Braun I, Montel J M, Nicollet C. 1998. Elecron microprobe dating of monazite from high-grade gneisses and pegmatites of the Kerala Khondalite Belt, Southern India. Chem. Geol., 146: 65~8.
[7]
Crowley J L, Ghent E D. 1999. An electron microprobe study of the U-Th-Ph systematics of metamorphosed monazite: the role of Pb diffsion versus overgrowth and recrystallization. Chem. Geol., 157: 285~302.
[8]
Frster H J, Harlov D E, Milke R. 2000. Composition and Th-U total Pb ages of huttonite and thorite from Gillespie\'s beach, South Island, New Zealand. The Canadian Mineralogist, 3:675~684.
[9]
Montel J M, Veschambre M, Nicollet C. 1994. Datation de monazite la microsonde électronique. C R Acad. Sci., 318:127~146.
[10]
Suzuki K, Adachi M. 1991a. Precambrian provenance and Silurian metamorphism of the Tsunosawa paragneiss in the South Kitakami terrane, Northeast Japan, revealed by the chemical Th-U-total Pb-isochron ages of monazite, zircon and xenotime. Geochem J., 25: 357~376.
[11]
Suzuki K, Adachi M. 1991b. The chemical Th-U-Total Pb isochron ages of ziron and monazite from the Gray granite of the hida terrane. Japan. Journal of Earth Sciences. Nagoya University, 38: 11~37.
[12]
Montel J M, Foret S, Veschambre M, Nicollet C, Provost A. 1996. A fast, non-expensive, rehable, in situ dating techniqu: Electron microprobe ages on monazite. Chem. Geol., 131: 37~53.
[13]
Nakai Y, Suzuki K. 1996. CHIME monazite ages of the Kamihara Tonalite and the Tenryukyo Granodiorite in the eastern Ryoke belt of central Japan. Journal of the Geological Society of Japan, 102(5):431~439.
[14]
Shannon R D. 1976. Revised effective ionic radii and systematic studies of interatomic distances in halides and chalcogenides. 32(A): 751~767.
[15]
Suzuki K, Adachi M, Tsuyoshi T. 1991c. Middle Precambrian provenance of Jurassic sandstone in the Mino Terrane central Japan: Th-U-total Pb evidence from an electron microprobe Monazite study. Sedimentary Geology, 75: 141~147.
[16]
Suzuki K, Adachi M. 1994a. Middle Precambrian detrital monazite and zircon from the Hida gneiss on Oki-Dogo island, Japan: theirorigin and implications for the correlation of basement gneiss of southwest Japan and Korea. Tectonophsysics, 235: 277~292.
[17]
Suzuki K, Adachi M, Kazjizuka I. 1994b. Electron microprobe observations of Ph diffusion in metamorphosed detrital monazites. Earth Planet. Sci. Lett., 128: 391~405.
[18]
Suzuki K, Nasu T, Shibata K. 1995. CHIME monazite ages of the Otagriri and Ichida granites in the Komagane are Nagano prefecture. The Journal of Earth and Planetary Sciences, Nogoya University, 42: 17~30.
[19]
Suzuki K, Adachi M, Nuraki T. 1996. CHIME age dating of monazites from metamorphic rocks and granitic rocks of the Ryoke belt in the Iwakwni are, Southwest Japan. Island Arc, 5:43~55
[20]
Suzuki K, Adachi M. 1998. Denudation history of the high T/P Ryoke metamorphic belt, southwest Japan: constraints from CHIME monazite ages of gneisses and granitoids. Journal of Metamorphic Geology, 16: 23~37.
[21]
Suzuki K, Adachi M. 1997. Th-U and Pb analytical data of monazites used in the paper Denudation history of the high T/p Ryoke metamorphic belt, Southwest Japan; Contraints from CHIME monazite ages of gneisses and granitoids. Journal of the Earth Planetary Science, Nagoya university, 44: 103~111.
[22]
Williams M L, Jercinovic M J, Terry M P. 1999, Age mapping and of monazite on the electron microprobe: Deconvoluting multistage tectonic histories. Geology, 27(11): 1023~1026.