate. Faults exposed in the Sierra Nevada, California, show that the internal architecture of earthquake faults is heterogeneous at a variety of scales. Field and microstructural observations are used to describe in detail the architecture of two pseudotachylyte-bearing fault systems in the Granite Pass region of Sequoia and Kings Canyon National Park; the Granite Pass fault (GPF) and associated faults, and the Glacier Lakes fault (GLF) and faults that splay from the GLF. The GPF and sub-parallel faults are 1 to 6.7km long with left-lateral strike-slip displacements up to 80m. The GPF and GPF-parallel faults have architectures that are heterogeneous along strike. They are composed of one to four fault core strands containing cataclasites and ultracataclasites that cross-cut early localized crystal-plastic deformation. Slip surfaces developed at the edges of, within and between fault cores are defined by pseudotachylytes and cataclasites with thicknesses of ~0.01 to 20mm. Fault-related subsidiary structures are developed on either side of fault cores, and comprise damage zones with widths orthogonal to the fault of up to 30m. The GLF and splay faults have architectures that are more homogeneous along strike. These faults are composed of a tabular volume of heavily fractured and altered host rock between approximately planar fault core strands. The fault cores are centimetres wide and contain cataclasites and foliated cataclasites that are cross-cut by pseudotachylytes. Fault-related damage is limited in extent to several metres beyond the bounding fault cores. The GLF contains additional cataclasites, ultracataclasites and pseudotachylytes in a fault core strand within the tabular zone of fractured rock. Thermochronologic analyses of the host rock granodiorite, combined with previously published palaeogeobarometry and apatite fission track data, define the temperature and pressure changes associated with cooling and exhumation of the pluton. The P-T conditions prevalent during the deformation history of the GPF fault system are evaluated by relating recrystallisation mechanisms in quartz to temperature, showing that the early stages of deformation occurred at temperatures of 450 to 600ºC. Dating of pseudotachylytes by the K-Ar isotopic method suggests subsequent brittle deformation took place at temperatures <350ºC and pressures ≤150MPa. A model for the architecture of the GPF architecture therefore has well constrained environmental controls, and should be transferrable to faults with comparable deformation histories. Small faults (cumulative displacements <1m) in the Mount Abbot Quadrangle, 55km north of Granite Pass, have been examined to illustrate the processes associated with the earliest stages of slip in the Sierra Nevada faults. The faults have branched or straight fault traces. Pseudotachylytes in branching faults show that these faults accumulated displacement in high velocity slip events, rather than by quasi-static fault growth. Branching faults without pseudotachylytes contain chlorite breccias interpreted to have formed in response to slip along faults with elevated pore fluid pressure. Straight faults also likely underwent slip events, but contain cataclased chlorite and epidote, suggesting low fluid pressures during slip. The small faults show that fluid-rock interactions are critical to fault geometry, and that lateral structural heterogeneity is established after small finite displacements. Field and thin section observations of exhumed seismogenic faults show that fault architecture and fault rock assemblage are critical to the earthquake rupture process. The heterogeneous composition of slip surfaces in the GPF faults imply that melt lubrication cannot account for all of the dynamic slip weakening as there are no continuous pseudotachylyte generation surfaces through the fault zones. Multiple slip weakening mechanisms must have been active during single rupture events. Slip weakening mechanisms also change at a given point on the fault in response to continued deformation. Splay faults at the GLF termination suggest that structural complexity observed at the terminations of fault surface traces can also be expected at depth. The off-fault damage at the termination of the GLF will change the bulk elastic properties of the host rock and must be accounted for in models of rupture propagation beyond fault terminations, or across geometrical discontinuities. Additionally, aftershock distributions and focal mechanisms may be controlled by the geometry of structures present at fault terminations.
APA, Harvard, Vancouver, ISO, and other styles
7

Samra, Charles P. "Structural and basin evolution of the western Gale Hills, Lake Mead Miocene extensional domain, Nevada." Thesis, Northern Arizona University, 2013. http://pqdtopen.proquest.com/#viewpdf?dispub=1543983.

