INFRARED MICROSPECTROSCOPY ANALYSIS OF WATER DISTRIBUTION IN DEFORMEDAND METAMORPHOSED ROCKS

Infrared microspectroscopy has been applied to thin sections of variou s deformed and metamorphosed rocks in order to investigate water conte nt of quartz in these rocks. The broad IR band absorbance around 3400 cm(-1) probably due to fluid-inclusion molecular water (H2O) was used to calculate water contents. Deformed granitic rocks from the Yanazawa -Kamimura area near the Median Tectonic Line (MTL) showed an increase of water content in quartz from about 300 ppm to 2500 ppm toward the M TL with increasing degree of deformation. Metacherts from Sambagawa me tamorphic rocks (Asemigawa route) showed a systematic decrease of wate r content in quartz from about 1000 ppm to 200 ppm with increasing met amorphic degree from chlorite, garnet, albite-biotite to oligoclase-bi otite zones. An Archaean metachert from the Napier Complex (granulite facies) has only 40 ppm water. Comparing this with an Inuyama unmetamo rphosed chert sample having water contents of 3500 to 7000 ppm (a star ting point of metamorphism), the systematic decrease of water in quart z with increasing metamorphic grade may extend from unmetamorphosed ch erts to the highest-grade metacherts. Water contents in high-pressure metamorphic rocks in Japan are mostly of the order of 500 ppm (300-700 ppm), except for those from Kurosegawa with a water content as high a s 1700 ppm. These results represent an exploratory analysis of intragr anular water contents in quartz in various deformed and metamorphosed rocks. Further micro FT-IR studies of the distribution of water in cru stal rocks will provide a quantitative basis for examining the geochem ical cycle of water in the earth's crust.