Late Cenozoic Volcanic Rocks of the Southern Sierra Nevada, California: I. Geology and Petrology

1980 ◽  
Vol 91 (9_Part_II) ◽  
pp. 1995-2038 ◽  
Author(s):  
James G. Moore ◽  
Franklin C. W. Dodge
2022 ◽  
pp. 106076
Author(s):  
D. Hatzenbühler ◽  
L. Caracciolo ◽  
G.J. Weltje ◽  
A. Piraquive ◽  
M. Regelous
Keyword(s):  

Author(s):  
Emmanuel Gabet

Hildreth et al. (2021) analyzed a set of table mountains near the San Joaquin River that are capped by a 9.3 Ma trachyandesite lava flow and concluded that, since the deposition of the volcanic rocks, the table mountains have been tilted 1.07° due to uplift of the central Sierra Nevada. While Gabet (2014) suggested that, under a limited set of conditions, the size of fluvial gravels under the table mountains would support the hypothesis of postdepositional uplift, the authors claimed that their evidence is more definitive. In addition, the authors proposed that the central Sierra Nevada tilted as a rigid block. However, their analyses rely on inferences and assumptions that are not supported by field evidence.


2019 ◽  
Vol 319 (6) ◽  
pp. 526-527
Author(s):  
Emmanuel J. Gabet ◽  
Jeffrey P. Schaffer ◽  
William A. Peppin ◽  
Daniel P. Miggins

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