Kwiecien O, Arz HW, Lamy F, et al. North Atlantic control on precipitation pattern in the eastern Mediterranean/Black Sea region during the last glacial[J]. Quat Res, 2009, 71: 375.
[2]
叶瑛,沈忠悦,彭晓彤,等. 塔里木盆地下第三系储层砂岩自生碳酸盐碳、氧同位素组成及流体来源讨论[J]. 浙江大学学报:理学版,2001,28(3):321-326. Ye Ying, Shen Zhongyue, Peng Xiaotong, et al. C-O isotope composition of the authigenic carbonate in Low Tertiary reservoirs andstones in Tarim Basin and its implication on the fluid origin[J]. Journal of Zhejiang University (Science Edition) , 2001 , 28(3) : 321-326(in Chinese).
[3]
高玉巧,刘立. 自生片钠铝石的碳、氧同位素特征及其成因意义[J]. 高校地质学报,2006,12(4):522-529.Gao Yuqiao, Liu Li. Carbonoxygen isotopic characteristics of authigenic dawsonite and its genetic significance[J]. Geological Journal of China Universities, 2006, 112(4): 522-529(in Chinese).
[4]
陈永权,周新源,赵葵东,等. 塔里木盆地中寒武统泥晶白云岩红层的地球化学特征与成因探讨[J]. 高校地质学报,2008,14(4):583-592.Chen Yongquan, Zhou Xinyuan, Zhao Kuidong, et al. Geochemical research on Middle Cambrian red dolostones in Tarim Basin: Implication for dolostone genesis[J]. Geological Journal of China Universities, 2008,14(4): 583-592(in Chinese).
Hu Mingyi, Gao Zhenzhong, Li Jianming. Diagenesis of carbonate rocks on platform margin and deep water slope in the upper simian-ordovician in the middle to upper Yangtze area[J]. Experime ntalpetroleum Geology, 1998, 20(3):239-248(in Chinese).
[8]
Scobar J E, Curtis J H, Brenner M, et al. Isotope measurements of single ostracod valves and gastropod shells for climate reconstruction: evaluation of withinsample variability and determination of optimum sample size[J]. J Palaeolimnol,2010, 43: 921.
[9]
Sp？tl C, Mattey D. Stable isotope microsampling of speleothems for palaeoenvironmental studies: a comparison of microdrill, micromill and laser ablation techniques[J]. Chem Geol, 2006, 235: 48.
[10]
Simstich J, Stanovoy V, Bauch D, et al. Holocene variability of bottom water hydrography on the Kara Sea shelf (Siberia) depicted in multiple single-valve analyses of stable isotopes in ostracods[J]. Mar Geol, 2004, 206: 147.
[11]
Leng M J, Marshall J D. Palaeoclimate interpretation of stable isotope data from lake sediment archives[J]. Quat Sci Rev, 2004, 23: 811.
[12]
Revesz K M, Landwehr J M.δ13C and δ18O isotopic composition of CaCO3 measured by continuous flow isotope ratio mass spectrometry: statistical evaluation and verification by application to Devils Hole DH-11 calcite[J].Rapid Communications in Mass Spectrometry, 2002, 16: 2102-2114.
[13]
Mangili C, Plessen B, Wolff C, et al. Climatic implications of annual to decadal resolution stable isotope data from calcite varves of the Piànico interglacial lake record, Southern Alps[J]. Global Planet Change, 2010, 71: 168.
[14]
Burman J, Gustafsson O, Segl M, et al. A simplified method of preparing phosphoric acid for stable isotope analyses of carbonates[J]. Rapid Communications in Mass Spectrometry, 2005, 19(21): 3086-3088.
