SUMARRY
Petrographical, geochemical composition and formation pressure -
temperature of Chiêm Hóa granites, Tuyên Quang province
Phạm Thị Dung, Trần Trọng
Ḥa, Trần Quốc Công, Trần Hồng Lam,
Đào Thái Bắc, Phạm Ngọc Cẩn, Bùi Ấn Niên, Phạm
Thị Phương Liên
Chiem Hóa granites are
exposed as small bodies in the Chiêm Hóa district, Tuyên Quang province. Their
petrographical composition includs light colored, small - to medium - grained
size biotite granite and two - mica granite, and aplite. The crystallization
temperature of granites calculated based on zircon saturation and chemical
composition of granites is 787 to 740o C, coreponding to the forming
- pressure and depth of <5 Kbar and 15 km, respectively. The rocks have high aluminum content with ASI>
1.1. The results of calculating the temperature by the method of zircon
saturation and the main element for the forming temperature fluctuate in a wide
range from about 787 to 740oC; The forming pressure is calculated based on the
main element, fluctuating in the range <5 Kbar (corresponding to the forming
depth of <15 km). Petrographic composition and geochemistry indicate that
Chiêm Hóa granite is characterized by S-type granite, originated from the crust
and formed at medium to shallow depth, similar to Phia Bioc granite.
Keywords: Chiêm Hóa granite, pressure, temperature,
Permian - Triassic.