ZIRCON U-PB ISOTOPE AGE OF SYENITE FROM PU SAM CÁP COMPLEX
AND ITS GEOLOGICAL IMPLICATION
Nguyễn Thị Bích Thủy
General Department of Geology and
Minerals of Vietnam
Corresponding
author: thuynguyendcks@yahoo.com
Abstract: The Pu Sam Cáp complex consists of granosyenite, syenite, alkaline
syenite and granite. These rocks exposed under the form of small bodies. The
rocks are grey, light grey in color and have the porphyritic texture with phenocryst
of K-feldspar. The main rock-forming minerals are K-feldspar, plagioclase,
biotite and alkaline amphibole and pyroxene. Accessory phases are sphene,
zircon and apatite. Zircon grains separated from two syenite samples collected
in Chinh Sáng area have grain sizes ranging from 80 to 120 µm. Most of
zircon grains have isometric and euhedral shape, display oscillatory zoning
indicating magmatic origin. LA-ICP-MS zircon U-Pb analytical results from these
two samples revealed emplacement age of the Pu Sam Cáp complex at ca. 35 Ma. The new geochronological data of magmatic rocks of the Pu Sam Cáp
complex provide evidence for Middle Paleogene
magmatism and formation of continental crust in the study area.
Keywords: Pu Sam Cáp
syenite, U-Pb zircon age, Chinh Sáng, Northwest Vietnam
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