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| Autore: |
Howard Jeffrey L.
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| Titolo: |
Conglomerates of the Upper Middle Eocene to Lower Miocene Sespe Formation along the Santa Ynez Fault : implications for the geologic history of the eastern Santa Maria Basin area, California / / by Jeffrey L. Howard. Reconnaissance bulk-rock and clay mineralogies of argillaceous Great Valley and Franciscan strata, Santa Maria Basin Province, California / by Richard M. Pollastro, Hugh McLean, and Laura L. Zink
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| Pubblicazione: | [Reston, Va.] : , : U.S. Department of the Interior, U.S. Geological Survey, , 1995 |
| Washington : , : United States Government Printing Office | |
| Descrizione fisica: | 1 online resource (v, 50 pages) : illustrations, maps |
| Soggetto topico: | Argillite - California - Santa Maria Basin |
| Conglomerate - California - Santa Maria Basin | |
| Geology, Stratigraphic - Cenozoic | |
| Geology, Stratigraphic - Eocene | |
| Mineralogy - California - Santa Maria Basin | |
| Sedimentation and deposition - California - Santa Maria Basin | |
| Argillite | |
| Cenozoic Geologic Period | |
| Conglomerate | |
| Eocene Geologic Epoch | |
| Geology, Stratigraphic | |
| Mineralogy | |
| Sedimentation and deposition | |
| Soggetto geografico: | Santa Maria Basin (Calif.) |
| Sespe Formation (Calif.) | |
| California Santa Maria Basin | |
| California Sespe Formation | |
| Persona (resp. second.): | McLeanHugh <1939-> |
| ZinkLaura L. | |
| PollastroRichard M. | |
| Note generali: | Title from title screen (viewed Aug. 28, 2014). |
| Nota di bibliografia: | Includes bibliographical references. |
| Altri titoli varianti: | Conglomerates of the Upper Middle Eocene to Lower Miocene Sespe Formation along the Santa Ynez Fault |
| Titolo autorizzato: | Conglomerates of the Upper Middle Eocene to Lower Miocene Sespe Formation along the Santa Ynez Fault ![]() |
| Formato: | Materiale a stampa |
| Livello bibliografico | Monografia |
| Lingua di pubblicazione: | Inglese |
| Record Nr.: | 9910707691803321 |
| Lo trovi qui: | Univ. Federico II |
| Opac: | Controlla la disponibilità qui |