We studied the Lake George ring complex which is part of the Pikes Peak batholith.
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Our new U–Pb ages show that the Lake George ring complex started to form at 1115 Ma.
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New U–Pb ages also indicate that the Lake George ring complex formed over ⩾27 My.
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Our new Hf isotopic data indicate sequential tapping of mantle and crustal sources.
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This study calls for a general reassessment of Pikes Peak batholith emplacement age.
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