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Institute on Lake Superior Geology: 49th annual meeting, May 7-12, 2003, Iron Mountain, Michigan
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摘要
The Niagara suture zone formed during the Penokean orogeny at about 1875 Ma by collision of island arcs of the Wisconsin magmatic terranes with the southern margin of the Superior craton and its epicratonic cover of the Marquette Range Supergroup.

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