2 edition of Late Cenozoic structure of the central Wassuk Range, Mineral County, Nevada found in the catalog.
Late Cenozoic structure of the central Wassuk Range, Mineral County, Nevada
Jana L. McIntyre
Written in English
|Statement||by Jana L. McIntyre.|
|The Physical Object|
|Pagination||107 leaves, bound :|
|Number of Pages||107|
Singatse Range toward the Buckskin Range. More recent published mapping in the area includes work to the west in the Buckskin Range (e.g., Lipske and Dilles, ) and eastward into the Wassuk Range along the northeastern (McIntyre, ; Dilles, ) and southeastern and southern (Surpless, , ) edges of the district. Hawthorne/Wassuk Range area, Nevada, $, NSF Tectonics. Timing and Kinematics of Cenozoic of E-W Extension in Central Tibet Transition in the Strain Field of the Tibetan Plateau. Supplement $21, Apache Egypt Oil Contract. Thermochronometric Investigation of the SOKAR-1X Unconformity. $69,
Geology and mineral resources of the North-Central Idaho Sagebrush Focal Area: Chapter C in Mineral resources of the Sagebrush Focal Areas of Idaho, Montana, Nevada, Oregon, Utah, and Wyoming Info Spatial database of mining-related features in at selected phosphate mines, Bannock, Bear Lake, Bingham, and Caribou Counties, Idaho. Thomson SN () Late cenozoic geomorphic and tectonic evolution of the Patagonian Andes between latitudes 42 S and 46 S: an appraisal based on fission-track results from the transpressional intra-arc Liquiñe-Ofqui fault zone. Geol Soc Am Bull – Google Scholar.
Turquoise is an opaque, blue-to-green mineral that is a hydrated phosphate of copper and aluminium, with the chemical formula Cu Al 6 (PO 4) 4 8 4H 2 is rare and valuable in finer grades and has been prized as a gemstone and ornamental stone for thousands of years owing to its unique hue. Like most other opaque gems, turquoise has been devalued by the introduction onto the market of. Active faulting in the Walker Lane Active faulting in the Walker Lane Wesnousky, Steven G. Deformation across the San Andreas and Walker Lane fault systems accounts for most relative Pacific–North American transform plate motion. The Walker Lane is composed of discontinuous sets of right‐slip faults that are located to the east and strike approximately parallel to .
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At least % nearly east-west extension of late Cenozoic age has been accommodated by down-to-the-east normal and oblique-slip faults in the central Wassuk Range. One northwest striking, right-lateral strike-slip fault probably contributes an additional component of WNW-ESE slip.
Late Cenozoic structure of the central Wassuk Range, Mineral County, Nevada At least % nearly east-west extension of late Cenozoic age has been accommodated by down-to-the-east normal and oblique-slip faults in the central Wassuk Range.
One northwest striking, right-lateral strike-slip fault probably contributes an additional. Title: Late Cenozoic Structure of the Central Wassuk Range. Mineral County, Nevada. Signature redacted for privacy. Abstract approved: At least % nearly east-west extension of late Cenozoic age has been accommodated by down-to-the-east normal and oblique-slip faults in the central Wassuk Range.
the central Wassuk Range fault block, Hawthorne, Nevada, in an attempt to illustrate the utility of this approach. Geologic and tectonic History The Wassuk Range (Figure 2.) is a nearly N-S trending moun-tain range on the western margin of the Basin and Range Province at the latitude of Lake Tahoe.
The entire range is characterizedCited by: 2. The Wassuk Range of west-central Nevada lies within the tectonically active western margin of the GB (Fig.
This region is geologically complex due largely Late Cenozoic structure of the central Wassuk Range competing forces throughout the. Apatite fission track and (U‐Th)/He thermochronological data provide new constraints on the timing of faulting and exhumation of the Wassuk Range, western Nevada, where east dipping normal faults h.
The total extension accommodated across the central Wassuk Range since the middle Miocene is >%, with only a brief period of dextral fault activity during the late Miocene. Late Cenozoic Structure and Evolution of the Great Basin – Sierra Nevada Transition Edited by J.S.
Oldow, University of Idaho and P. Cashman, University of Nevada, Reno Volume Focus: The transition between the Sierra Nevada and the Great Basin has received substantial attention over the. Upper‐Crustal Thermal Structure of the Southern Wassuk Range  The WR and PGH were part of the Sierra Nevada prior to middle Miocene extension and therefore probably experienced a similar pre‐extensional thermal history and post‐Cretaceous geothermal gradient of.
