Origin of the Qiyugou gold deposit in the southern margin of the North China Craton: Insights from trace elements of pyrite and mineralogy of Bi-minerals

2021 ◽  
Vol 133 ◽  
pp. 104085
Author(s):  
Qiang Wu ◽  
Tai-Ping Zhao ◽  
Wei Terry Chen ◽  
Xin-Yu Gao ◽  
Lei Meng ◽  
...  
Keyword(s):  
Trace Elements ◽  
Gold Deposit ◽  
North China Craton ◽  
North China ◽  
The North ◽  
Southern Margin

The gold occurrence in pyrite and Te–Bi mineralogy of the Fancha gold deposit, Xiaoqinling gold field, southern margin of the North China Craton: Implication for ore genesis

2019 ◽  
Vol 55 (8) ◽  
pp. 5791-5811 ◽  
Author(s):  
Junchen Liu ◽  
Yitian Wang ◽  
Shikang Huang ◽  
Ran Wei ◽  
Zhenghao Sun ◽  
...  
Keyword(s):  
Gold Deposit ◽  
North China Craton ◽  
North China ◽  
Ore Genesis ◽  
The North ◽  
Gold Occurrence ◽  
Southern Margin

Crust–Mantle Interaction Recorded by Early Cretaceous Volcanic Rocks within the Southern Margin of the North China Craton

2021 ◽  
Author(s):  
An-Qi Wang ◽  
Debin Yang ◽  
Wen-Liang Xu ◽  
Hao-Tian Yang ◽  
Mao-Song Mu ◽  
...  
Keyword(s):  
Early Cretaceous ◽  
North China Craton ◽  
North China ◽  
Volcanic Rocks ◽  
The North ◽  
Southern Margin

scholarly journals Geochemistry and tectonic significance of late Paleoproterozoic A-type granites along the southern margin of the North China Craton

2020 ◽  
Vol 10 (1) ◽  
Author(s):  
Yan Wang ◽  
Yi-Zeng Yang ◽  
Wolfgang Siebel ◽  
He Zhang ◽  
Yuan-Shuo Zhang ◽  
...  
Keyword(s):  
North China Craton ◽  
North China ◽  
Published Data ◽  
Pb Isotope ◽  
Granite Sample ◽  
The North ◽  
Southern Margin ◽  
Basement Rocks ◽  
Type Granite ◽  
Melting Product

AbstractThe Longwangzhuang pluton is a typical example of Paleoproterozoic A-type granite intrusions at the southern margin of the North China Craton. This pluton is composed of arfvedsonite granite and minor aegirine–augite granites. Samples from both granite types display similar zircon U-Pb ages with 207U-206Pb ages of 1612 ± 19 Ma [mean square weighted deviation (MSWD) = 0.66] and 1609 ± 24 Ma (MSWD = 0.5), respectively. The granites exhibit similar high silica (SiO2 = 71.1–73.4 wt.%), high alkaline (Na2O + K2O = 8.10–9.26 wt.%, K2O/Na2O > 1), and low Al2O3 (11.8–12.8 wt. %) contents and metaluminous to weakly peraluminous bulk chemistry. The chemical variations of the Longwangzhuang pluton suggest the effects of mineral fractionation. In addition, all samples show typical characteristics of A-type granites, such as high 10000Ga/Al ratios (4.10–7.28), high FeOtot/(FeOtot + MgO) ratios (0.88–0.99), and high Zr (484–1082 ppm), Ce (201–560 ppm), and Y (78–156 ppm) contents. The εNd(t) values and the (206Pb/204Pb)t, (207Pb/204Pb)t, and (208Pb/204Pb)t ratios of the arfvedsonite granite samples vary from −4.6 to –5.3, 15.021 to 17.349, 15.241 to 15.472, and 33.206 to 36.905, respectively, and those for the aegirine–augite granite sample amount at −0.2, 14.421, 15.175, and 33.706. The distinct and variable Nd and Pb isotope values indicate the presence of heterogeneous protoliths. Based on its geochemistry, its low initial Pb isotope ratios, and its enrichment in Nd isotopes, we infer that the Longwangzhuang A-type granite is the partial melting product of basement rocks such as the Taihua Group gneisses accompanied by some involvement of juvenile material from the mantle. Together with published data from other Paleoproterozoic A-type granite plutons exposed at the southern margin of the craton, our findings suggest that these granites had a similar origin. Furthermore, geochemically, they can be divided into two groups: A2-type, which formed earlier (~1.8–1.6 Ga), and A1-type, which formed later (~1.6–1.5 Ga). Combining this information with the variations in whole-rock Nd and zircon Hf isotopic composition at ca. 1.6 Ga, we propose that tectonic transformation from post-orogenic to anorogenic magmatism occurred at the southern margin of the North China Craton at that time.

Sign in / Sign up

Export Citation Format

Share Document