Full text
Abstract:

This study focuses on the western Gale Hills located in the western portion of the Lake Mead domain in southern Nevada. The western Gale Hills preserve a record of the Miocene sedimentation and deformation related to the breakup of the hanging walls of the South Virgin-White Hills detachment fault and the Lime Ridge oblique, strike-slip fault of the Lake Mead fault system, the initiation of the right-lateral Las Vegas Valley shear zone in the western Lake Mead domain, and subsequent middle to late Miocene deformation. This study focuses on the lower Horse Spring Formation north of the Las Vegas Valley shear zone. To better understand the stratigraphy and deformation, a detailed geologic map (1:10,000 scale) was produced, data from primary and secondary structures were collected, and ash-fall tuff deposits were dated and correlated through 40Ar/39Ar geochronology and tephrachronology. The stratigraphy of the Gale Hills records the initial buttressing of the lower Thumb Member of the Horse Spring Formation onto pre-Tertiary topography. Deposition of the lower Thumb Member records a rapid transgression of the basin margin to the north and northwest across the majority of the Gale Hills. This time was period was then followed by a coarsening up interval and progradation of large alluvial fans in the middle to upper Thumb Member. A transition to a marginal clastic lake in the uppermost Thumb Member then abruptly changed to the Bitter Ridge Limestone algal lake.

Many studies have evaluated the exhumation history of the Gold Butte block in the eastern Lake Mead domain, which forms the footwall of the major South Virgin-White Hills detachment fault and the relationship with the Frenchman Mountain block. This study shows that the Frenchman Mountain block was just south of the Gale Hills during the early to peak stages of detachment faulting from ca. 17-14 Ma. Two new 40Ar/39Ar dates (15.35 Ma) from a prominent ash-fall tuff in the Thumb Member in the northern and southern regions of the western Gale Hills is also in the Frenchman Mountain block. In addition, new tephrachronology correlations have tied Proterozoic-clast debris flows in the western Gale Hills to Proterozoic-clast megabreccia deposits in the Frenchman Mountain block, indicating that the two areas were one connected basin during upper Thumb Member time.

This study suggests that the left-lateral Government Wash and Southern Gale Hills faults are reactivated northeast-striking, west-down normal faults that were in the correct orientation to be major Riedel prime shears (R') to the right-lateral Las Vegas Valley shear zone. Map and facies relationships show that the Thumb Member deposits were faulted locally during deposition at ca. 15.5 Ma, with increased fault activity and sedimentation rates throughout the Thumb Member after 15.35 Ma and before ∼14.5 Ma.

An analysis of structures in the western Gale Hills results in a new model of progressive clockwise rotation and faulting along the Las Vegas Valley shear zone that for the first time honors paleomagnetic results and accounts for all major faulting north of the shear zone. The model is primarily based on clockwise vertical-axis block rotation of domains between oblique left-lateral faults that curve progressively toward the Las Vegas Valley shear zone and terminate into major folds or areas of complex deformation. This model predicts that the western Gale Hills began as a north-northeast elongate block that was reduced in length and elongated in an east-west direction from about 20 to 14 km during translation and rotations. Most of this complex faulting occurred from ca. 13.8 to 8 Ma, after deposition of the Bitter Ridge Limestone.

APA, Harvard, Vancouver, ISO, and other styles
8

Foy, Travis A. "Quaternary faulting in Clayton Valley, Nevada: implications for distributed deformation in the Eastern California shear zone-walker lane." Thesis, Georgia Institute of Technology, 2011. http://hdl.handle.net/1853/39561.

