[1]DePaolo D J. 1988. Neodymium isotope geochemistry[M]. Berlin: Springer. 181p.
[2]
[2]Jacobsen S and Wasserburg G J. 1984. Sm-Nd isotopic evolution in chondrite and achondrite Ⅱ[J]. Earth Planet. Sci. Lett., 67: 137~150.
[3]
[3]Liu H. 1986. Metal element distribution model of the polymetallic ore deposits occurring in the Dongqiyishan district, Inner Mongolia[J]. Geol. and Prospecting, 22(7): 60~62 (in Chinese with English abstract).
[4]
[4]Liu X Y and Wang Q. 1995. Tectonics of the orogenic belts in Beishan Mt. Western China and their evolution[J]. Geological Research, 28: 37~48 (in Chinese with English abstract).
[5]
[5]Ludwig K R. 1992. Isoplot V. 2.57: A plotting and regression program for radiogenic isotope data[CP]. U.S. Geological Survey Open File Report 91-445, rev., March, 1992. 40p.
[6]
[6]Mearns E W. 1986. Sm-Nd ages for Norwegian garnet peridotite[J]. Lithos, 19: 269~278.
[7]
[7]Nie F J and Bjorlykke. 1994. Lead and sulfur isotope studies of the Wulashan quartz-K feldspar and quartz vein gold deposit, south western Inner Mongolia, People\'s Republic of China[J]. Econ. Geol., 89: 1289~1395.
[8]
[8]Zhou J Y, Zhang B, Zhang C W,et al. 1996. Geology of silver, rhenium-molybdenum, gold and copper deposits occurring within the eastern Tianshan ancient continent and along its margin[M]. Beijing: Geol. Pub. House. 1~191 (in Chinese).
[9]
[9]Zuo G C, Liu C Y, Feng Y Z, et al. 1992. Discovery of Chengjiang period granitoid in Hanshan area of Beishan and its geochemical Features[A]. Modern Geological Selections (Upper Part)[C]. Beijing: Geol. Pub. House. 68~73 (in Chinese).