Constraining the timing of deformation in the southwestern central zone of the Damara Belt, Namibia
Structural investigations and U-Pb sensitive high-resolution ion microprobe (SHRIMP) dating of rocks from the southwestern Central Zone of the Damara Belt, Namibia, reveal that a major SE-verging deformation event (D2) occurred at between 520 and 508 Ma.
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|Source:||Geological Society of London Special Publication|
|01_Longridge_Constraining_the_timing_of_2012.pdf||1.27 MB||Adobe PDF||Request a copy|
|02_Longridge_Constraining_the_timing_of_2012.pdf||1.27 MB||Adobe PDF||Request a copy|