New paleomagnetic results from Ordovician sedimentary rocks from NW Anatolia: Tectonic implications for the paleolatitudinal position of the Istanbul Terrane
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文摘

We have conducted a paleomagnetic study to determine the paleolatitude of the Istanbul terrane during the Ordovician.

Characteristic higher temperature components passed fold test and direction-correction test (DC test).

Our result shows a lower paleolatitudinal position closer to the equatorial zone than previously inferred.

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