Mesoproterozoic continental arc magmatism and crustal growth in the eastern Central Tianshan Arc Terrane of the southern Central Asian Orogenic Belt: Geochronological and geochemical evidence
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文摘

Voluminous Mesoproterozoic continental arc magmatism occurred from at least 1.45 to 1.40 Ga in the CTA;

Widespread Mesoproterozoic crustal growth was associated with the continental arc magmatism in the CTA;

The Mesoproterozoic CTA underwent multiple reworking and metamorphic events in the Neoproterozoic and the Paleozoic;

A Precambrian correlation of the CTA and the Tarim Craton is questionable;

The CTA and the southern Beishan microcontinents underwent a similar Precambrian tectonothermal evolution.

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