Full text
Abstract:
The eastern California shear zone (ECSZ) and Walker Lane belt represent an important inland component of the Pacific-North America plate boundary. Current geodetic data indicate accumulation of transtensional shear at a rate of ~9.2 ± 0.3 mm/yr across the region, more than double the total geologic rate (<3.5 mm/yr) for faults in the northern ECSZ over the late Pleistocene [Bennett et al., 2003, Kirby et al., 2006, Lee et al., 2009, Frankel et al., 2007]. Unraveling the strain puzzle of the Walker Lane is therefore essential to understanding both how deformation is distributed through the lithosphere along this transtensional part of the Pacific-North America plate boundary and how the plate boundary is evolving through time. The observed mismatch between geodetic and geologic slip rates in the central Walker Lane is characteristic of other active tectonic settings, including the nearby Mojave segment of the ECSZ [Oskin et al., 2008] and the Altyn Tagh fault in China [Cowgill, 2007]. In each case, lack of fault slip data spanning multiple temporal and spatial scales hinders interpretation of fault interactions and their implications for lithospheric dynamics. The discrepancy between geodetic and geologic slip rates in the central Walker Lane indicates that if strain rates have remained constant since the late Pleistocene [e.g. Frankel et al., in press], then the "missing" strain is distributed on structures other than the two major dextral faults at this latitude (Death Valley-Fish Lake Valley fault and White Mountains fault). Otherwise the region could presently be experiencing a strain transient similar to that of the nearby Mojave section of the ECSZ [e.g., Oskin et al., 2008], or the rate of strain accumulation could actually increasing over the late Pleistocene [e.g. Reheis and Sawyer, 1997; Hoeft and Frankel, 2010]. The Silver Peak-Lone Mountain extensional complex (SPLM), to which the Clayton Valley faults belong, is the prime candidate to account for the "missing" strain. The down-to-the-northwest orientation of the SPLM faults makes them the most kinematically suitable structures to accommodate the regional pattern of NW-SE dextral shear. We use differential GPS to measure fault offset and terrestrial cosmogenic nuclide (TCN) geochronology to date offset landforms. Using these tools, we measure extension rates that are time-invariant, ranging from 0.1 ± 0.1 to 0.3 ± 0.1 mm/yr for fault dips of 30° and 60°. These rates are not high enough to account for the discrepancy between geologic and geodetic data in the ECSZ-Walker Lane transition zone. Based on geologic mapping and previously published geophysical data [Davis, 1981; Zampirro, 2005], deformation through Clayton Valley appears to be very widely-distributed. The diffuse nature of deformation leads to geologic slip rates that are underestimated due to the effects of off-fault deformation and unrecognized fault strands. Our results from Clayton Valley suggest that the discrepancy between geodetic and geologic strain rates at the latitude of the northern ECSZ is a result of long-term geologic rates that are underestimated. If the true geologic rates could be calculated, they would likely be significantly higher and therefore in closer agreement with geodetic data, as is the case everywhere else in the ECSZ north of the Garlock fault [Frankel et al., 2007a, in press; Kirby et al., 2008; Lee et al., 2009a].
APA, Harvard, Vancouver, ISO, and other styles
9

Hammond, K. Jill. "Structural and Geochemical Analyses of Disseminated-Gold Deposits, Bald Mountain-Alligator Ridge District, Nevada: Insights into Fault-Zone Architecture and Its Effect on Mineralization." DigitalCommons@USU, 2001. https://digitalcommons.usu.edu/etd/6719.

Full text
Abstract:
Structural and geochemical analyses of the Top and Casino deposits, Bald Mountain-Alligator Ridge district, Nevada, were conducted to determine how structures affected gold deposition in Carlin-type deposit s. We also examined how permeability changed over time in a fault that cuts siltstone-dominated sedimentary rocks. The association of gold and related arsenic with faults at the margins of a Jurassic pluton and sedimentary rocks suggests that ore fluids migrated along faults and fracture s. Permeability of the faults changed over time within the Casino deposit, where the ore-controlling fault was a distributed conduit in the early stages of mineralization but a barrier and a localized conduit a t opposite ends of the deposit during later stages. Results indicate that faults may significantly influence patterns of ore deposition and change character over deposit-scale distances, and continued slip along faults may create clay-rich low-permeability faults that are mineralized during early stages of development.
APA, Harvard, Vancouver, ISO, and other styles
10

Vice, Garrett S. "Structural controls of the Astor Pass-Terraced Hills geothermal system in a region of strain transfer in the western Great Basin, northwestern Nevada." abstract and full text PDF (UNR users only), 2008. http://0-gateway.proquest.com.innopac.library.unr.edu/openurl?url_ver=Z39.88-2004&rft_val_fmt=info:ofi/fmt:kev:mtx:dissertation&res_dat=xri:pqdiss&rft_dat=xri:pqdiss:1456425.

Full text
APA, Harvard, Vancouver, ISO, and other styles
More sources

Books on the topic "Structural Nevada"

1

Cole, James C. Structural relationships of pre-Tertiary rocks in the Nevada Test Site region, southern Nevada. Washington: U.S. G.P.O., 1999.

Find full text
APA, Harvard, Vancouver, ISO, and other styles
2

Peters, S. G. Structural transect across the southern Carlin trend, Elko and Eureka counties, Nevada. [Reston, Va.?]: U.S. Dept. of the Interior, U.S. Geological Survey, 1997.

Find full text
APA, Harvard, Vancouver, ISO, and other styles
3

United States Geological Survey. Geophysical framework of the southwestern Nevada volcanic field and hydrogeologic implications. Denver, CO: U.S. Geological Survey, 2000.

Find full text
APA, Harvard, Vancouver, ISO, and other styles
4

Peters, S. G. Structural transect across the central Carlin trend, Eureka County, Nevada. [Reston, Va.?]: U.S. Dept. of the Interior, U.S. Geological Survey, 1997.

