Arc-continent collision zones are primary sites of net continental crustal growth: Evidence from Neoproterozoic and Mesozoic magmatic rocks in the periphery of the Yangtze craton

Details Arc-continent collision zones are primary sites of net continental crustal growth: Evidence from Neoproterozoic and Mesozoic magmatic rocks in the periphery of the Yangtze craton Arc-continent collision zones are primary sites of net continental crustal growth: Evidence from Neoproterozoic and Mesozoic magmatic rocks in the periphery of the Yangtze craton

Jun 2009

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2009gecas..73q1524z&link_type=openurl

Geochimica et Cosmochimica Acta Supplement, Volume 73, p.A1524

Physics

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