Ibarra, Yadira, Corsetti, Frank A., Cheetham, Michael I., and Feakins, Sarah J. Were fossil spring-associated carbonates near Zaca Lake, Santa Barbara, California deposited under an ambient or thermal regime?. Retrieved from https://par.nsf.gov/biblio/10076103. Sedimentary Geology 301.C Web. doi:10.1016/j.sedgeo.2013.12.005.

Ibarra, Yadira, Corsetti, Frank A., Cheetham, Michael I., & Feakins, Sarah J. Were fossil spring-associated carbonates near Zaca Lake, Santa Barbara, California deposited under an ambient or thermal regime?. Sedimentary Geology, 301 (C). Retrieved from https://par.nsf.gov/biblio/10076103. https://doi.org/10.1016/j.sedgeo.2013.12.005

Ibarra, Yadira, Corsetti, Frank A., Cheetham, Michael I., and Feakins, Sarah J. "Were fossil spring-associated carbonates near Zaca Lake, Santa Barbara, California deposited under an ambient or thermal regime?". Sedimentary Geology 301 (C). Country unknown/Code not available. https://doi.org/10.1016/j.sedgeo.2013.12.005. https://par.nsf.gov/biblio/10076103.

@article{osti_10076103,
place = {Country unknown/Code not available}, title = {Were fossil spring-associated carbonates near Zaca Lake, Santa Barbara, California deposited under an ambient or thermal regime?}, url = {https://par.nsf.gov/biblio/10076103}, DOI = {10.1016/j.sedgeo.2013.12.005}, abstractNote = {}, journal = {Sedimentary Geology}, volume = {301}, number = {C}, author = {Ibarra, Yadira and Corsetti, Frank A. and Cheetham, Michael I. and Feakins, Sarah J.}, }