Find full text
APA, Harvard, Vancouver, ISO, and other styles
5

Peters, S. G. Structural transect across the north-central Carlin trend, Eureka County, Nevada. [Reston, Va.?]: U.S. Dept. of the Interior, U.S. Geological Survey, 1997.

Find full text
APA, Harvard, Vancouver, ISO, and other styles
6

Society, Nevada Petroleum. Structural and stratigraphic investigations and petroleum potential of Nevada, with special emphasis south of the Railroad Valley producing trend: Nevada Petroleum Society 1994 conference volume II. Edited by Dobbs Steven W and Taylor Wanda J. Reno, Nev: The Society, 1994.

Find full text
APA, Harvard, Vancouver, ISO, and other styles
7

1958-, Wernicke Brian P., and Geological Society of America, eds. Basin and range extensional tectonics near the latitude of Las Vegas, Nevada. Boulder, Colo: Geological Society of America, 1990.

Find full text
APA, Harvard, Vancouver, ISO, and other styles
8

S, Oldow John, and Cashman Patricia Hughes, eds. Late Cenozoic structure and evolution of the Great Basin: Sierra Nevada transition. Boulder, Colo: Geological Society of America, 2009.

Find full text
APA, Harvard, Vancouver, ISO, and other styles
9

Langenheim, Victoria E. Ground magnetic studies along a regional seismic-reflection profile across Bare Mountain, Crater Flat, and Yucca Mountain, Nevada. Menlo Park, Calif: Dept. of the Interior, U.S. Geological Survey, 1995.

Find full text
APA, Harvard, Vancouver, ISO, and other styles
10

Bell, John W. Surficial geology, hydrology, and Late Quaternary tectonics of the IXL Canyon area, Nevada: As related to the 1954 Dixie Valley earthquake. Reno, NV: Nevada Bureau of Mines & Geology, University of Nevada-Reno, 1987.

Find full text
APA, Harvard, Vancouver, ISO, and other styles
More sources

Book chapters on the topic "Structural Nevada"

1

de Saint Blanquat, Michel, and Basil Tikoff. "Development of Magmatic to Solid-State Fabrics during Syntectonic Emplacement of the Mono Creek Granite, Sierra Nevada Batholith." In Petrology and Structural Geology, 231–52. Dordrecht: Springer Netherlands, 1997. http://dx.doi.org/10.1007/978-94-017-1717-5_15.

Full text
APA, Harvard, Vancouver, ISO, and other styles
2

Blackburn, Paul W., John B. Fisher, William E. Dollarhide, Douglas J. Merkler, Joseph V. Chiaretti, and James G. Bockheim. "Diagnostic Horizons and Taxonomic Structure of Nevada Soils." In World Soils Book Series, 59–74. Cham: Springer International Publishing, 2020. http://dx.doi.org/10.1007/978-3-030-53157-7_6.

Full text
APA, Harvard, Vancouver, ISO, and other styles
3

Hill, D. P., and L. C. Pakiser. "Crustal Structure Between the Nevada Test Site and Boise, Idaho,From Seismic-Refraction Measurements." In The Earth Beneath the Continents, 391–419. Washington, D. C.: American Geophysical Union, 2013. http://dx.doi.org/10.1029/gm010p0391.

Full text
APA, Harvard, Vancouver, ISO, and other styles
4

Patrick, David W., and Calvin F. Miller. "Processes in a Composite, Recharging Magma Chamber: Evidence from Magmatic Structures in the Aztec Wash Pluton, Nevada." In Igneous Petrology, 121–35. London: CRC Press, 2021. http://dx.doi.org/10.1201/9780429070877-10.

Full text
APA, Harvard, Vancouver, ISO, and other styles
5

Carbonell, Ramon, and Scott B. Smithson. "Crustal anisotropy and the structure of the Mohorovicic discontinuity in western Nevada of the basin and range province." In Continental Lithosphere: Deep Seismic Reflections, 31–38. Washington, D. C.: American Geophysical Union, 1991. http://dx.doi.org/10.1029/gd022p0031.

Full text
APA, Harvard, Vancouver, ISO, and other styles
6

Berezina, Nadya A., and Vadim E. Panov. "Distribution, population structure and salinity tolerance of the invasive amphipod Gmelinoides fasciatus (Stebbing) in the Neva Estuary (Gulf of Finland, Baltic Sea)." In Biology of the Baltic Sea, 199–206. Dordrecht: Springer Netherlands, 2004. http://dx.doi.org/10.1007/978-94-017-0920-0_18.

