Geochemical and Stable Isotopic Studies of the Hwacheon Granite

화천 화강암에 대한 지화학 및 안정동위원소 연구

  • Published : 2003.04.01

Abstract

Oxygen and hydrogen isotopic data of whole rocks and mineral separates generally provide constraints on the nature of hydrothermal systems. We here report preliminary results of analyses of samples taken from the peraluminous granitic rocks and banded gneiss country rocks in Hwacheon area. Oxygen isotopic values for quartz and feldspar separates from the granitoids in Hwacheon area range from 8.2 to 10.6$\textperthousand$ and 5.8 to 8.5$\textperthousand$, respectively. (omitted)

Keywords