Northrop D A, Clayton R N. Oxygen isotopic fractionation in systems containing dolomite. J Geol, 1966, 74:174 - 196
[4]
Faure G. Principles of isotope geology. New York: John Wiley & Sons, 1977:368 - 369
[5]
Fritz P, Smith D G W. The isotopic composition of secondary dolomites. Geochimica et Comochimica Acta, 1970, 34:1161 - 1173
[6]
Lister G S, et al. Lake Qinghai, China: closed-basin lake levels and the oxygen isotope record for ostracoda since the latest Pleistocene. Palaeogeogr Palaeoclimatol Palaeoecol, 1991, 84:141 - 162
[7]
Yu J Q, Kelts K R. Abrupt changes in climatic conditions across the late glacial/Holocene transition on the N. E. Tibet-Qinghai Plateau: evidence from Lake Qinghai, China. J Paleolimno, 2002, 28:195 - 206
Sheppard S M F, Schwarcz H P. Fractionation of carbon and oxygen isotopes and magnesium between coexisting metamorphic calcite and dolomite. Contr Mineral Petrol. 1970, 26:161 - 198
[10]
O\' Neil J R, Epstein S. Oxygen isotope fractionation in the system dolomite-calcite-carbon dioxide. Science, 1966, 152:198 - 201
[11]
Yu J Q, et al. Paleoenvironmental signatures from carbonate minerals and stable isotopic composition from Lake Qinghai,China. Chtem Geol, 2004 (in review)
