Taconian retrograde eclogite from northwest Connecticut, USA, and its petrotectonic implications
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文摘

We confirm the presence of Taconian eclogite in northwest Connecticut.

The PT path is characterized by a post-peak-T pressure increase of > 5 kbar.

The protoliths were likely rifting-related mafic dikes that intruded in the Early Cambrian.

A new U–Pb zircon age of 456 ± 4.6 Ma (2σ) dates the timing of high-pressure metamorphism.

Taconic metamorphism took place ~ 10 Myr later in Connecticut than in Newfoundland.

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