(Q29011)
Statements
G.Corbett, 92p. Dickinson, W.R., and Lawton, T.F., 2001. Carboniferous to Cretaceous assembly and fragmentation
fault-bounded prism of strongly deformed Jurassic and Cretaceous oceanic and arc volcanic rocks that structurally
age, limestones and calcareous sedimentary rocks of Cretaceous age and continental conglomerates of
Dickinson, W.R., and Lawton, T.F., 2001. Carboniferous to Cretaceous assembly and fragmentation of Mexico.
west-dipping fault-bounded prism of strongly deformed Jurassic and Cretaceous oceanic and arc volcanic
intruded by granodiorite to diorite stocks of possible Neogene age. Figure 7.2 Local geology of the San
dacitic volcanic and volcaniclastic rocks of presumed Paleogene age. These units have been significantly
to dacitic effusive volcanic sequence of presumed Paleogene age. Further to the east, these andesites
area is underlain by a thick sequence of presumed Paleogene-age andesitic to dacitic volcanic and
Martinez-Serrano, et al, 2008). In the Taviche area, the Paleogene-age volcanics are intruded by granodiorite
dacitic volcanic and volcaniclastic rocks of presumed Paleogene age (Figure 7.3). These units have been
displacement Andesitic to dacitic subaerial to subaqueous lava flows Paleogene (?) Quartz-carbonate veins, hydrothermal
dacitic subaerial and subaqueous lava flows of presumed Paleogene age. Major vein systems recognized in
P97 (Deleted Property)
4530692:5PU2ZIPQ Property P97 not found, cannot determine the data type to use.
0 references