作者: D. M. Anderson , P. Hoekstra
DOI: 10.1126/SCIENCE.149.3681.318
关键词:
摘要: The nature of crystalline water in frozen pastes made from representative clay minerals and was studied by x-ray diffraction. Only the diffraction peaks corresponding to normal hexagonal ice structure were detected. relative intensities revealed evidence epitaxy that crystals appeared be preferentially oriented with their c-axes perpendicular individuial crystallites.