Oxygen Isotopes in Co3 Chondrites

نویسندگان

  • R. C Greenwood
  • I. A. Franchi
چکیده

Introduction: The results of a number of studies seem to indicate that CO3 chondrites can be subdivided into a metamorphic series analogous to that seen in ordinary chondrites [1,2,3]. It has been suggested that this sequence is the result of hydrothermal alteration on the CO parent body [4]. One particularly intriguing feature of CO3 chondrites is the reported general correlation between whole rock oxygen isotope values and petrographic subtype, such that values appear to become increasingly O-rich with increasing metamorphic grade [4,5]. In view of the importance of trying to disentangle nebular from later parent body processes we have undertaken a further investigation of the oxygen isotope systematics of CO3 chondrites.

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تاریخ انتشار 2001