Constraining the timing and sources of volcanism at the Apollo 12 landing site using new Pb isotopic compositions and crystallisation ages
The basaltic suites collected at the Apollo 12 landing site have been interpreted as representing a stratigraphic sequence of volcanic flows emplaced in the Oceanus Procellarum region between approximately 3100–3300 Ma. This study presents Secondary Ion Mass Spectrometry (SIMS) Pb isotopic analyses...
| Main Authors: | , , , , |
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| Format: | Journal Article |
| Published: |
Elsevier Science BV
2018
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| Online Access: | http://hdl.handle.net/20.500.11937/67265 |