Tertiary volcanic stratigraphy and paleotopography of the Diamond and Fort Sage Mountains: Constraining slip along the Honey Lake fault zone in the northern Walker Lane, northeastern California and western Nevada

Author(s):  
Nicholas H Hinz ◽  
James E Faulds ◽  
Christopher D Henry
2020 ◽  
Author(s):  
Zachery M. Lifton

Field photographs, stratigraphic columns, displacement modeling results, depth profile modeling results, and slip rate modeling results.


2020 ◽  
Author(s):  
Zachery M. Lifton

Field photographs, stratigraphic columns, displacement modeling results, depth profile modeling results, and slip rate modeling results.


2014 ◽  
Vol 119 (6) ◽  
pp. 5014-5032 ◽  
Author(s):  
Ryan D. Gold ◽  
Richard W. Briggs ◽  
Stephen F. Personius ◽  
Anthony J. Crone ◽  
Shannon A. Mahan ◽  
...  

2020 ◽  
Author(s):  
J. Lee ◽  
et al.

Figure 2. Layer A. Shaded relief map showing major Quaternary faults in central Walker Lane, Mina deflection, northern Eastern California shear zone, and western Basin and Range Province. Heavy black arrow in the northwest corner of the map shows the present-day azimuth of motion of the Sierra Nevada block with respect to the central Great Basin (SN-CBG) (Bennett et al., 2003). Fault abbreviations: APHF—Agai Pah Hills fault; BSF—Benton Spring fault; CF—Coaldale fault; CVF—Clayton Valley fault; EIFZ—Eastern Inyo fault zone; EPF—Emigrant Peak fault; FLVFCDV—Fish Lake Valley–Furnace Creek–Death Valley fault zone; GHF—Gumdrop Hills fault; HLF—Honey Lake fault; HMF—Hunter Mountain fault; IHF—Indian Head fault; MVF—Mohawk Valley fault; OF—Olinghouse fault; OVF—Owens Valley fault; PLF—Pyramid Lake fault; PSF—Petrified Spring fault; PVF—Panamint Valley fault; QVF—Queen Valley fault; SLF—Stateline fault; SNFF—Sierra Nevada frontal fault zone; WMF—White Mountains fault zone; WRF—Wassuk Range fault; WSF—Warm Springs fault. Layer B. Geographic names. Layer C. Tectonic domains. Semi-transparent brown shows the Walker Lane–northern Eastern California shear zone. Layer D. Yellow dashed polygon shows the location of the Gabbs Valley–Gillis Ranges (GVGR) field area (see Fig. 3). Layer E. Yellow stars show the locations of documented middle Miocene fault-slip initiation age. Numbers in the stars are tied to numbers in Table 3. Layer F. Thin blue arrows show GPS velocities relative to stable North America (ITRFNA2005 reference frame) from Lifton et al. (2013), and heavy multi-colored arrows show GPS velocities relative to stable North America (NA12 North America reference frame) from Bormann et al. (2016). GPS velocity scales are in the upper right corner of the map. Maps, labels, and data sets for this figure are organized in a series of layers that may be viewed separately or in combination using the capabilities of the Acrobat (PDF) layering function (click “Layers” icon along vertical bar on left side of window for display of available layers; turn layers on or off by clicking the box that encompasses the layer label located within the gray box in the lower left corner of the map).


Author(s):  
Rich W. Briggs ◽  
William J. Stephenson ◽  
John H. McBride ◽  
Jackson K. Odum ◽  
Nadine G. Reitman ◽  
...  
Keyword(s):  

2020 ◽  
Vol 133 (1-2) ◽  
pp. 307-324
Author(s):  
Zachery M. Lifton ◽  
Jeffrey Lee ◽  
Kurt L. Frankel ◽  
Andrew V. Newman ◽  
Jeffrey M. Schroeder

Abstract The White Mountains fault zone in eastern California is a major fault system that accommodates right-lateral shear across the southern Walker Lane. We combined field geomorphic mapping and interpretation of high-resolution airborne light detection and ranging (LiDAR) digital elevation models with 10Be cosmogenic nuclide exposure ages to calculate new late Pleistocene and Holocene right-lateral slip rates on the White Mountains fault zone. Alluvial fans were found to have ages of 46.6 + 11.0/–10.0 ka and 7.3 + 4.2/–4.5 ka, with right-lateral displacements of 65 ± 13 m and 14 ± 5 m, respectively, yielding a minimum average slip rate of 1.4 ± 0.3 mm/yr. These new slip rates help to resolve the kinematics of fault slip across this part of the complex Pacific–North American plate boundary. Our results suggest that late Pleistocene slip rates on the White Mountains fault zone were significantly faster than previously reported. These results also help to reconcile a portion of the observed discrepancy between modern geodetic strain rates and known late Pleistocene slip rates in the southern Walker Lane. The total middle to late Pleistocene slip rate from the southern Walker Lane near 37.5°N was 7.9 + 1.3/–0.6 mm/yr, ∼75% of the observed modern geodetic rate.


2020 ◽  
Author(s):  
J. Lee ◽  
et al.

Figure 2. Layer A. Shaded relief map showing major Quaternary faults in central Walker Lane, Mina deflection, northern Eastern California shear zone, and western Basin and Range Province. Heavy black arrow in the northwest corner of the map shows the present-day azimuth of motion of the Sierra Nevada block with respect to the central Great Basin (SN-CBG) (Bennett et al., 2003). Fault abbreviations: APHF—Agai Pah Hills fault; BSF—Benton Spring fault; CF—Coaldale fault; CVF—Clayton Valley fault; EIFZ—Eastern Inyo fault zone; EPF—Emigrant Peak fault; FLVFCDV—Fish Lake Valley–Furnace Creek–Death Valley fault zone; GHF—Gumdrop Hills fault; HLF—Honey Lake fault; HMF—Hunter Mountain fault; IHF—Indian Head fault; MVF—Mohawk Valley fault; OF—Olinghouse fault; OVF—Owens Valley fault; PLF—Pyramid Lake fault; PSF—Petrified Spring fault; PVF—Panamint Valley fault; QVF—Queen Valley fault; SLF—Stateline fault; SNFF—Sierra Nevada frontal fault zone; WMF—White Mountains fault zone; WRF—Wassuk Range fault; WSF—Warm Springs fault. Layer B. Geographic names. Layer C. Tectonic domains. Semi-transparent brown shows the Walker Lane–northern Eastern California shear zone. Layer D. Yellow dashed polygon shows the location of the Gabbs Valley–Gillis Ranges (GVGR) field area (see Fig. 3). Layer E. Yellow stars show the locations of documented middle Miocene fault-slip initiation age. Numbers in the stars are tied to numbers in Table 3. Layer F. Thin blue arrows show GPS velocities relative to stable North America (ITRFNA2005 reference frame) from Lifton et al. (2013), and heavy multi-colored arrows show GPS velocities relative to stable North America (NA12 North America reference frame) from Bormann et al. (2016). GPS velocity scales are in the upper right corner of the map. Maps, labels, and data sets for this figure are organized in a series of layers that may be viewed separately or in combination using the capabilities of the Acrobat (PDF) layering function (click “Layers” icon along vertical bar on left side of window for display of available layers; turn layers on or off by clicking the box that encompasses the layer label located within the gray box in the lower left corner of the map).


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