@article{oai:nipr.repo.nii.ac.jp:00002756,
 author = {タイノショウ, ヨシアキ and カガミ, ヒロオ and タカハシ, ユウヘイ and イイズミ, シゲル and オサナイ, ヤスヒト and ツチヤ, ノリヨシ and TAINOSHO, Yoshiaki and KAGAMI, Hiroo and TAKAHASHI, Yuhei and IIZUMI, Shigeru and OSANAI, Yasuhito and TSUCHIYA, Noriyoshi},
 journal = {Proceedings of the NIPR Symposium on Antarctic Geosciences},
 month = {Sep},
 note = {P(論文), The Sm-Nd whole rock isochron age was determined for metamorphic rocks from Mount Pardoe, Napier Complex. Acidic gneiss (orthopyroxene-mesoperthite-quartz gneiss), being one of the main representative metamorphic rocks, gave an age of 2516±274 Ma with an initial ^<143>Nd/^<144>Nd ratio of 0.50914±0.00021. εNd values normalized to 2516 Ma for individual acidic gneiss range from -3.7 to -7.0. This Sm-Nd whole-rock isochron age indicates a major period of equilibration of the isotopic system on a whole-rock scale at 2516±274 Ma.},
 pages = {115--121},
 title = {PRELIMINARY RESULT FOR THE Sm-Nd WHOLE-ROCK AGE OF THE METAMORPHIC ROCKS FROM MOUNT PARDOE IN THE NAPIER COMPLEX, EAST ANTARCTICA},
 volume = {7},
 year = {1994}
}