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 411-415

  Gans, Phillip B ^a   Miller, Elizabeth L ^a  

^a NONE

Author keywords

[No Author keywords available]

Indexed keywords

EID: 84982746850     PISSN: 02787407     EISSN: 19449194     Source Type: Journal    
DOI: 10.1029/TC004i004p00411     Document Type: Note

References (10)

1. Cenozoic and Mesozoic structure of the eastern Basin and Range province, Utah, from COCORP seismic‐reflection data
2. The Snake Range decollement interpreted as a major extensional shear zone
3. Metamorphic bathozones and bathograds: A measure of the depth of post‐metamorphic uplift and erosion on the regional scale
4. 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
5. Style of mid‐Tertiary extension in east‐central Nevada, Guidebook, part 1
6. Tertiary extensional faulting and evolving ductile‐brittle transition zones in the northern Snake Range and vicinity: New insights from seismic data
7. Gradients in silicic magma chambers: Implications for lithospheric magmatism
8. Stability of andalusite and the aluminum silicate phase diagram
9. The Snake Range decollement: An exhumed mid‐Tertiary ductile‐brittle transition