Samples from 12 different mare sites were identified and classified among the Apollo 15 samples. The genesis of the Apollo 15 mare units is summarized given the general model of mare basalt source regions and of more basalt genesis derived from a synthesis of the major oxide/major mineral, compatible siderophile, and incompatible trace element data and isotopic ratios of the Rb/Sr and Sm/Nd systems.
Apollo 15 mare units and their petrogenesis
1985-01-01
Conference paper
No indication
English
British Library Conference Proceedings | 1994
|British Library Conference Proceedings | 1994
|