Glacial deposits and paleomagnetic data indicate that Qiangtang and Shan Thai-Malaya were still located far south adjacent to Gondwana during the Carboniferous.
Os depósitos glaciais e os datos paleomagnéticos indican que Qiangtang e Shan Thai-Malaia estaban aínda localizados moi ao sur, adxacentes a Gondwana durante o Carbonífero.