Tertiary Normal Faulting in the Canyon Range, Eastern Sevier Desert

1999 ◽  
Vol 107 (6) ◽  
pp. 659-681 ◽  
Author(s):  
Stewart Wills ◽  
Mark H. Anders
Keyword(s):  
Normal Faulting ◽  
Canyon Range ◽  
Sevier Desert

scholarly journals Miocene unroofing of the Canyon Range during extension along the Sevier Desert Detachment, west central Utah

Tectonics ◽  
2001 ◽  
Vol 20 (3) ◽  
pp. 289-307 ◽  
Author(s):  
Daniel F. Stockli ◽  
Jonathan K. Linn ◽  
J. Douglas Walker ◽  
Trevor A. Dumitru
Keyword(s):  
West Central ◽  
Canyon Range ◽  
Sevier Desert

Apercu geologique sur les collines de Boutenac (Aude)

1962 ◽  
Vol S7-IV (3) ◽  
pp. 362-379
Author(s):  
Alain Combes
Keyword(s):  
Upper Cretaceous ◽  
Upper Triassic ◽  
Normal Faulting ◽  
The West ◽  
Southern France ◽  
Sandy Limestone

Abstract The Boutenac hills in the northeastern Corbieres region of southern France, are part of the autochthonous foreland of the eastern Corbieres nappe. They are an isolated massif between the Paleozoic formations of the Alaric mountain on the west, and the Jurassic and Cretaceous formations of the Fontfroide chain on the east, entirely surrounded by alluvium. Structurally, they comprise Mesozoic formations on the east thrust over the Eocene on the west, on a fault that is the prolongation of the Saint Chinian frontal fault to the northeast. The Mesozoic formations comprise upper (?) Triassic shale and dolomite, sandy limestone, dolomite, and limestone; Jurassic red sandstones and shales; and upper Cretaceous transgressive clastics. The Eocene is limestone and marl overlain by continental conglomerate and molasse, transgressive on the west upon the Alaric Paleozoics. Folding and thrust and normal faulting are important in the structure.

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