Rehman, Hafiz Ur et al. (2012) Sm-Nd and Lu-Hf Isotope Geochemistry of the Himalayan High- and Ultrahigh- Pressure Eclogites, Kaghan Valley, Pakistan , Geochemistry-Earth’s System Processes (Eds. by Panagiotaras, D.), 6, 105-126, doi: 10.5772/32859. < 20200120131418-350584 > pub
- abstract:
Eclogites are generally considered as derived from basaltic or gabbroic rocks which have either been intensely metamorphosed during subduction-obduction related processes or, associated with continental crust and affected by major crustal thrusting. The advantage of petrological, geochemical, and geochronological study of eclogitic rocks is twofold. First, metabasic rocks are capable of preserving the original magmatic characteristics of igneous formations. Second, the study of eclogites enables us to appreciate the behaviour of isotopic tracers during high-grade metamorphism.
- doi: 10.5772/32859
- modified at 16 h ago
Table 2. Lu-Hf concentrations and isotopic ratios of the whole rock Group I and II eclogites and their constituent minerals Rehman, Hafiz Ur et al. (2012)
1: PH380 2: PH380Grt 3: PH380Cpx 4: PH381 5: PH381-Grt 6: PH381-Cpx 7: PH381-Cpxr 8: PH422 9: PH422Grt 10: PH422Cpx 11: PH422Ep 12: PH423 13: PH423Grt 14: PH423Cpx 15: PH423Ep 16: PH425 17: PH425Grt 18: PH425Cpx 19: PH425Ep
(a) Hf isotopes_procedures of Lu et al. (2007) on MC-ICP-MS Finnigan, Neptune
@article{20200120131418-350584,
author = "Rehman, Hafiz Ur and Kobayashi, Katsura and Tsujimori, Tatsuki and Ota, Tsutomu and Nakamura, Eizo and Yamamoto, Hiroshi and Kaneko, Yoshiyuki and Khan, Tahseenullah",
title = "Sm-Nd and Lu-Hf Isotope Geochemistry of the Himalayan High- and Ultrahigh- Pressure Eclogites, Kaghan Valley, Pakistan ",
journal = "Geochemistry-Earth’s System Processes (Eds. by Panagiotaras, D.)",
year = "2012",
volume = "6",
pages = "105-126",
doi = "10.5772/32859",
}