Zircon trace element constrains on the link between volcanism and plutonism in SE-China

Journal article

Publication Details

Author(s): Yan LL, He Z, Beier C, Klemd R
Journal: Lithos
Publication year: 2018
Journal issue: 320-321
Pages range: 28-34
ISSN: 0024-4937
Language: English


Trace elements in igneous zircon crystals are variable within single crystals or amongst populations of crystals and are particularly sensitive to changes in melt composition. In this study, we present zircon trace element data from both volcanic and plutonic rocks of the Yandangshan caldera complex from SEChina. The erupted rhyolitic rocks are interpreted to represent the most differentiated magma, whereas the intruded porphyritic quartz syenites are thought to be representative of the residual crystal mush. The zircon crystals of both lithologies are subdivided into two types based on their internal structures: type A with a distinct oscillatory growth zoning and type B crystals are bright in cathodoluminescence (CL-bright). Type B zircon occurs as rims of type A zircon or as individual grains. Compared to type A, type B zircons commonly show lower Hf, U, Th and Y concentrations and higher Ti and Zr/Hf and Eu/Eu* ratios. The zircon trace element compositions of the volcanic samples generally overlap those of the intracaldera porphyritic quartz syenite and mafic microgranular enclaves that contain both type A and type B zircons. Despite a general overlap, zircon grains from the volcanic rocks show relatively higher Hf contents and Y/Dy ratios, lower Ti contents and Th/U ratios and larger negative Eu anomalies than the plutonic samples. We suggest that the inter- and intragrain compositional variability of zircon crystals can be used to track the evolution of magmatic systems. We show that in our case, the volcanic and plutonic rocks crystallized continuously during the magmatic evolution in a common magma system and that the magmas of these rocks may be linked by fractional crystallization. Furthermore, the type B zircon grains are inferred to have crystalized in relatively hot and less evolved magma indicating a magma recharge event. Consequently, the geochemical variability of igneous zircon crystals can be used to infer on the magmatic evolution of single volcanic system which may also be applicable in other geodynamic environments.

FAU Authors / FAU Editors

Beier, Christoph PD Dr.
Lehrstuhl für Endogene Geodynamik
Klemd, Reiner Prof. Dr.
Professur für Geochemie und Lagerstättenkunde

External institutions with authors

Chinese Academy of Geological Sciences (CAGS) / 中国地质科学院

How to cite

Yan, L.L., He, Z., Beier, C., & Klemd, R. (2018). Zircon trace element constrains on the link between volcanism and plutonism in SE-China. Lithos, 320-321, 28-34. https://dx.doi.org/10.1016/j.lithos.2018.08.040

Yan, Lili Li, et al. "Zircon trace element constrains on the link between volcanism and plutonism in SE-China." Lithos 320-321 (2018): 28-34.


Last updated on 2019-20-05 at 20:23