Reply [to “Comment on ‘The Snake Range Decollement interpreted as a major extensional shear zone” by John. M. Bartley and Brian P. Wernicke”]

Tectonics

Volumn 4, Issue 4, 1985, Pages 417-419

  Wernicke, Brian ^a   Bartley, John M ^a  

^a NONE

Author keywords

[No Author keywords available]

Indexed keywords

EID: 84982684051     PISSN: 02787407     EISSN: 19449194     Source Type: Journal    
DOI: 10.1029/TC004i004p00417     Document Type: Letter

References (14)

1. The Snake Range decollement interpreted as a major extensional shear zone
2. Mesozoic thrusts and folds in the northern Quinn Canyon Range, Nye County, Nevada
3. Regional gravity and tectonic patterns their relation to late Cenozoic epeirogeny and lateral spreading in the western Cordillera, Cenozoic Tectonics and Regional Geophysics of the Western Cordillera; edited by R. B. Smith and G. P. Eaton
4. The influence of erosion upon the mineral facies of rocks from different metamorphic environments
5. Origin of Mesozoic and Tertiary granite in the western United States and implications for pre‐Mesozoic crustal structure, 1, Nd and Sr isotope studies in the geocline of the Northern Great Basin
6. Comment on "The Snake Range decollement interpreted as a major extensional shear zone" by John M. Bartley and Brian P. Wernicke
7. Tertiary extensional faulting and evolving ductile‐brittle transition zones in the northern Snake Range and vicinity: New insights from seismic data
8. Evolution of lithospheric strength after thrusting;
9. Tertiary stratigraphy and geologic history of the Sacramento Pass area, Nevada
10. Gradients in silicic magma chambers, Implications for lithospheric magmatism
11. The Snake Range decollement: An exhumed mid‐Tertiary ductile‐brittle transition
12. Low‐angle normal faults in the Basin and Range province: nappe tectonics in an extending orogen
13. Structural discordance between Neogene detachments and frontal Sevier thrusts, central Mormon Mountains, southern Nevada