The lofty Wassuk Range, with up to m of relief, bounds the basin on the west, and the lower-relief (~Range occurs on the east (Fig. The Gillis Range principally consists of complexly faulted Triassic-Jurassic metavoleanic sequences unconformably overlain by Oligo-Miocene ash- flow tuff intervals (Hardyman, ).
The Walker Lake basin is a complex half-graben, bound on the west by the Wassuk Range-front fault system and defined to the east by a broad, gently west-dipping ramp, cut locally by west-dipping antithetic faults ().Within the map area, the Wassuk Range-front fault bifurcates into two major strands from the Lucky Boy Mine area to the mouth of Cat Canyon (Faults A and B1, Fig.
Molinari, Mark Philip,Late Cenozoic geology and tectonics of Stewart and Monte Cristo valleys, west-central Nevada [M.S.]: Univ. Nevada, Reno, p. Mollazal, Yazdan,Petrology and petrography of Ely Limestone in part of eastern Great Basin [M.S.]: Brigham Young Univ. Timing and Kinematics of Cenozoic of E-W Extension in central Tibet Important Transition in the Strain Field of the Tibetan Plateau.
$, - DOE Geothermal Technologies Program. Novel Coupled Thermochronometric and Geochemical Investigation of Blind Geothermal Resources in Fault- Controlled Dilational Corners, Dixie Valley, Nevada. The amount of late Cenozoic extension across the Great Basin is strongly heterogeneous, and in the region of the southern arc segment varies from ∼10% (northeast California–northwest Nevada; Colgan et al., ) to >% (Yerington district–northern Wassuk Range; Proffett, ; Dilles and Gans, ).
Fault ID: Refers to fault numbers WL11A, WL11B, and WL11C (Wassuk Range fault system) of dePolo ( #). County(s) and State(s) LYON COUNTY, NEVADA MINERAL COUNTY, NEVADA: Physiographic province(s) BASIN AND RANGE: Reliability. During the late Pleistocene, the absence of such information indicates that ponderosa pine forest was nearly or entirely absent from the northern and central Rockies, the Great Basin, the Mojave Desert, the Colorado Plateau, and the Chihuahuan Desert (Wells, a; Van Devender et al., ; Thompson, ; Anderson et al., ).
Late Eocene extension may have contributed more extensional strain than the mid-Miocene event in other parts of the Great Basin, including areas of east-central Nevada that are south of Spruce Mountain, such as the northern Egan Range and the Robinson district (Gans and Miller, ; Gans et al.,).
Even in areas where the magnitude. Dohrenwend, J.C.,Map showing late Cenozoic faults in the Walker Lake 1° by 2° quadrangle, Nevada-California: U.S. Geological Survey Miscellaneous Field Studies Map MFD, 1. Hook, Donald L. Late Cenozoic stratigraphy and structure of a part of the Walnut Grove Basin, Yavapai County, Arizona M.S.
50p. Horstman, Kevin Charles Geological, remote sensing, and geophysical investigation of the greater Arivaca region, Pima and Santa Cruz Counties, Arizona Ph.D. NBMG A mineral inventory of the Nevada Test Site and portionsof Nellis Bombing and Gunnery Range, southern Nye County, Nevada, by J.
Quade, J. Tingley, J. Bentz, and P. Smith. NBMG Reconnaissance Geochemical Assessment of Mineral Resources in Rough Hills WSA (NV) Elko County, Nevada, by J. Quade and J. Tingley, p. (). Cenozoic deformation along the Sierra Nevada province and Basin and Range province boundary.
(). Cenozoic geology of the Yerington district, Nevada, and implications for the nature and origin of Basin and Range faulting. (). Change in the size of Walker lake during the past years. (). Changes in meander morphology.Halleck is an unincorporated community in central Elko County, northeastern Nevada, in the Western United States.
Thorne: Thorne, Nevada is located in Mineral County, Nevada, at 38°32'4\" North, °38'28\" West (, ). Etna: Etna is an Unincorporated community in Lincoln County, Nevada. It lies at an elevation of feet.Fitzgerald PG, Stump E, Redfield TF () Late Cenozoic uplift of Denali and its relation to relative plate motion and fault morphology.
Science ()– CrossRef Google Scholar Fitzgerald PG, Sorkhabi RB, Redfield TF, Stump E () Uplift and denudation of the central Alaska Range: a case study in the use of apatite fission track.