Full text
APA, Harvard, Vancouver, ISO, and other styles
7

Orlova, Marina I., and Vadim E. Panov. "Establishment of the zebra mussel, Dreissena polymorpha (Pallas), in the Neva Estuary (Gulf of Finland, Baltic Sea): distribution, population structure and possible impact on local unionid bivalves." In Biology of the Baltic Sea, 207–17. Dordrecht: Springer Netherlands, 2004. http://dx.doi.org/10.1007/978-94-017-0920-0_19.

Full text
APA, Harvard, Vancouver, ISO, and other styles
8

Whitmore, Ross J., Patricia H. Cashman, and Daniel M. Sturmer. "Structures at Buck Mountain, Nevada: Establishing the Southeastern Extent of Mid-Pennsylvanian Tectonism." In Late Paleozoic and Early Mesozoic Tectonostratigraphy and Biostratigraphy of Western Pangea, 102–13. SEPM (Society for Sedimentary Geology), 2022. http://dx.doi.org/10.2110/sepmsp.113.06.

Full text
Abstract:
This paper reports the structural and stratigraphic history of Buck Mountain, Nevada, and its regional significance in the development of southwestern Laurentia during the late Paleozoic. The two distinct generations of folding have similar style and/or timing to other fold sets in late Paleozoic strata of northern Nevada. Unconformities in the upper Paleozoic strata at Buck Mountain are consistent with unconformities documented in northern and east-central Nevada. Northwest-vergent folds (F1) in the Morrowan–Atokan Ely Limestone are erosionally truncated and unconformably overlain by the middle Desmoinesian Hogan Formation and middle Wolfcampian (Sakmarian) Upper Strathearn Formation. This upper Paleozoic stratigraphic package was subsequently refolded by the Buck Mountain Syncline and associated mesoscale folds (F2). F2 folds lack tight age control but are interpreted to be associated with the Cretaceous central Nevada thrust belt. Critically, none of these structures are localized above or below low-angle faults. The unconformity between the Ely and Hogan formations is consistent with the C5 regional unconformity. Importantly, it constrains the age of northwest-vergent deformation on Buck Mountain. West-vergent folds and west-directed thrusts are documented at several locations in northern and east-central Nevada, but because of the dominance of the C6 unconformity and/or lack of robust age control, the age of these structures has not been tightly constrained. The evidence at Buck Mountain indicates that west-vergent structures predate the C5 unconformity. Buck Mountain is important because it: (1) precisely brackets the age of west-vergent deformation in Nevada to pre–mid-Desmoinesian (sub C5-unconformity) and (2) defines a southeastern edge to the late Paleozoic west-vergent deformation in northern and east-central Nevada.
APA, Harvard, Vancouver, ISO, and other styles
9

Russo, Angela G., Wanda J. Taylor, and Patricia H. Cashman. "Late Paleozoic Shortening in South-Central Nevada and Regional Correlations of Major Pre-Sevier Structures." In Late Paleozoic and Early Mesozoic Tectonostratigraphy and Biostratigraphy of Western Pangea, 114–26. SEPM (Society for Sedimentary Geology), 2022. http://dx.doi.org/10.2110/sepmsp.113.05.

Full text
Abstract:
Recent tectonic reinterpretations of the Late Paleozoic Southwest Laurentian margins recognize widespread Late Paleozoic deformation as a critical component in the boundary region development. Overprinted late Paleozoic structures record repeated shortening events in both northern and southern Nevada, but spatial and temporal data are currently lacking to resolve the evolution of this margin. The Timpahute Range, south-central Nevada, bridges part of the spatial gap between previous detailed studies of Late Paleozoic deformation. The purpose here is to (1) evaluate structures in the area that do not appear to fit with recognized Sevier hinterland structures (the Central Nevada thrust belt [CNTB]) and (2) consider whether these contractional structures may be Late Paleozoic and possibly link, or not, structures to the north and south. New mapping in the Timpahute Range documents four geometrically or kinematically distinct sets of structures: Tempiute Ridge folds, Schofield Pass fault zone (SPFZ), structures of the CNTB, and Cenozoic extensional faults. The first three are interpreted to represent separate shortening events based on cross-cutting relations and differences in orientations of the Tempiute Ridge folds and SPFZ (north [N]), and structures of the CNTB (northwest [NW]). The Tempiute Ridge folds represent the oldest event, D1. These folds are large, trend N and verge east (E). The SPFZ is west (W)-vergent, cuts across the limb of a D1 fold and represents D2. The SPFZ is interpreted to be older than the CNTB structures, D3, based on positions of fault cut offs, and differences in footwall and hangingwall facies. All of the shortening events predate the newly dated 102.9 ± 3.2 Ma Lincoln stock and its contact metamorphic aureole. New and previous correlations suggest that a belt of Permian deformation extends from southeast (SE) California northward at least to the Timpahute Range. The Tempiute Ridge folds and SPFZ have the same distinctive geometries, styles, and kinematics as structures in the Nevada National Security Site. The mountain-size, E-vergent Tempiute Ridge folds and the W-vergent SPFZ correlate to structures associated with the Belted Range thrust and the W-vergent CP thrust, respectively. The Belted Range thrust previously has been correlated southward into the Death Valley region. Thus, convergence created large-amplitude folds and thrusts for ~200 km along strike. Structures of this age are exposed in northern Nevada but are smaller. These new relations fill a data gap and suggest differences in the size and structural style of Permian structures along strike and corresponding variations in the plate boundary configuration.
APA, Harvard, Vancouver, ISO, and other styles
10

