Geology of the Tick Canyon Area


Autoria(s): Woodcock, J. Richard
Data(s)

1952

Resumo

The eastern part of the Ventura Basin contains great thicknesses of non-marine Tertiary sediments. The lower formations of the Tertiary strata outcrop in the Tick Canyon Area and are described in this report. Emphasis is placed on the description of the Vasquez formation which is the lowest Tertiary unit in the Tick Canyon Area and which contains the only Tertiary lavas found in the East Ventura Basin.

Formato

application/pdf

Identificador

http://thesis.library.caltech.edu/9047/1/Woodcock_jr_1952.pdf

Woodcock, J. Richard (1952) Geology of the Tick Canyon Area. Senior thesis (Major), California Institute of Technology. http://resolver.caltech.edu/CaltechTHESIS:07022015-144741256 <http://resolver.caltech.edu/CaltechTHESIS:07022015-144741256>

Relação

http://resolver.caltech.edu/CaltechTHESIS:07022015-144741256

http://thesis.library.caltech.edu/9047/

Tipo

Thesis

NonPeerReviewed