U-Pb Zircon (SHRIMP) ages of granite sheets and timing of deformational events in the Natal Metamorphic Belt, southeastern Africa: Evidence for deformation partitioning and implications for Rodinia reconstructions
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文摘

Two adjacent granitic sheets of structurally different ages were dated.

The pre-D1 granite intruded at 1075 ± 6 Ma and D2 occurred at ∼1042 ± 10 Ma.

Coeval zones of pure shear and simple shear indicate deformation partitioning.

The D2 transpression may be related to collision with Laurentia.

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