The young Nd model ages suggest a significant crustal growth in the period of Neoproterozoic-Phanerozoic.
年轻的钕同位素模式年龄表明该区存在新元古—显生宙的地壳增生。
This study provides new evidence for continental crustal growth in the central Asian orogenic belt during the Phanerozoic.
该研究从另一个侧面证明中亚造山带存在一定规模的显生宙陆壳生长。
The results showed that the late Mesoproterozoic to early Neoproterozoic magmatic activities occurred in the Dabie area, which might also be a period of crustal growth in the Yangtze block.
这些结果证实，大别地区存在中元古代晚期到新元古代早期的岩浆作用，且这一时期扬子板块有不同程度的地壳生长。
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