Age and tectonic implications of Paleoproterozoic Deo Khe Granitoids within the Phan Si Pan Zone, Vietnam. (1st November 2015)

• Record Type: Journal Article
• Authors: Anh, Hoang Thi Hong; Hieu, Pham Trung; Tu, Vu Le; Son, La Mai; Choi, Sung Hi; Yu, Yongjae
• Is Part Of: Journal of Asian earth sciences. Volume 111(2015)
• Page Start: 781
• Page End: 791
• Publication Date: 2015-11-01
• Subjects: Vietnam -- Granitoids -- Archean -- Paleoproterozoic -- Zircon age -- Hf isotope; Earth sciences -- Asia -- Periodicals; Sciences de la terre -- Asie -- Périodiques; Earth sciences; Asia; Periodicals; 555.05
• DOI: 10.1016/j.jseaes.2015.07.014
• Languages: English
• ISSNs: 1367-9120

Abstract

Graphical abstract: Highlights: The first U–Pb zircon ages of 1855–1873 Ma in northern Vietnam is provided. The Deo Khe Granitoids are a product of recycled Archean crustal rocks. Northern Vietnam and South China may share a similar tectonic history. Abstract: We report the first U–Pb zircon ages of 1855–1873 Ma for the Deo Khe Granitoids (DKG) in the Phan Si Pan Zone (PSPZ) of northern Vietnam. The DKG are medium-grained two-mica granitoids predominantly composed of quartz, K-feldspar, and muscovite. Trace element analyses indicate that the DKG are enriched in large ion lithophile elements but depleted in high field strength elements. Zircons from the granitoids have negative ε Hf ( t ) values ranging from −23.6 to −17.5. The magmatic zircons from the DKG have single-stage Hf model ages ( T DM1 ) that range from 3.3 to 2.8 Ga and their ε Hf ( t ) data all plot well below the evolution trend of 2800 Ma average juvenile mantle. Observed Hf model ages are contemporaneous with the emplacement of 2.90–2.84 Ga tonalite–trondhjemite–granodiorite (TTG) gneiss observed in a nearby Ca Vinh Complex, suggesting that PSPZ in northern Vietnam is a product of partial melting of Archean crust. A sequence of similar tectonic events including initial emplacement of TTG protolith at 2.8–2.9 Ga, metamorphic development of TTG gneiss at 1.9–2.0 Ga, and magmatic activity at 1.8–2.0 Ga are now recognized both in northern Vietnam and Yangtze block which we interpret to indicate basement rocks in northern Vietnam are similar to those found along southern China.