Dobak, Paul J., François Robert, Shaun L. L. Barker, Jeremy R. Vaughan, and Douglas Eck. "Chapter 15: Goldstrike Gold System, North Carlin Trend, Nevada, USA." In Geology of the World’s Major Gold Deposits and Provinces, 313–34. Society of Economic Geologists, 2020. http://dx.doi.org/10.5382/sp.23.15.

Full text
Abstract:
Abstract The Eocene Goldstrike system on the Carlin Trend in Nevada is the largest known Carlin-type gold system, with an endowment of 58 million ounces (Moz) distributed among several coalesced deposits in a structural window of gently dipping carbonate rocks below the regional Roberts Mountains thrust. The 3.5- × 2.5-km Goldstrike system is bounded to the east by the Post normal fault system and to the south by the Jurassic Goldstrike diorite stock and is partly hosted in the favorable slope-facies apron of the Bootstrap reef margin that passes through the system. The carbonate and clastic sedimentary sequence is openly folded, cut by sets of reverse and normal faults, and intruded by the Jurassic Goldstrike stock and swarms of Jurassic and Eocene dikes, establishing the structural architecture that controlled fluid flow and distribution of Eocene mineralization. A proximal zone of permeability-enhancing decarbonatization with anomalous gold (&gt;0.1 ppm) extends a few hundreds of meters beyond the ore footprint and lies within a carbonate δ18O depletion anomaly extending ~1.4 km farther outboard. The full extent of the larger hydrothermal system hosting Goldstrike and adjacent deposits on the northern Carlin Trend is outlined by a 20- × 40-km thermal anomaly defined by apatite fission-track analyses. The bulk of the mineralization is hosted in decarbonatized sedimentary units with elevated iron contents and abundant diagenetic pyrite relative to background. Gold is associated with elevated concentrations of As, Tl, Hg, and Sb, and occurs in micron-sized arsenian pyrite grains or in arsenian pyrite overgrowths on older, principally diagenetic pyrite, with sulfidation of available iron as the main gold precipitation mechanism. The intersection of a swarm of Jurassic lamprophyre dikes with the edge of the limestone reef provided a favorable deeply penetrating structural conduit within which a Jurassic stock acted as a structural buttress, whereas the reef’s slope-facies apron of carbonate units, with high available iron content, provided a fertile setting for Carlin-type mineralization. The onset of Eocene extension coupled with a southwestward-sweeping Cenozoic magmatic front acted as the trigger for main-stage gold mineralization at 40 to 39 Ma. All these factors contributed to the exceptional size and grade of Goldstrike.
APA, Harvard, Vancouver, ISO, and other styles

Conference papers on the topic "Structural Nevada"

1

Opfer, Russell P., and Jeff A. Dark. "Application of GravStat to seismic statics and structural correction in Nevada." In SEG Technical Program Expanded Abstracts 1989. Society of Exploration Geophysicists, 1989. http://dx.doi.org/10.1190/1.1889503.

Full text
APA, Harvard, Vancouver, ISO, and other styles
2

Sadowski, Andrew J., and James E. Faulds. "STRUCTURAL CONTROLS OF THE BLACK WARRIOR BLIND GEOTHERMAL SYSTEM, TRUCKEE RANGE, NORTHWESTERN NEVADA." In GSA Annual Meeting in Denver, Colorado, USA - 2016. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016am-283560.

