Geochemistry and geochronology of late Mesozoic volcanic rocks in the northern part of the Eastern Pontide Orogenic Belt (NE Turkey): Implications for the closure of the Neo-Tethys Ocean
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文摘

Volcanic activity started 86 My and finished 75 My ago.

The Ordu volcanics are calc-alkaline and likely produced in a continental arc environment.

Chemical characteristics of the volcanic rocks were controlled by AFC and FC.

The Ordu volcanic rocks have initial Sr ratios varying between 0.70569 and 0.70606 and initial Nd ratios between 0.51244 and 0.51249.

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