Open AccessWater in the lower crustal granulite xenoliths from Nushan, eastern China
Author(s) -
Xia QunKe,
Yang XiaoZhi,
Deloule Etienne,
Sheng YingMing,
Hao YanTao
Publication year - 2006
Publication title -
journal of geophysical research: solid earth
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.67
H-Index - 298
eISSN - 2156-2202
pISSN - 0148-0227
DOI - 10.1029/2006jb004296
Subject(s) - granulite , geochemistry , geology , xenolith , basalt , pyroxene , crust , anhydrous , continental crust , plagioclase , olivine , chemistry , facies , geomorphology , paleontology , quartz , organic chemistry , structural basin
Nominally anhydrous clinopyroxene (cpx), orthopyroxene (opx), and plagioclase (pl) from 10 lower crustal granulite (two‐pyroxene granulite and hypersthene granulite) xenoliths in Cenozoic basalts from the Nushan volcano, eastern China, have been analyzed for their hydrogen content by microscopic Fourier transform infrared spectroscopy (Micro‐FTIR). The results demonstrate that hydrogen was incorporated in all these minerals in the manner of OH and that the content (H 2 O weight) is up to 2360 ppm for cpx, 1170 ppm for opx, and 880 ppm for pl. On the basis of the water content of constitutive minerals and their proportions, whole rock water contents of the Nushan granulites were estimated to be 150–950 ppm. Estimated equilibrium temperatures of the Nushan granulites are in the range of 810–892°C, corresponding to the lowermost crust at Nushan (about 25–30 km). Therefore this study provides direct evidence that the lower continental crust, even the lowermost part devoid of hydrous minerals, can contain a certain amount of water in nominally anhydrous minerals.