Chonghui Yang

TL;DR: The 3.8-Ga meta-quartz dioritic rocks discovered recently in the Anshan area show relatively high ∑REE contents and low (La/Yb) n ratios, with t DM of 3.50-4.16 and ǫ Nd of −1.24 to 4.51 as mentioned in this paper.

TL;DR: The North China Craton (NCC) is characterized by major ∼2.5 Ga tectono-thermal events and is thus different from many other cratons worldwide where ∼ 2.7 Ga events are well developed as mentioned in this paper.

TL;DR: In this paper, the SHRIMP results on basaltic andesite are divided into two groups and interpreted as the eruption age of the base of the Hutuo Group, which is consistent with the basement crustal age in Fuping and Wutai areas.

TL;DR: In this article, a suite of banded TTG gneisses from the Zanhuang Complex was delineated, which is intimately associated with melanocratic dioritic and leucocratic trondhjemitic veins.

TL;DR: In this article, the Huangjinshan granite porphyry in the Wutai area, North China Craton (NCC) yielded concordant ages, with a weighted mean 207 Pb/ 206 Pb age of 2137-±-9-Ma, which indicates that the granite was emplaced in the middle Paleoproterozoic.