O¹⁸/O¹⁶ and DIH Rations of Soils, Weathering Zones, and Clay Deposits
NOTE: Text or symbols not renderable in plain ASCII are indicated by [...]. Abstract is included in .pdf document. D/H and O18/O16 ratios have been determined for a large variety of bulk samples and mineral separates from: Quaternary soils and clay-rich weathering zones; Tertiary, Cretaceous and...
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Format: | Others |
Language: | en |
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1970
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Online Access: | https://thesis.library.caltech.edu/149/1/Lawrence_jr_1970.pdf Lawrence, James Robert (1970) O¹⁸/O¹⁶ and DIH Rations of Soils, Weathering Zones, and Clay Deposits. Dissertation (Ph.D.), California Institute of Technology. doi:10.7907/Y4JD-S067. https://resolver.caltech.edu/CaltechETD:etd-01132004-094857 <https://resolver.caltech.edu/CaltechETD:etd-01132004-094857> |
Internet
https://thesis.library.caltech.edu/149/1/Lawrence_jr_1970.pdfLawrence, James Robert (1970) O¹⁸/O¹⁶ and DIH Rations of Soils, Weathering Zones, and Clay Deposits. Dissertation (Ph.D.), California Institute of Technology. doi:10.7907/Y4JD-S067. https://resolver.caltech.edu/CaltechETD:etd-01132004-094857 <https://resolver.caltech.edu/CaltechETD:etd-01132004-094857>