Fluid composition and carbon & oxygen isotope geochemistry of Cenozoic alkali basalts in eastern China
The fluid compositions of Cenozoic alkali basalts in eastern China have been determined by the pyrolysis-MS method, meanwhile the carbon and oxygen isotopic compositions of CO^sub 2^ released from these samples at different heating temperatures have been analyzed by the vacuum step-heating method. T...
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Veröffentlicht in: | Acta geochimica 1999, Vol.18 (3), p.276-282 |
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Format: | Artikel |
Sprache: | eng |
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Zusammenfassung: | The fluid compositions of Cenozoic alkali basalts in eastern China have been determined by the pyrolysis-MS method, meanwhile the carbon and oxygen isotopic compositions of CO^sub 2^ released from these samples at different heating temperatures have been analyzed by the vacuum step-heating method. The data show the volatile heterogeneity in upper-mantle sources and different evolution trends of alkali basaltic magmas in eastern China, and these alkali basaltic magmas may be generated in the oxidizing milieu, as compared with mantle-derived xenoliths in these alkali basalts, and exotic volatile components were mixed into these magmas in the process of their formation and development.[PUBLICATION ABSTRACT] |
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ISSN: | 1000-9426 2096-0956 1993-0364 2365-7499 |
DOI: | 10.1007/BF02831074 |