Full text
APA, Harvard, Vancouver, ISO, and other styles
3

Gesualdo, Anthony M., Zeynep Baran, Alvis L. Lisenbee, Colin J. Paterson, and Kelli A. McCormick. "STRUCTURAL CONTROLS ON MINERALIZATION AND FAULT REACTIVATION AT MARIGOLD MINE, HUMBOLDT COUNTY, NEVADA." In GSA Annual Meeting in Denver, Colorado, USA - 2016. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016am-282356.

Full text
APA, Harvard, Vancouver, ISO, and other styles
4

"Relationships Between Deterioration and Structural Performance: Three Case Studies." In "SP-154: Advances in Concrete Technology - Proceeding Second CANMET/ ACI International Symposium - Las Vegas, Nevada, USA". American Concrete Institute, 1995. http://dx.doi.org/10.14359/990.

Full text
APA, Harvard, Vancouver, ISO, and other styles
5

Evans, Michael. "STRUCTURAL DEVELOPMENT AND TECTONIC ROLE OF THE ARROWHEAD MINE FAULT, PAHRANAGAT SHEAR ZONE, NEVADA." In 112th Annual GSA Cordilleran Section Meeting. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016cd-274605.

Full text
APA, Harvard, Vancouver, ISO, and other styles
6

Pearson, William C. "Three‐dimensional gravity modeling in Newark Valley, Nevada: A structural interpretation from gravity data." In SEG Technical Program Expanded Abstracts 1986. Society of Exploration Geophysicists, 1986. http://dx.doi.org/10.1190/1.1893181.

Full text
APA, Harvard, Vancouver, ISO, and other styles
7

Henry, Christopher D. "STRUCTURAL AND TOPOGRAPHIC EVOLUTION OF THE SIERRA NEVADA BASED ON FAR-TRAVELED OLIGOCENE-MIOCENE IGNIMBRITES." In Cordilleran Section-117th Annual Meeting-2021. Geological Society of America, 2021. http://dx.doi.org/10.1130/abs/2021cd-363131.

Full text
APA, Harvard, Vancouver, ISO, and other styles
8

James, Randy J., Kenneth Jaquay, and Michael J. Anderson. "Design by Analysis of Waste Packages at Yucca Mountain for Impact Loads." In 17th International Conference on Nuclear Engineering. ASMEDC, 2009. http://dx.doi.org/10.1115/icone17-75355.

Full text
Abstract:
The proposed geologic repository under development at Yucca Mountain, Nevada, will employ multiple shell metallic containers (waste packages) for the disposal of nuclear waste. The waste packages represent a primary engineered barrier for protection and containment of the radioactive waste, and the design of these containers must consider a variety of structural conditions to insure structural integrity. Some of the more challenging conditions for structural integrity involve severe impact loading due to hypothesized event sequences, such as drops or collisions during transport and placement. Due to interactions between the various components leading to complex structural response during an impact sequence, nonlinear explicit dynamic simulations and highly refined models are employed to qualify the design for these severe impact loads. This paper summarizes the Design by Analysis methodologies employed for qualification of waste package design under impact loading and provides several illustrative examples using these methods. Example evaluations include a collision of a waste package by the Transport and Emplacement Vehicle (TEV) and two scenarios due to seismic events, including WP impact within the TEV and impact by falling rock. The examples are intended to illustrate the stringent Design by Analysis methods employed and also highlight the scope of structural conditions included in the design basis for waste packages to be used for proposed nuclear waste storage at Yucca Mountain.
APA, Harvard, Vancouver, ISO, and other styles
9

""Long-Term Durability of Silica Fume Structural Concrete, Shotcrete, Grout, and Slab Overlays"." In "SP-154: Advances in Concrete Technology - Proceeding Second CANMET/ ACI International Symposium - Las Vegas, Nevada, USA". American Concrete Institute, 1995. http://dx.doi.org/10.14359/970.

Full text
APA, Harvard, Vancouver, ISO, and other styles
10

Kusek, Stephen, Michael Caraway, Timothy McFarland, Matthew Lynn, Aaron Sahm, Robert Boehm, and Omer Ayubi. "Initial Testing of the HiTek Solar Tracking Monitor." In ASME 2012 6th International Conference on Energy Sustainability collocated with the ASME 2012 10th International Conference on Fuel Cell Science, Engineering and Technology. American Society of Mechanical Engineers, 2012. http://dx.doi.org/10.1115/es2012-91204.

