Upper and lower crust recycling in the source of CAMP basaltic dykes from southeastern North America
The densest dykes swarm of the Central Atlantic magmatic province (CAMP) occur in southeastern North America (SENA) and were intruded between 202 and 195 Ma during Pangea break-up. New combined geochemical data (major and trace elements, Sr–Nd–Pb–Os isotopes) constrain the mantle source of these mag...
| Main Authors: | , , , , , , , , |
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| Format: | Journal Article |
| Published: |
Elsevier Science BV
2013
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| Subjects: | |
| Online Access: | http://hdl.handle.net/20.500.11937/42388 |