Full text
Abstract:
HiTek Services, Inc. has designed, fabricated, and tested a solar monitoring system that can measure the sun’s position with high accuracy. Sun position data, measured by the University of Nevada, Las Vegas Center for Energy Research, is presented showing that the instrument’s accuracy is better than 0.004 degrees (one σ). A histogram is presented showing that nearly 100 % of the time the measurement error is less than 0.008 degrees. The capability of using multiple sun monitors with synchronized data collection to measure the structural bending of one part of a tracking structure relative to another part of the structure is discussed and data are presented. Other operating features, such as being self-contained, no external cables required, and the ability to record data for a week without recharging the batteries, are discussed.
APA, Harvard, Vancouver, ISO, and other styles

Reports on the topic "Structural Nevada"

1

Hudson, M. R. Structural geology of the French Peak accommodation zone, Nevada Test Site, southwestern Nevada. Office of Scientific and Technical Information (OSTI), December 1997. http://dx.doi.org/10.2172/573191.

Full text
APA, Harvard, Vancouver, ISO, and other styles
2

Cashman, P. H., and J. C. Cole. Structural relationships of pre-Tertiary rocks in the Nevada Test Site region, southern Nevada. Office of Scientific and Technical Information (OSTI), August 1999. http://dx.doi.org/10.2172/10451.

Full text
APA, Harvard, Vancouver, ISO, and other styles
3

Cole, J. C. Major structural controls on the distribution of pre-Tertiary rocks, Nevada Test Site vicinity, southern Nevada. Office of Scientific and Technical Information (OSTI), October 1998. http://dx.doi.org/10.2172/1060.

Full text
APA, Harvard, Vancouver, ISO, and other styles
4

J. King. CHARACTERIZE FRAMEWORK FOR SEISMICITY AND STRUCTURAL DEFORMATION AT YUCCA MOUNTAIN, NEVADA. Office of Scientific and Technical Information (OSTI), February 2004. http://dx.doi.org/10.2172/859408.

Full text
APA, Harvard, Vancouver, ISO, and other styles
5

Caskey, S. John. Mesozoic and Cenozoic structural geology of the CP Hills, Nevada Test Site, Nye County, Nevada; and regional implications. Office of Scientific and Technical Information (OSTI), August 1991. http://dx.doi.org/10.2172/138733.

Full text
APA, Harvard, Vancouver, ISO, and other styles
6

McCallen, D., and S. Larsen. Nevada - A Simulation Environment for Regional Estimation of Ground Motion and Structural Response. Office of Scientific and Technical Information (OSTI), March 2003. http://dx.doi.org/10.2172/15004876.

Full text
APA, Harvard, Vancouver, ISO, and other styles
7

Carter Krogh, K. E., and G. A. Valentine. Structural control on basaltic dike and sill emplacement, Paiute Ridge mafic intrusion complex, southern Nevada. Office of Scientific and Technical Information (OSTI), August 1996. http://dx.doi.org/10.2172/373820.

Full text
APA, Harvard, Vancouver, ISO, and other styles
8

Theodore H. Asch, Brian D. Rodriguez, Jay A. Sampson, Erin L. Wallin, and and Jackie M. Williams. Deep Resistivity Structure of Yucca Flat, Nevada Test Site, Nevada. Office of Scientific and Technical Information (OSTI), September 2006. http://dx.doi.org/10.2172/894298.

Full text
APA, Harvard, Vancouver, ISO, and other styles
9

Ladkany, S. G., and B. R. Kniss. A study of a container for long term storage of high level waste using finite elements. Task B.1, Structural analysis and design: The Waste Package Project at The University of Nevada, Las Vegas. Office of Scientific and Technical Information (OSTI), June 1992. http://dx.doi.org/10.2172/10146783.

Full text
APA, Harvard, Vancouver, ISO, and other styles
10

Theodore H. Asch, Brian D. Rodriguez, Jay A. Sampson, Jackie M. Williams, and Maryla Deszcz-Pan. Deep Resistivity Structure of Rainier Mesa-Shoshone Mountain, Nevada Test Site, Nevada. Office of Scientific and Technical Information (OSTI), December 2006. http://dx.doi.org/10.2172/896251.

Full text
APA, Harvard, Vancouver, ISO, and other styles
You might also be interested in the extended bibliographies on the topic 'Structural Nevada' for particular source types:
Journal articles Dissertations / Theses Books
We offer discounts on all premium plans for authors whose works are included in thematic literature selections. Contact us to get a unique promo code!

To the bibliography